Natural Resources
Conservation Service
Major Land Resource Area 010X
Major Land Resource Area
Accessed: 04/23/2026
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Description
This MLRA is characterized by gently rolling to steep hills, plateaus, and low mountains at the foothills of the Blue Mountains in Oregon and the Central Rocky Mountains in Idaho. The geology of this area is highly varied and ranges from Holocene volcanics to Cretaceous sedimentary rocks. Mollisols are the dominant soil order and the soil climate is typified by mesic or frigid soil temperature regimes, and xeric or aridic soil moisture regimes. Elevation ranges from 1,300 to 6,600 feet (395 to 2,010 meters), increasing from west to east. The climate is characterized by dry summers and snow dominated winters with precipitation averaging 8 to 16 inches (205 to 405 millimeters) and increasing from west to east. These factors support plant communities with shrub-grass associations with considerable acreage of sagebrush grassland. Big sagebrush, bluebunch wheatgrass, and Idaho fescue are the dominant species. Stiff sagebrush, low sagebrush, and Sandberg bluegrass are often dominant on sites with shallow restrictive layers. Western juniper is one of the few common tree species and since European settlement has greatly expanded its extent in Oregon. Nearly half of the MLRA is federally owned and managed by the Bureau of Land Management. Most of the area is used for livestock grazing with areas accessible by irrigation often used for irrigated agriculture. For further information, see "Land Resource Regions and Major Land Resource Areas of the United States, the Caribbean, and the Pacific Basin (U.S. Department of Agriculture Handbook 296, 2006)" available online at: https://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/survey/?cid=nrcs142p2_053624
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i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
-
i
Key Characteristics
- Site located north of the Columbia River.
- Within a national park soil survey or in an area joining with a national park in the Washington Cascades Range
- NORTH CASCADES NATIONAL PARK
- Site is forested and more than 25 percent is covered with trees
- Site typically is on west slope of North Cascade Mountains, but areas are throughout the mountains
- Site is in many landscape positions at middle elevations (2,200 to 4,600 feet above sea level). It is cold and moist with snow commonly persisting until late in spring or early in summer. Pacific silver fir and western hemlock are common trees. Black huckleberry, false azalea, oakfern, and queenscup beadlily are common in the understory. If yes, the site is Low Cryic/Udic West Coniferous (F003NX924WA).
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Sites occurring in east of the Snake River.
Sites occurring west of the Snake River.
Occurring on the Upper Snake River Lava Plains and Hills
Occurring the Footslopes and Plains of the Big and Little Wood Rivers
Site occurs on uplands.
Site occurs on bottomlands with slopes less than five percent.
Site Occurs on Uplands
Site occurs on bottomlands with slopes less than 8 percent
Sites occurring on fluvial landforms including stream channels, terraces, secondary terraces, meadows, bottoms, swales, and fans. These sites occur across LRU boundaries.
Not as above
Sites occurring on high elevation fens
R010XY032OR – Meadow Fen 14+ PZ
R010XY032OR – Meadow Fen 14+ PZ
Not as above
Sites occurring in the Madras Plains LRU. Characterized by deeper soils on nearly level plateaus. Most areas are row cropped. The dominant area for this unit is the Agency Plain. The dominant soils are the Agency and Madras soil series. Surface texture is sandy loam or loam. The soils lack the strong volcanic ash influence typical of the Pumice Lava Plains LRU. Temperature regime is mesic; moisture regime is aridic.
Not as above
Sites occurring on north aspect slopes
Not as above
Sites occurring in the Pumice Lava Plains LRU. Characterized by moderately deep and shallow soils formed in ash from Mt. Mazama over basalt. Most areas are native rangelands or used for irrigated pasture or hayland. Slopes are nearly level to undulating. The dominant soils are Deschutes and Deskamp. Texture is sandy loam and loamy sand throughout the profile. Temperature regime is mesic; moisture regime is aridic.
Not as above
Site is on a cinder butte. Soils are ash over scoriaceous cinders
R010XA014OR – Juniper Cinder Hills 10-12 PZ
R010XA014OR – Juniper Cinder Hills 10-12 PZ
Not as above
Sites occurring in the John Day Sediments LRU. This unit is characterized by rangeland soils on hills or mountains associated with the John Day/Clarno Formation and/or basalt. Temperature regime is dominantly mesic; moisture regime is aridic and xeric. (warm climate).
Not as above
Soil has an abrupt textural change within 10 inches of the surface (well-developed claypan)
R010XB024OR – JD Warm Ashy Claypan 9-12 PZ
R010XB024OR – JD Warm Ashy Claypan 9-12 PZ
Not as above
Sites occurring in the John Day Mountain Foothills LRU. Characterized by rangeland soils on hills or mountains associated with basalt. Temperature regime is frigid; moisture regime is xeric. (cool moist climate) Soils are commonly influenced by Mt. Mazama ash in the surface. Textures are dominantly loams and clays.
Not as above
Soil has an abrupt textural change within 10 inches of the surface (well-developed claypan)
Not as above
Sites occurring in the Snake River Mountain Foothills LRU. Characterized by rangeland soils on hills or mountains associated with basalt. Temperature regime is frigid; moisture regime is xeric. (cool moist climate) Textures are dominantly loams and silt loams or silty clay loams.
Not as above
Soil has an abrupt textural change within 10 inches of the surface (well-developed claypan)
R010XB029OR – Blue Mountain Foothills, Claypan 9-12 PZ
R010XB029OR – Blue Mountain Foothills, Claypan 9-12 PZ
Not as above
Snake River Warm Plains LRU. Located between Oregon's Blue and Wallowa Mountains and the northwestern Snake River Plain. Characterized by soils on hills and mountains associated with basalt and exposed tuffaceous sediments. Plants are subject to wide temperature ranges, high evapotranspiration, and high early-season moisture stress. Temperature regime is mesic and the moisture regime is aridic. Mean annual precipitation is 9 to 12 inches. (warm dry)
Soils are very shallow over highly fractured bedrock. Ecosite identified but not developed
Not as above
Slopes greater than 30 percent on northerly aspects
Slopes greater than 30 percent on southerly aspects
Slopes less than 30 percent on all aspects (non-aspect)
Soils derived from granite
Soils not derived from granite
Site occurs in 12 to 16 inch precipitation zones at 3000 to 4500 feet elevation
R010XY014ID – North Slope Granitic 12-16 PZ ARTRX/FEID
R010XY014ID – North Slope Granitic 12-16 PZ ARTRX/FEID
Site occurs in 16 to 22 inch precipitation zones at 4000 to 5500 feet elevation
R010XY013ID – North Slope Granitic 16-22 PZ ARTRV/FEID
R010XY013ID – North Slope Granitic 16-22 PZ ARTRV/FEID
Site occurs in 12 to 16 inch precipitation zones at 2100 to 4000 feet elevation. Soils are moderately deep to deep loams and silt loams
R010XY001ID – North Slope Loamy 12-16 PZ FEID-PSSPS
R010XY001ID – North Slope Loamy 12-16 PZ FEID-PSSPS
Site occurs in 16 to 22 inch precipitation zones at 3000 to 5500 feet elevation. Soils are deep silt loams
R010XY005ID – North Slope Loamy 16-22 PZ ARTRV/FEID
R010XY005ID – North Slope Loamy 16-22 PZ ARTRV/FEID
Site occurs in 16 to 20 inch precipitation zones at 2700 to 5800 feet elevation. Soils are excessively drained coarse sandy loams to fine gravelly sandy loams over 20 inches deep
R010XY027ID – North Slope Brush 16-20 PZ PREM/ELGLG
R010XY027ID – North Slope Brush 16-20 PZ PREM/ELGLG
Soils are not stony
Soils are stony
Soils derived from granite
Soils not derived from granite
Site occurs in 12 to 16 inch precipitation zones at 3000 to 5000 feet elevation. Soils are moderately deep and coarse textured
R010XY008ID – South Slope Granitic 12-16 PZ PUTR2/PSSPS
R010XY008ID – South Slope Granitic 12-16 PZ PUTR2/PSSPS
Site occurs in 16 to 20 inch precipitation zones at 3000 to 6000 feet elevation. Soils are moderately deep to deep coarse sandy loams
R010XY028ID – South Slope Granitic 16-20 PZ ARTRX/PSSPS
R010XY028ID – South Slope Granitic 16-20 PZ ARTRX/PSSPS
Site occurs in 12 to 16 inch precipitation zones at 3000 to 4800 feet elevation. Soils are loamy derived from acid igneous alluvial or lacustrine deposits and are moderately deep to deep
R010XY019ID – South Slope Loamy 12-16 PZ ARTRX/PSSPS
R010XY019ID – South Slope Loamy 12-16 PZ ARTRX/PSSPS
Site occurs in 16 to 22 inch precipitation zones at 3000 to 5000 feet elevation. Soils are deep silt loams to silty clay loams derived from colluvium, tuff, rhyolite, basalt, and siltstone
R010XY004ID – South Slope Loamy 16-22 PZ ARTRX/PSSPS
R010XY004ID – South Slope Loamy 16-22 PZ ARTRX/PSSPS
Site occurs in 12 to 16 inch precipitation zone at 2600 to 3900 feet elevation. Soils are deep, sand to sandy loams formed from lacustrine deposits
R010XY031ID – South Slope Sandy 12-16 PZ
R010XY031ID – South Slope Sandy 12-16 PZ
Soil depth is moderately deep to deep
Soil depth is shallow
Site occurs in 12 to 16 inch precipitation zones at 2000 to 3500 feet. Textures are stony loams
R010XY011ID – South Slope Stony 12-16 PZ ARTRT/PSSPS
R010XY011ID – South Slope Stony 12-16 PZ ARTRT/PSSPS
Site occurs in 16 - 22 inch precipitation zones at 3500 to 4500 feet. Textures are stony to extremely stony loams
R010XY021ID – Stony Loam 16-22 PZ ARTRT/PSSPS
R010XY021ID – Stony Loam 16-22 PZ ARTRT/PSSPS
Site occurs in 12 to 16 inch precipitation zones at 3000 to 4500 feet. Textures are stony loams to clay loams
R010XY016ID – Shallow South Stony 12-16 PZ ARTRX/PSSPS
R010XY016ID – Shallow South Stony 12-16 PZ ARTRX/PSSPS
Site occurs in 14 to 18 inch precipitation zones at 2400 to 5000 feet. Textures are very stony loams to very gravelly clay loams
R010XY018ID – Shallow South Stony 14-18 PZ PSSPS-POSE
R010XY018ID – Shallow South Stony 14-18 PZ PSSPS-POSE
Site occurs in 12 to 20 inch precipitation zones at 4000 to 7500 feet. Textures are cobbly and stony clay loams. Soil depths range from 10 to 40 inches
R010XY017ID – South Slope Clayey 12-20 PZ ARAR8/PSSPS
R010XY017ID – South Slope Clayey 12-20 PZ ARAR8/PSSPS
Soils are not stony
Soils are stony
Site occurs in 12 to 16 inch precipitation zones at 2500 to 4500 feet. Textures are loamy
R010XY007ID – Loamy 12-16 PZ
R010XY007ID – Loamy 12-16 PZ
Site occurs in 12 to 16 inch precipitation zones at 2500 to 3200 feet. Textures are loamy fine sand to very fine sandy loam
R010XY032ID – Loamy 12-16 PZ
R010XY032ID – Loamy 12-16 PZ
Site occurs in 16 to 20 inch precipitation zones at 3000 to 4000 feet elevation. Textures are sandy loams to clay loams
R010XY003ID – Loamy 16-22 PZ PUTR2/FEID
R010XY003ID – Loamy 16-22 PZ PUTR2/FEID
Site occurs in 16 to 22 inch precipitation zones at 3000 to 5000 feet. Textures are coarse sandy loams derived from granite
R010XY022ID – Granitic 16-22 PZ PSSPS-FEID
R010XY022ID – Granitic 16-22 PZ PSSPS-FEID
Site occurs in 8 to 16 inch precipitation zones at 2000 to 3000 feet. Textures are clay and deep vertisols
R010XY006ID – Churning Clay 8-16 PZ ARTRX/PSSPS
R010XY006ID – Churning Clay 8-16 PZ ARTRX/PSSPS
Soil depth is moderately deep to deep
Soil depth is very shallow to shallow
Site occurs in 12 to 16 inch precipitation zones at 2500 to 4500 feet. Textures are stony loams
R010XY009ID – Stony Loam 12-16 PZ ARTRT/PSSPS
R010XY009ID – Stony Loam 12-16 PZ ARTRT/PSSPS
Site occurs in 16 to 22 inch precipitation zones at 3500 to 4500 feet. Textures are deep, stony to extremely stony, loams
R010XY021ID – Stony Loam 16-22 PZ ARTRT/PSSPS
R010XY021ID – Stony Loam 16-22 PZ ARTRT/PSSPS
Site occurs in 12 to 20 inch precipitation zones at 2500 to 4000 feet. Soils are very shallow, stony to extremely stony loams to clay loams
R010XY002ID – Very Shallow 12-20 PZ ARRI2/POSE
R010XY002ID – Very Shallow 12-20 PZ ARRI2/POSE
Site occurs in 12 to 20 inch precipitation zones at 2500 to 4500 feet. Soils are shallow, very stony loams to very gravelly clay loams
R010XY025ID – Shallow Stony Loam 12-20 PZ ARTRX/PSSPS
R010XY025ID – Shallow Stony Loam 12-20 PZ ARTRX/PSSPS
Water standing at or above the surface into late summer
R010XY030ID – Marsh TYLA-SCAC3
R010XY030ID – Marsh TYLA-SCAC3
Water at or near the surface at beginning of growing season and down to 10 to 20 inches at the end of the growing season
R010XY029ID – Wet Meadow Carex-Juncus
R010XY029ID – Wet Meadow Carex-Juncus
Water at or near the surface at beginning of growing season and down to 20 to 40 inches at the end of the growing season
R010XY023ID – Meadow DECA18-CANE2
R010XY023ID – Meadow DECA18-CANE2
Water at or near the surface at beginning of the growing season and greater than forty inches at the end of the growing season
R010XY024ID – Dry Meadow PONE3-PHAL2
R010XY024ID – Dry Meadow PONE3-PHAL2
Slopes greater than 30 percent on northerly aspects
Slopes greater than 30 percent on southerly aspects
Slopes generally less than 30 percent, occurring on all aspects
Site occurs in greater than 20 inch precipitation zones, in areas of moisture accumulating topography
R010XA016ID – Quaking Aspen 20+ PZ POTR5
R010XA016ID – Quaking Aspen 20+ PZ POTR5
Site is in 12 to 16 inch precipitation zones with elevation below 7000 feet
Site occurs in 16 to 22 inch precipitation zones
Soils are volcanic cinders
Soils are not volcanic cinders
Coarse cinder soils, little soil development, cryic soil temperature regime
R010XA043ID – Cinder North 12-16 PZ PIFL2/PUTR2
R010XA043ID – Cinder North 12-16 PZ PIFL2/PUTR2
Somewhat finer cinder soils, greater soil development, frigid soil temperature regime
R010XA047ID – Cindery North 12-16 PZ ARTRV-PUTR2/FEID-PSSPS
R010XA047ID – Cindery North 12-16 PZ ARTRV-PUTR2/FEID-PSSPS
Soils are extremely bouldery loams. Large boulders are common on the surface.
R010XA037ID – Shrubby Stony North 12-16 PZ ARTRV/FEID
R010XA037ID – Shrubby Stony North 12-16 PZ ARTRV/FEID
Soils are moderately deep to deep stony loams.
R010XA036ID – North Slope Stony 12-16 PZ ARTRX/PSSPS
R010XA036ID – North Slope Stony 12-16 PZ ARTRX/PSSPS
Soils are deep and loamy, site occurs at an elevation between 5000 to 8800 feet
R010XA008ID – North Slope Loamy 16-22 PZ
R010XA008ID – North Slope Loamy 16-22 PZ
Soils are generally shallow to fractured bedrock or clay. Roots penetrate below 20 inches.
R010XA010ID – North Slope Fractured 16-22 PZ
R010XA010ID – North Slope Fractured 16-22 PZ
Soils are very shallow to bedrock or clay
R010XA011ID – Clayey North 16-22 PZ
R010XA011ID – Clayey North 16-22 PZ
Occurs in 16 to 22 inch precipitation zone
Occurs in less than 16 inch precipitation zones
Site occurs in greater than 20 inch precipitation zones, in areas of moisture accumulating topography
R010XA016ID – Quaking Aspen 20+ PZ POTR5
R010XA016ID – Quaking Aspen 20+ PZ POTR5
Slopes greater than 45 percent
R010XA014ID – Steep South Slope 16-22 PZ
R010XA014ID – Steep South Slope 16-22 PZ
Slopes less than 45 percent
R010XA015ID – South Slope Loamy 16-22 PZ
R010XA015ID – South Slope Loamy 16-22 PZ
Soils are volcanic cinders
Soils not volcanic cinders
Coarse cinder soils, little soil development... R010XA045ID – Cinder South 12-16 PUTR2/HECO26 (Draft concept)
Somewhat finer cinder soils, greater soil development... R010XA048ID – Cindery South 12-16 PUTR2-ARTRV/PSSPS (Draft concept)
Site occurs in association with rock outcrops and talus slopes
R010XA030ID – South Slope Channery 11-13 PZ ARTRX/PSSPS
R010XA030ID – South Slope Channery 11-13 PZ ARTRX/PSSPS
Not as above
Soils greater than 20 inches to bedrock
Soils less than 20 inches to fractured bedrock
Coarse fragments greater than 35 percent throughout the soil profile
R010XA009ID – South Slope Gravelly 12-16 PZ
R010XA009ID – South Slope Gravelly 12-16 PZ
Not as above
R010XA025ID – South Slope Loamy 11-13 PZ ARTRW8/PSSPS
R010XA025ID – South Slope Loamy 11-13 PZ ARTRW8/PSSPS
Site occurs on exposed ridgetops... R010XA024ID – STONY WINDSWEPT RIDGE 8-16 (Draft concept)
Not as above
R010XA021ID – South Slope Fractured 12-16 PZ
R010XA021ID – South Slope Fractured 12-16 PZ
Site associated with recent lava flows
Not as above
Soils 10 to 20 inches deep over fractured basalt
R010XA020ID – Mixed Shrub 12-16 PZ
R010XA020ID – Mixed Shrub 12-16 PZ
Soils less than 10 inches to basalt or lava bedrock
R010XA050ID – Very Shallow Loam 12-16 PZ ARAR8/POSE
R010XA050ID – Very Shallow Loam 12-16 PZ ARAR8/POSE
Soils greater than 20 inches deep
Site nearly devoid of vegetation, coarse cinder soils, little soil development
R010XA046ID – Cinder Garden 12-16 PZ EROVD-LERE7
R010XA046ID – Cinder Garden 12-16 PZ EROVD-LERE7
Somewhat finer cinder soils, greater soil development, cryic soil temperature regime
R010XA044ID – Cinder 12-16 PZ PIFL2/ARTRV
R010XA044ID – Cinder 12-16 PZ PIFL2/ARTRV
Soils with greater soil development than on Cinder 12 to 16. Increased fine soil particles within the profile... R010XA049ID – Gravelly Loam 12-16 ARTRV/PUTR2/PSSPS (Draft concept)
Soils are 20 inches or less
Soils are greater than 20 inches deep
Site occurs on exposed ridgetops... R010XA024ID – STONY WINDSWEPT RIDGE 8-16 (Draft concept)
Not as above
Surface texture is generally loam to silt loam but may be finer
R010XA007ID – Shallow Stony Loam 8-16 PZ
R010XA007ID – Shallow Stony Loam 8-16 PZ
Surface texture is generally clay loam to silty clay but may be coarser
R010XA038ID – Stony Clayey 8-16 PZ ARAR8/PSSPS
R010XA038ID – Stony Clayey 8-16 PZ ARAR8/PSSPS
Soils are sandy
R010XA022ID – Sandy Loam 12-16 PZ
R010XA022ID – Sandy Loam 12-16 PZ
Soils are clayey to loamy
Site has large boulders on or near surface
Not as above
Site is below 5000 feet elevation
R010XA032ID – Bouldery 11-13 PZ ARTRX/PSSPS
R010XA032ID – Bouldery 11-13 PZ ARTRX/PSSPS
Site is above 5000 feet elevation
R010XA031ID – Bouldery Loam 12-16 PZ ARTRV/FEID
R010XA031ID – Bouldery Loam 12-16 PZ ARTRV/FEID
Soils are 20 to 40 inches to a duripan
Not as above
Sites occur in 12 to 16 inch precipitation zones, root restricting clayey subsurface at 14 to 18 inches
R010XA001ID – Clayey 12-16 PZ ARARL/FEID
R010XA001ID – Clayey 12-16 PZ ARARL/FEID
Sites occur in 10 to 12 inch precipitation zones
R010XA034ID – Claypan 10-12 PZ ARTR4/PSSPS-ACTH7
R010XA034ID – Claypan 10-12 PZ ARTR4/PSSPS-ACTH7
Site occurs in 11 to 13 inch precipitation zones
Site occurs in 12 to 16 inch precipitation zones
Site occurs in greater than 20 inch precipitation zone, in areas of moisture accumulating topography
R010XA016ID – Quaking Aspen 20+ PZ POTR5
R010XA016ID – Quaking Aspen 20+ PZ POTR5
Sites occur on slopes of 1 to 15 percent at elevations 4250 to 5000 feet. Soils are moderately deep. Textures are loams and silt loams.
R010XA033ID – Loamy 11-13 PZ ARTRX/PSSPS
R010XA033ID – Loamy 11-13 PZ ARTRX/PSSPS
Sites occur on slopes of 5 to 25 percent and elevations from 4000 to 5500 feet. Soils are moderately deep. Textures are loams and silt loams.
R010XA026ID – Loamy 11-13 PZ ARTRW8/PSSPS
R010XA026ID – Loamy 11-13 PZ ARTRW8/PSSPS
Sites occur on slopes from 1 to 30 percent and elevations from 4500 to 6500 feet. Soils are moderately deep to deep. Textures are loams, silt loams and gravelly silt loams
R010XA004ID – Loamy 12-16 PZ ARTRV/FEID-PSSPS
R010XA004ID – Loamy 12-16 PZ ARTRV/FEID-PSSPS
Sites occur on slopes from 1 to 20 percent and elevations from 4000 to 5500 feet. Soils are moderately deep to deep. Surface soils are silt loams. Subsoils are silty clay loam to clay loam.
R010XA023ID – Loamy 12-16 PZ ARTR4/FEID
R010XA023ID – Loamy 12-16 PZ ARTR4/FEID
Water table usually not present.
R010XA042ID – Loamy Bottom 12-16 PZ LECI4
R010XA042ID – Loamy Bottom 12-16 PZ LECI4
Water table present for most of the growing season.
Water standing at or above the surface into late summer... R010XA040ID MARSH TYLA-SCAC3 (Draft concept)
Water at or near the surface at beginning of growing season and down to 10 to 20 inches at the end of the growing season.
R010XA039ID – Wet Meadow Carex/Juncus
R010XA039ID – Wet Meadow Carex/Juncus
Water at or near the surface at beginning of growing season and down to 20 to 40 inches at the end of the growing season
R010XA027ID – Meadow DECA18-CANE2
R010XA027ID – Meadow DECA18-CANE2
Water at or near the surface at beginning of the growing season and greater than 40 inches at the end of the growing season.
R010XA028ID – Dry Meadow 8-15 PZ PONE3-PHAL2
R010XA028ID – Dry Meadow 8-15 PZ PONE3-PHAL2
Sites occurring along the active channel of a perennial or intermittent stream to riparian sites
Not as above
Soil temperature regime is mesic
Soil temperature regimes is mesic near frigid or cooler
Site occupies depositional floodplains and gravel bars
R010XY010OR – Coyote Willow Riparian
R010XY010OR – Coyote Willow Riparian
Site occupies primary terraces
R010XY011OR – Cottonwood-Willow-Riparian
R010XY011OR – Cottonwood-Willow-Riparian
Depth to alluvial sediments is 60 inches or greater
R010XY225OR – Aspen Riparian 12-18 PZ
R010XY225OR – Aspen Riparian 12-18 PZ
Not as above
Soil temperature regime is mesic near frigid to frigid near mesic
R010XY012OR – Booth-Yellow Willow Riparian
R010XY012OR – Booth-Yellow Willow Riparian
Soil temperature regimes is frigid to cryic
R010XY013OR – Booth-Geyer-Yellow Willow Riparian
R010XY013OR – Booth-Geyer-Yellow Willow Riparian
Site occurs on floodplains of perennial streams and rivers, near channels occupying primary terraces to meadows
Not as above
Soil temperature regime is mesic to frigid near mesic
Soil temperature regime is frigid to cryic
Water table is within 12 inches of the soil surface March through July
R010XY003OR – Wet Meadow
R010XY003OR – Wet Meadow
Water table is deeper than 12 inches of the soil surface March through July
Soil has sodic properties
R010XY008OR – Sodic Meadow
R010XY008OR – Sodic Meadow
Soil does not have sodic properties
R010XY004OR – Meadow
R010XY004OR – Meadow
Water table is within 12 inches of the soil surface March through July
R010XY001OR – Cold Wet Meadow
R010XY001OR – Cold Wet Meadow
Water table is deeper than 12 inches of the soil surface March through July
Shrub component common, dominated by silver sagebrush
R010XY002OR – Cold Meadow
R010XY002OR – Cold Meadow
Not as above
R010XY033OR – Cold Moist Meadow
R010XY033OR – Cold Moist Meadow
Site occurs on floodplains of perennial streams and rivers, occupying secondary terraces to bottoms
Not as above
Soil temperature regime is mesic to frigid near mesic
Soil temperature regime is frigid to cryic
R010XY006OR – Mountain Loamy Bottom
R010XY006OR – Mountain Loamy Bottom
Soil has sodic properties
R010XY007OR – Sodic Bottom
R010XY007OR – Sodic Bottom
Soil does not have sodic properties
Soils are sandy in the particle control section
R010XY009OR – Sandy Bottom
R010XY009OR – Sandy Bottom
Soils are not sandy in the particle control section
Soils are clayey in the particle control section
R010XY014OR – Clayey Bottom
R010XY014OR – Clayey Bottom
Soils are loamy in the particle control section
R010XY005OR – Loamy Bottom
R010XY005OR – Loamy Bottom
Site occurs adjacent to and on floodplains or ephemeral streams, upper end of drainages to swales
Not as above
Soil temperature regime is mesic to frigid near mesic
Soil temperature regime is frigid and mesic near frigid
Soil moisture regime is aridic
R010XY113OR – Swale 9-12 PZ
R010XY113OR – Swale 9-12 PZ
Soil moisture regime is xeric
R010XY116OR – Swale 12-16 PZ
R010XY116OR – Swale 12-16 PZ
Soil moisture regime is aridic
R010XY114OR – Cool Swale 9-12 PZ
R010XY114OR – Cool Swale 9-12 PZ
Soil moisture regime is xeric
Sites have higher available water holding capacities (8 to 10 inches). In the reference state, basin wildrye is the dominant grass species and has higher production than the Dry Mountain Swale site
R010XY117OR – Mountain Swale 12-16 PZ
R010XY117OR – Mountain Swale 12-16 PZ
Sites have lower plant available water (3 to 6 inches). In the reference state, Idaho fescue is the dominant grass and has lower production than the Mountain Swale sites
R010XY119OR – Dry Mountain Swale 12-16 PZ
R010XY119OR – Dry Mountain Swale 12-16 PZ
Site occurs on mountain side slopes and plateaus in areas receiving additional subsurface moisture from ephemeral subsurface flows
R010XY230OR – Aspen Upland 12-18 PZ
R010XY230OR – Aspen Upland 12-18 PZ
Not as above or sites occurring on alluvial fans
Precipitation 9 to 12 inches, aridic soil moisture regime
Precipitation 12 to 16 inches, xeric soil moisture regime
R010XY125OR – Gravelly Fan 12-16 PZ
R010XY125OR – Gravelly Fan 12-16 PZ
Soil has sodic properties
R010XY126OR – Sodic Fan 9-12 PZ
R010XY126OR – Sodic Fan 9-12 PZ
Soil does not have sodic properties
Typically occurring on lower fan toeslope or terrace positions, hydrologically connected to stream networks
R010XY120OR – Loamy Fan 9-12 PZ
R010XY120OR – Loamy Fan 9-12 PZ
Not as above
Soils are clays with very fine particle size classes
R010XY121OR – Droughty Clayey Fan 9-12 PZ
R010XY121OR – Droughty Clayey Fan 9-12 PZ
Soils are typically loamy-skeletal (sometimes fine) particle size classes
R010XY153OR – Droughty Fan 9-12 PZ
R010XY153OR – Droughty Fan 9-12 PZ
Sites occurring on south aspect slopes
R010XA007OR – Juniper Pumice South 9-12 PZ
R010XA007OR – Juniper Pumice South 9-12 PZ
Not as above or sites that are not influenced by aspect
Ecosites associated with buttes and often slopes greater than 40 percent
R010XA014OR – Juniper Cinder Hills 10-12 PZ
R010XA014OR – Juniper Cinder Hills 10-12 PZ
Not as above
Sites associated with swales, fans, or terraces
Sites associated with plateaus and ridges
Sites occur on slopes greater than 30 percent
R010XA002OR – Juniper Shrubby Pumice Hills 8-10 PZ
R010XA002OR – Juniper Shrubby Pumice Hills 8-10 PZ
Sites occur on slopes less than 15 percent
R010XA003OR – Droughty 8-10 PZ
R010XA003OR – Droughty 8-10 PZ
Particle size class is clayey to fine loamy but not skeletal or ashy
R010XA001OR – Loamy 8-10 PZ
R010XA001OR – Loamy 8-10 PZ
Particle size class is most often coarse to fine loamy or loamy skeletal but not clayey
Particle size class is often fine to fine loamy. Soils have a water holding potential of three to six inches leading to higher annual production and higher cover of western juniper compared to Shrubby Loam 8 to 12 precipitation zone sites
R010XA018OR – Juniper Shrubby Loam 10-12 PZ
R010XA018OR – Juniper Shrubby Loam 10-12 PZ
Particle size class is often coarse loamy to loamy skeletal. Soils have a water holding potential of two to four inches leading to lower annual production and lower western juniper cover than the Juniper Shrubby Loam 10 to 12 precipitation zone sites
R010XA019OR – Shrubby Loam 8-12 PZ
R010XA019OR – Shrubby Loam 8-12 PZ
Sites occurring on north aspect slopes
Not as above
Soil temperature regime is mesic
Soil temperature regime is frigid
R010XA026OR – Juniper Pumice North 10-12 PZ
R010XA026OR – Juniper Pumice North 10-12 PZ
Soils are less than 20 inches deep and contain more than 35 percent rock fragments
R010XA025OR – Juniper Shallow North 10-12 PZ
R010XA025OR – Juniper Shallow North 10-12 PZ
Soils are deeper than 20 inches
Soils are moderately deep between 20 and 40 inches
R010XA024OR – Pumice North 8-10 PZ
R010XA024OR – Pumice North 8-10 PZ
Soils are deep between 40 and 60 inches
R010XA083OR – Juniper Shrubby North 9-12 PZ
R010XA083OR – Juniper Shrubby North 9-12 PZ
Sites occurring on south aspect slopes. Soil temperature regime is mesic
R010XA007OR – Juniper Pumice South 9-12 PZ
R010XA007OR – Juniper Pumice South 9-12 PZ
Not as above or sites that are not influenced by aspect
Soil temperature regime is mesic
Soil temperature regime is frigid
Soils are very shallow or shallow
Soils are moderately deep to deep
Soils are volcanic ash/pumice over exposed lava flows and lava blisters or small knolls dispersed across lava plains
Not as above
R010XA018OR – Juniper Shrubby Loam 10-12 PZ
R010XA018OR – Juniper Shrubby Loam 10-12 PZ
Sites occur in eight to ten inch precipitation zones
R010XA022OR – Juniper Lava Blisters 8-10 PZ
R010XA022OR – Juniper Lava Blisters 8-10 PZ
Sites occur in 10 to 12 inch precipitation zones
R010XA023OR – Juniper Shrubby Lava Blisters 10-12 PZ
R010XA023OR – Juniper Shrubby Lava Blisters 10-12 PZ
Soils are loamy with less than thirty-five percent clay and greater than fifteen percent sand
Soils are sandy with less than eighteen percent clay and soil textures including sand or loamy sand
Particle size class is often coarse loamy to loamy skeletal. Soils have a water holding potential of two to four inches leading to lower annual production and lower western juniper cover than the Juniper Shrubby Loam 10 to 12 precipitation zone sites
R010XA019OR – Shrubby Loam 8-12 PZ
R010XA019OR – Shrubby Loam 8-12 PZ
Particle size class is often fine to fine loamy. Soils have a water holding potential of three to six inches leading to higher annual production and higher cover of western juniper compared to Shrubby Loam 8 to 12 precipitation zone sites
R010XA018OR – Juniper Shrubby Loam 10-12 PZ
R010XA018OR – Juniper Shrubby Loam 10-12 PZ
Sites occur in areas that receive eight to ten inches of precipitation annually
R010XA027OR – Juniper Pumice Flat 8-10 PZ
R010XA027OR – Juniper Pumice Flat 8-10 PZ
Sites occur in areas that receive ten to twelve inches of precipitation annually
R010XA009OR – Juniper Shrubby Pumice Flat 10-12 PZ
R010XA009OR – Juniper Shrubby Pumice Flat 10-12 PZ
Sites with surface fragment cover over 80 percent usually consisting of small channers
R010XA675OR – Juniper Hills 8-11 PZ
R010XA675OR – Juniper Hills 8-11 PZ
Not as above
Sites usually found on gentler slopes associated with plains
R010XA659OR – Juniper Pumice Plains 8-11 PZ
R010XA659OR – Juniper Pumice Plains 8-11 PZ
Sites occur on steeper slopes associated with hills
Sites usually occur below 4600 feet in elevation
R010XA021OR – Juniper Shallow Pumice Hills 10-12 PZ
R010XA021OR – Juniper Shallow Pumice Hills 10-12 PZ
Sites usually occur above 4600 feet in elevation
R010XA673OR – Juniper Pumice Hills 8-11 PZ
R010XA673OR – Juniper Pumice Hills 8-11 PZ
Soil is very shallow over highly fractured bedrock, interspersed with areas of rock outcrop
Not as above
Soil moisture regime is aridic
R010XB057OR – JD Mahogany Rockland 9-12 PZ
R010XB057OR – JD Mahogany Rockland 9-12 PZ
Soil moisture regime is xeric
R010XB058OR – JD Mahogany Rockland 12-16 PZ
R010XB058OR – JD Mahogany Rockland 12-16 PZ
Sites occurring on north aspect slopes and soil temperature regime is mesic
Not as above
Soil moisture regime is aridic
Soil moisture regime is xeric
Soils are very shallow
R010XB065OR – JD Droughty Clayey North 9-12 PZ
R010XB065OR – JD Droughty Clayey North 9-12 PZ
Soils are shallow
R010XB035OR – JD Shallow North 9-12 PZ
R010XB035OR – JD Shallow North 9-12 PZ
Soils are moderately deep to deep
R010XB064OR – JD North 9-12 PZ
R010XB064OR – JD North 9-12 PZ
Soils are shallow
R010XB033OR – JD Shallow North 12-16 PZ
R010XB033OR – JD Shallow North 12-16 PZ
Soils are moderately deep to deep
R010XB070OR – JD North 12-16 PZ
R010XB070OR – JD North 12-16 PZ
Sites occurring on south aspect slopes and soil temperature regime is mesic
Not as above or sites that are not influenced by aspect
Soil moisture regime is aridic
Soil moisture regime is xeric
Soils are shallow
Soils are moderately deep to deep
Soils have greater than 35 percent clay content
R010XB051OR – JD Shallow South 9-12 PZ
R010XB051OR – JD Shallow South 9-12 PZ
Soils have less than 35 percent clay content
R010XB052OR – JD Droughty Shallow South 9-12 PZ
R010XB052OR – JD Droughty Shallow South 9-12 PZ
Soils are skeletal
R010XB041OR – JD Clayey South 9-12 PZ
R010XB041OR – JD Clayey South 9-12 PZ
Soils are not skeletal
Surface texture is a very cobbly clay loam over clay subsoils
R010XB043OR – JD Droughty Clayey South 9-12 PZ
R010XB043OR – JD Droughty Clayey South 9-12 PZ
Surface texture is a loam or gravelly loam over clay subsoils
R010XB044OR – JD Droughty South 9-12 PZ
R010XB044OR – JD Droughty South 9-12 PZ
Soils are shallow
R010XB047OR – JD Shallow South 12-16 PZ
R010XB047OR – JD Shallow South 12-16 PZ
Soils are moderately deep to deep
Surface soils have a rock fragment volume below 35 percent
Surface soils have a total cobble volume between 60 and 90 percent
R010XB048OR – JD Loamy South 12-16 PZ
R010XB048OR – JD Loamy South 12-16 PZ
Sites predominately occur above 3500 feet. Soils are loamy with surface shale volume between fifteen and thirty-five percent. Rock fragment volume typically increases with depth
R010XB046OR – JD Shrubby Mountain South 12-16 PZ
R010XB046OR – JD Shrubby Mountain South 12-16 PZ
Sites predominately occur below 4000 feet. Soil surface textures are cobbly clay loams
R010XB045OR – JD Clayey South 12-16 PZ
R010XB045OR – JD Clayey South 12-16 PZ
Soil temperature regime is mesic
Soil temperature regime is frigid. Soil moisture regime is xeric
R010XB083OR – JD Shrubby Shallow 12-16 PZ
R010XB083OR – JD Shrubby Shallow 12-16 PZ
Soil moisture regime is aridic
Soil moisture regime is xeric
Soils are shallow
R010XB023OR – JD Shallow 9-12 PZ
R010XB023OR – JD Shallow 9-12 PZ
Soils are moderately deep to deep
Soils contain greater than 35 percent clay
Soils contain less than thirty-five percent clay
Soil surface textures are clays with high shrink-swell potential
R010XB019OR – JD Gumbo 9-12 PZ
R010XB019OR – JD Gumbo 9-12 PZ
Soils have higher fragment amounts. Surface textures are stony clay loam to loam
R010XB022OR – JD Clayey 9-12 PZ
R010XB022OR – JD Clayey 9-12 PZ
Surface soil textures are fine to coarse sandy loams. Subsoils are often gravelly to very gravelly
R010XB025OR – JD Sandy Loam 9-12 PZ
R010XB025OR – JD Sandy Loam 9-12 PZ
Surface soil textures are loams sometimes with an ash component
R010XB034OR – JD Loamy 9-12 PZ
R010XB034OR – JD Loamy 9-12 PZ
Soils are shallow
R010XB031OR – JD Shallow 12-16 PZ
R010XB031OR – JD Shallow 12-16 PZ
Soils are moderately deep to deep
Surface textures are silt loams
Surface textures are cobbly to stony loams. Subsurface soils are very cobbly to very stony
R010XB027OR – JD Clayey 12-16 PZ
R010XB027OR – JD Clayey 12-16 PZ
Surface texture is most often a silt loam with no ashy textures. In the reference state, antelope bitterbrush is the dominant shrub and Idaho fescue is the dominant grass
R010XB013OR – JD Shrubby Loam 12-16 PZ
R010XB013OR – JD Shrubby Loam 12-16 PZ
Surface texture is most often a loam sometimes with an ash influence. In the reference state, basin big sagebrush is the dominant shrub and bluebunch wheatgrass is the dominant grass
R010XB030OR – JD Loamy 12-16 PZ
R010XB030OR – JD Loamy 12-16 PZ
Sites occurring on north aspect slopes
R010XB081OR – Blue Mountain Foothills, Claypan North 12-16 PZ
R010XB081OR – Blue Mountain Foothills, Claypan North 12-16 PZ
Sites occurring on south aspect slopes
R010XB096OR – Blue Mountain Foothills, Claypan South 12-16 PZ
R010XB096OR – Blue Mountain Foothills, Claypan South 12-16 PZ
Sites that are not influenced by aspect
Soil moisture regime is aridic
R010XB029OR – Blue Mountain Foothills, Claypan 9-12 PZ
R010XB029OR – Blue Mountain Foothills, Claypan 9-12 PZ
Soil moisture regime is xeric
The surface soil is often three to six inches thick over a non-fractured substratum. In the reference state, little sagebrush is the dominant shrub with very low cover of antelope bitterbrush and yellow rabbitbrush
R010XB080OR – Blue Mountain Foothills, Claypan 12-16 PZ
R010XB080OR – Blue Mountain Foothills, Claypan 12-16 PZ
The surface soil is often five to ten inches thick over a fractured substratum. In the reference state, antelope bitterbrush is dominant with little sagebrush being subdominant
R010XB082OR – JD Shrubby Claypan 12-16 PZ
R010XB082OR – JD Shrubby Claypan 12-16 PZ
Soils are very shallow over highly fractured bedrock, interspersed with areas of rock outcrop
R010XC059OR – SR Mahogany Rockland 12+ PZ
R010XC059OR – SR Mahogany Rockland 12+ PZ
Not as above
Soils are very shallow over lithic bedrock
Not as above
Sites occur below 4000 feet elevation. Surface fragment cover is typically around 60 percent and extremely gravelly subsoil
R010XB032OR – JD Very Shallow 12-16 PZ
R010XB032OR – JD Very Shallow 12-16 PZ
Sites occur above 4000 feet elevation. Surface fragment cover is typically less than 30 percent
R010XC039OR – SR Very Shallow 12-16 PZ
R010XC039OR – SR Very Shallow 12-16 PZ
Soils are very shallow over sediments
R010XY015OR – Buckwheat Scabland 9-12 PZ
R010XY015OR – Buckwheat Scabland 9-12 PZ
Not as above
Sites occurring on north aspect slopes
Not as above
Soils are shallow
R010XC075OR – SR Mountain Shallow North 12-16 PZ
R010XC075OR – SR Mountain Shallow North 12-16 PZ
Soils are moderately deep to deep
Surface soils have an ashy influence with textures being ashy loam to ashy loamy sand
R010XB085OR – JD Mountain North 12-16 PZ
R010XB085OR – JD Mountain North 12-16 PZ
Soil surface not ash influenced
Surface soils are often a shaly loam with very shaly loam to gravelly clay loam subsoils
R010XB071OR – JD Shrubby Mountain North 12-16 PZ
R010XB071OR – JD Shrubby Mountain North 12-16 PZ
Surface soil textures are silt loam to clay loam and subsoils are clay loams
R010XC066OR – SR Mountain North 12-16 PZ
R010XC066OR – SR Mountain North 12-16 PZ
Sites occurring on south aspect slopes
Not as above or sites that are not influenced by aspect
Soils are shallow
R010XC054OR – SR Mountain Shallow South 12-16 PZ
R010XC054OR – SR Mountain Shallow South 12-16 PZ
Soils are moderately deep to deep
R010XC047OR – SR Mountain South 12-16 PZ
R010XC047OR – SR Mountain South 12-16 PZ
Soils are shallow
Soils are moderately deep to deep
Soils are clayey. Surface textures are stony silt loams with clay loams and clays in subsoils
R010XC037OR – SR Mountain Shallow 12-16 PZ
R010XC037OR – SR Mountain Shallow 12-16 PZ
Surfaces are very gravelly to very stony and may be ashy. Soils are loamy formed predominately from tuffaceous materials
R010XB086OR – JD Shrubby Mountain Shallow 12-16 PZ
R010XB086OR – JD Shrubby Mountain Shallow 12-16 PZ
Family particle size class is clayey
Family particle size class is loamy
Surface texture is a silt loam to silty clay loam
R010XC032OR – SR Mountain 12-16 PZ
R010XC032OR – SR Mountain 12-16 PZ
Surface texture is gravelly loam to very stony loam
R010XB028OR – JD Shrubby Mountain 12-16 PZ
R010XB028OR – JD Shrubby Mountain 12-16 PZ
Soils are moderately deep over fragmented tuffaceous bedrock. In the reference condition, curl-leaf mountain mahogany is the dominant shrub
R010XC082OR – SR Dry Pine 14-16 PZ
R010XC082OR – SR Dry Pine 14-16 PZ
Soils are moderately deep over bedrock. In the reference state, mountain big sagebrush is the dominant shrub and western juniper may be present in low amounts
R010XC080OR – SR Mahogany Mountain Loam 14-18 PZ
R010XC080OR – SR Mahogany Mountain Loam 14-18 PZ
Soil is very shallow to moderately deep over highly fractured bedrock with surface soils of cobbly to stony loams. Areas interspersed with rock outcrops.
Not as above
Sites occurring on moderate to very steep slopes of 12 to 60 percent on canyon walls and mountain side slopes. Western juniper is often the dominant tree species.
R010XC059OR – SR Mahogany Rockland 12+ PZ
R010XC059OR – SR Mahogany Rockland 12+ PZ
Sites occurring on nearly level to moderately steep slopes of 2 to 20 percent on tablelands and mountain plateaus. Ponderosa pine is often the dominant tree species.
R010XC080OR – SR Mahogany Mountain Loam 14-18 PZ
R010XC080OR – SR Mahogany Mountain Loam 14-18 PZ
Soil is very shallow over lithic bedrock
Not as above
Precipitation range is 12 to 16 inches
Soil temperature regime is frigid, precipitation range is 16 to 20 inches
R010XC040OR – SR Very Shallow 16-20 PZ
R010XC040OR – SR Very Shallow 16-20 PZ
Soil temperature regime is mesic to frigid near mesic, precipitation range is 12 to 16 inches
R010XC041OR – SR Very Shallow Rockland 12-16 PZ
R010XC041OR – SR Very Shallow Rockland 12-16 PZ
Soil temperature regime is frigid to mesic near frigid.
Underlying bedrock is highly fractured
R010XC039OR – SR Very Shallow 12-16 PZ
R010XC039OR – SR Very Shallow 12-16 PZ
Not as above
R010XC042OR – SR Juniper Tableland 12-16 PZ
R010XC042OR – SR Juniper Tableland 12-16 PZ
Sites occurring on north aspect slopes. Sites have a frigid soil temperature regime and a xeric soil moisture regime.
Not as above
Precipitation range is 12 to 16 inches
Precipitation amount is greater than 16 inches
Soil is shallow
R010XC075OR – SR Mountain Shallow North 12-16 PZ
R010XC075OR – SR Mountain Shallow North 12-16 PZ
Soil is moderately deep to deep
R010XC066OR – SR Mountain North 12-16 PZ
R010XC066OR – SR Mountain North 12-16 PZ
Site occurs above 5000 feet
Site occurs below 5000 feet
R010XC067OR – SR Shrubby Mountain North 16-20 PZ
R010XC067OR – SR Shrubby Mountain North 16-20 PZ
Surface soil is a silt loam over a silt loam to stony clay loam subsoil. Often occurs above 6000 feet elevation. Sites associated with higher annual production and trees such as western juniper and ponderosa pine
R010XC069OR – SR Mountain North 16-20 PZ
R010XC069OR – SR Mountain North 16-20 PZ
Surface layer a loam to very gravelly loam over a very gravelly loam to gravelly sandy loam subsoil. Often occurring from 5000 to 6000 feet in elevation and not normally associated with tree species
R010XC053OR – SR High Mountain Loam 18+ PZ
R010XC053OR – SR High Mountain Loam 18+ PZ
Sites occurring on south aspect slopes
Not as above
Soil temperature regime is mesic and soil moisture regime is aridic
R010XC044OR – SR South Schist 9-12 PZ
R010XC044OR – SR South Schist 9-12 PZ
Soil moisture regime is xeric.
Soil temperature regime is transitional between mesic and frigid.
Soil temperature regime is frigid.
Soils are shallow to moderately deep
R010XC055OR – SR Mountain Shallow South 16-20 PZ
R010XC055OR – SR Mountain Shallow South 16-20 PZ
Soils are moderately deep to deep
Precipitation range is 12 to 16 inches
R010XC047OR – SR Mountain South 12-16 PZ
R010XC047OR – SR Mountain South 12-16 PZ
Precipitation range is 16 to 20 inches
R010XC049OR – SR Shrubby Mountain South 16-20 PZ
R010XC049OR – SR Shrubby Mountain South 16-20 PZ
Site predominantly occurs on south exposures of canyon walls and the backslopes of tablelands and mountain plateaus
R010XC051OR – SR High Mountain South 16-20 PZ
R010XC051OR – SR High Mountain South 16-20 PZ
Site occurs on tops and shoulders of ridges as well as north-facing mountain back slopes. Slopes may be up to 60 percent but more often range from 2 to 35 percent
R010XC053OR – SR High Mountain Loam 18+ PZ
R010XC053OR – SR High Mountain Loam 18+ PZ
Soil temperature regime is mesic and soil moisture regime is aridic
R010XC030OR – SR Cool 9-12 PZ
R010XC030OR – SR Cool 9-12 PZ
Soil moisture regime is xeric
Soil temperature regime is transitional between mesic and frigid.
Soil temperature regime is frigid
Precipitation range is 12 to 16 inches
Precipitation range is 16 to 20 inches
R010XC034OR – SR Shrubby Mountain Loam 16-20 PZ
R010XC034OR – SR Shrubby Mountain Loam 16-20 PZ
Sites occur below 4000 feet
R010XC033OR – SR Cool 12-16 PZ
R010XC033OR – SR Cool 12-16 PZ
Sites occur above 4000 feet
Surface texture is a silt or clay loam with very low, if any, surface fragment cover
R010XC028OR – SR Shrubby Cool 12-16 PZ
R010XC028OR – SR Shrubby Cool 12-16 PZ
Surface texture is a very cobbly, very stony, or gravelly loam with approximately 10 to 20 percent surface gravel cover and 4 to 27 percent surface cobble cover
R010XB028OR – JD Shrubby Mountain 12-16 PZ
R010XB028OR – JD Shrubby Mountain 12-16 PZ
Precipitation range is 12 to 16 inches
Precipitation range is greater than 16 inches
Soils are shallow
R010XC037OR – SR Mountain Shallow 12-16 PZ
R010XC037OR – SR Mountain Shallow 12-16 PZ
Soils are moderately deep to deep
R010XC032OR – SR Mountain 12-16 PZ
R010XC032OR – SR Mountain 12-16 PZ
Site typically occurs between 4000 and 5700 feet on tablelands and mountain plateaus
R010XC082OR – SR Dry Pine 14-16 PZ
R010XC082OR – SR Dry Pine 14-16 PZ
Site typically occurs between 6000 and 7500 feet on mountain ridges and plateaus
R010XC070OR – SR Mountain 16-20 PZ
R010XC070OR – SR Mountain 16-20 PZ
Soils are very shallow over lithic bedrock
R010XC038OR – SR Very Shallow 9-12 PZ
R010XC038OR – SR Very Shallow 9-12 PZ
Not as above
Soils are very shallow over paralithic contact
R010XC057OR – SR Shallow Escarpment 9-12 PZ
R010XC057OR – SR Shallow Escarpment 9-12 PZ
Not as above
Sites occurring on north aspect slopes
Not as above
Soil temperature regime is mesic. Soil moisture regime is aridic
Soil temperature regime is transitional between cool mesic to frigid. Soil moisture regime is xeric
R010XC068OR – SR Cool Mountain North 12-16 PZ
R010XC068OR – SR Cool Mountain North 12-16 PZ
Elevation typically between 3200 and 4500 feet with less than 100 frost free days. Soil temperature regime is mesic to near frigid
R010XC065OR – SR Cool North 9-12 PZ
R010XC065OR – SR Cool North 9-12 PZ
Not as above
Site predominately found on mid elevation terraces on droughty sites. Soil clay content between 18 and 35 percent
R010XC063OR – SR Droughty North 9-12 PZ
R010XC063OR – SR Droughty North 9-12 PZ
Soil clay content above 35 percent
R010XC064OR – SR North 9-12 PZ
R010XC064OR – SR North 9-12 PZ
Sites occurring on south aspect slopes, soil temperature regime is mesic and soil moisture regime is aridic
Not as above or sites that are not influenced by aspect
Soils range from shallow to deep, occur on unstable landscape positions and have little structural development
R010XC056OR – SR Terrace Escarpment 9-12 PZ
R010XC056OR – SR Terrace Escarpment 9-12 PZ
Soils are shallow
Soils are moderately deep to deep
R010XC043OR – SR South 9-12 PZ
R010XC043OR – SR South 9-12 PZ
Soils are a stony loam to gravelly clay loam about six inches thick
BX010X00C050 – Shallow South 9-12 PZ Snake River Warm Plains
BX010X00C050 – Shallow South 9-12 PZ Snake River Warm Plains
Soils are generally shallow with areas of rock outcrop. The surface layer is a channery loam about three inches thick with a very channery loam subsoil
R010XC052OR – SR Shallow South Schist 9-12 PZ
R010XC052OR – SR Shallow South Schist 9-12 PZ
Soil temperature regime is mesic. Soil moisture regime is aridic
Soil temperature regime is transitional between mesic and frigid. Soil moisture regime is xeric
R010XC033OR – SR Cool 12-16 PZ
R010XC033OR – SR Cool 12-16 PZ
Soils are shallow
Soils are moderately deep to deep
Sites occur on gentle slopes of 2 to 12 percent on terraces, tablelands, and rolling uplands
Sites occur on steep slopes of 2 to 40 percent on hillsides, escarpments, and eroded hills
R010XC057OR – SR Shallow Escarpment 9-12 PZ
R010XC057OR – SR Shallow Escarpment 9-12 PZ
Typically occurs between 2000 to 3500 feet in elevation
R010XC035OR – SR Shallow 9-12 PZ
R010XC035OR – SR Shallow 9-12 PZ
Typically occurs between 3500 to 4200 feet in elevation
R010XC036OR – SR Shallow Cool 9-12 PZ
R010XC036OR – SR Shallow Cool 9-12 PZ
Soils are clayey. Typically, both the surface and subsoil are clays with high shrink well potentials. Soil churning is prevalent.
R010XC018OR – SR Adobeland 9-12 PZ
R010XC018OR – SR Adobeland 9-12 PZ
Soils are not as described above
Soil clay above 35 percent
Soil clay below 35 percent
Soil temperature regime is mesic to near frigid. Typical elevation between 2700 and 4400 feet. Site averages less than 100 frost free days. Plant communities are typically dominated by Wyoming big sagebrush and Idaho fescue.
R010XC030OR – SR Cool 9-12 PZ
R010XC030OR – SR Cool 9-12 PZ
Soil temperature regime is mesic. Elevations range from 2000 to 3500 feet. Site averages approximately 140 frost free days per year. Plant communities are typically dominated by Wyoming big sagebrush and bluebunch wheatgrass
R010XC021OR – SR Clayey 9-12 PZ
R010XC021OR – SR Clayey 9-12 PZ
Soil clay above 18 percent
Soil clay below 18 percent
R010XC025OR – SR Sandy 9-12 PZ
R010XC025OR – SR Sandy 9-12 PZ
Soils are made up of greater than 40 percent silt, often contain a cambic horizon, and coarse loamy particle size class. In the reference state, wild crab apple is present
R010XC020OR – SR Loamy 9-12 PZ
R010XC020OR – SR Loamy 9-12 PZ
Soils are made up of less than 40 percent silt, often contain an argillic horizon, and fine to fine loamy particle size class. In the reference state, wild crab apple is not present
BX010X00C022 – Silty 9-12 PZ Snake River Warm Plains
BX010X00C022 – Silty 9-12 PZ Snake River Warm Plains
Long term average mean annual precipitation
- No filter
- 20 – 25cm (8 – 10in)
- 25 – 30cm (10 – 12in)
- 30 – 35cm (12 – 14in)
- 35 – 40cm (14 – 16in)
- 40 – 50cm (16 – 20in)
- 50 – 60cm (20 – 24in)
- 60 – 80cm (24 – 31in)
—
cm
Long term average frost free days
- No filter
- 0 – 30days
- 30 – 50days
- 50 – 70days
- 70 – 90days
- 90 – 110days
- 110 – 130days
- 130 – 150days
- 150 – 170days
- 170 – 190days
—
days
- No filter
- 0 – 200m (0 – 700ft)
- 200 – 400m (700 – 1300ft)
- 400 – 600m (1300 – 2000ft)
- 600 – 800m (2000 – 2600ft)
- 800 – 1000m (2600 – 3300ft)
- 1000 – 1200m (3300 – 3900ft)
- 1200 – 1400m (3900 – 4600ft)
- 1400 – 1600m (4600 – 5200ft)
- 1600 – 1800m (5200 – 5900ft)
- 1800 – 2000m (5900 – 6600ft)
- 2000 – 2200m (6600 – 7200ft)
- 2200 – 2400m (7200 – 7900ft)
- 2400 – 2600m (7900 – 8500ft)
- 2600 – 2800m (8500 – 9800ft)
—
m
- No filter
- 0 – 3%
- 3 – 5%
- 5 – 10%
- 10 – 15%
- 15 – 20%
- 20 – 25%
- 25 – 30%
- 30 – 35%
- 35 – 40%
- 40 – 45%
- 45 – 50%
- 50 – 60%
- 60 – 70%
- 70 – 80%
- 80 – 90%
—
%
- No filter
- Alluvial fan
- Basin floor
- Braided stream
- Butte
- Canyon
- Canyon wall
- Channel
- Depression
- Drainageway
- Escarpment
- Fan
- Fan remnant
- Fen
- Flood plain
- Flood-plain step
- Hill
- Hillside
- Hillslope
- Kipuka
- Lakeshore
- Landslide
- Lava flow
- Lava plain
- Lava plateau
- Marsh
- Mesa
- Mountain
- Mountain slope
- Mountain valley
- Oxbow
- Plain
- Plateau
- Ravine
- Ridge
- Rim
- Slough
- Slump
- Stack (geom.)
- Stream
- Stream terrace
- Structural bench
- Swale
- Terrace
- Toe
- Valley
- Valley floor
- Valley side
- No filter
- Andesite
- Basalt
- Diatomite
- Diorite
- Granodiorite
- Graywacke
- Igneous, unspecified
- Latite
- Limestone, unspecified
- Metavolcanics
- Monzonite
- Quartz-diorite
- Quartzite
- Rhyolite
- Sandstone, unspecified
- Sandstone, volcanic
- Schist, biotite
- Sedimentary, unspecified
- Serpentinite
- Shale, unspecified
- Siltstone, calcareous
- Siltstone, unspecified
- Tuff, acidic
- Tuff, unspecified
- Tuff, welded
- Volcanic and sedimentary
- Volcanic breccia, unspecified
- Volcanic, unspecified
- No filter
- Alluvium
- Cinders
- Colluvium
- Eolian deposits
- Flow deposits
- Glaciofluvial deposits
- Lacustrine deposits
- Loess
- Organic, mossy material
- Overbank deposits
- Residuum
- Tephra
- Volcanic ash
- Volcanic ash, basic
Soil surface texture
- No filter
- Clay
- Clay loam
- Coarse sandy loam
- Fine sandy loam
- Loam
- Loamy coarse sand
- Loamy fine sand
- Loamy sand
- Sand
- Sandy clay loam
- Silty clay
- Silty clay loam
- Silt loam
- Sandy loam
- Very fine sandy loam
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Ecological site keys
MLRA10X
I.
Sites occurring in east of the Snake River.
A.
Occurring on the Upper Snake River Lava Plains and Hills
B.
Occurring the Footslopes and Plains of the Big and Little Wood Rivers
II.
Sites occurring west of the Snake River.
A.
Sites occurring on fluvial landforms including stream channels, terraces, secondary terraces, meadows, bottoms, swales, and fans. These sites occur across LRU boundaries.
B.
Not as above
1
Sites occurring in the Madras Plains LRU. Characterized by deeper soils on nearly level plateaus. Most areas are row cropped. The dominant area for this unit is the Agency Plain. The dominant soils are the Agency and Madras soil series. Surface texture is sandy loam or loam. The soils lack the strong volcanic ash influence typical of the Pumice Lava Plains LRU. Temperature regime is mesic; moisture regime is aridic.
2
Not as above
i.
Sites occurring in the Pumice Lava Plains LRU. Characterized by moderately deep and shallow soils formed in ash from Mt. Mazama over basalt. Most areas are native rangelands or used for irrigated pasture or hayland. Slopes are nearly level to undulating. The dominant soils are Deschutes and Deskamp. Texture is sandy loam and loamy sand throughout the profile. Temperature regime is mesic; moisture regime is aridic.
ii.
Not as above
a.
Sites occurring in the John Day Sediments LRU. This unit is characterized by rangeland soils on hills or mountains associated with the John Day/Clarno Formation and/or basalt. Temperature regime is dominantly mesic; moisture regime is aridic and xeric. (warm climate).
b.
Not as above
1)
Sites occurring in the John Day Mountain Foothills LRU. Characterized by rangeland soils on hills or mountains associated with basalt. Temperature regime is frigid; moisture regime is xeric. (cool moist climate) Soils are commonly influenced by Mt. Mazama ash in the surface. Textures are dominantly loams and clays.
2)
Not as above
a)
Sites occurring in the Snake River Mountain Foothills LRU. Characterized by rangeland soils on hills or mountains associated with basalt. Temperature regime is frigid; moisture regime is xeric. (cool moist climate) Textures are dominantly loams and silt loams or silty clay loams.
b)
Not as above
(1)
Snake River Warm Plains LRU. Located between Oregon's Blue and Wallowa Mountains and the northwestern Snake River Plain. Characterized by soils on hills and mountains associated with basalt and exposed tuffaceous sediments. Plants are subject to wide temperature ranges, high evapotranspiration, and high early-season moisture stress. Temperature regime is mesic and the moisture regime is aridic. Mean annual precipitation is 9 to 12 inches. (warm dry)
Fluvial Landforms
II.
Not as above
A.
Sites occurring along the active channel of a perennial or intermittent stream to riparian sites
1
Soil temperature regime is mesic
2
Soil temperature regimes is mesic near frigid or cooler
ii.
Not as above
a.
Soil temperature regime is mesic near frigid to frigid near mesic
... R010XY012OR – Booth-Yellow Willow Riparian
B.
Not as above
1
Site occurs on floodplains of perennial streams and rivers, near channels occupying primary terraces to meadows
i.
Soil temperature regime is mesic to frigid near mesic
a.
Water table is within 12 inches of the soil surface March through July
... R010XY003OR – Wet Meadow
b.
Water table is deeper than 12 inches of the soil surface March through July
ii.
Soil temperature regime is frigid to cryic
a.
Water table is within 12 inches of the soil surface March through July
... R010XY001OR – Cold Wet Meadow
b.
Water table is deeper than 12 inches of the soil surface March through July
2
Not as above
i.
Site occurs on floodplains of perennial streams and rivers, occupying secondary terraces to bottoms
a.
Soil temperature regime is mesic to frigid near mesic
2)
Soil does not have sodic properties
ii)
Soils are not sandy in the particle control section
ii.
Not as above
a.
Site occurs adjacent to and on floodplains or ephemeral streams, upper end of drainages to swales
1)
Soil temperature regime is mesic to frigid near mesic
2)
Soil temperature regime is frigid and mesic near frigid
ii)
Soil moisture regime is xeric
(a)
Sites have higher available water holding capacities (8 to 10 inches). In the reference state, basin wildrye is the dominant grass species and has higher production than the Dry Mountain Swale site
... R010XY117OR – Mountain Swale 12-16 PZ
(b)
Sites have lower plant available water (3 to 6 inches). In the reference state, Idaho fescue is the dominant grass and has lower production than the Mountain Swale sites
... R010XY119OR – Dry Mountain Swale 12-16 PZ
b.
Not as above
1)
Site occurs on mountain side slopes and plateaus in areas receiving additional subsurface moisture from ephemeral subsurface flows
... R010XY230OR – Aspen Upland 12-18 PZ
2)
Not as above or sites occurring on alluvial fans
i)
Precipitation 9 to 12 inches, aridic soil moisture regime
(b)
Soil does not have sodic properties
(1)
Typically occurring on lower fan toeslope or terrace positions, hydrologically connected to stream networks
... R010XY120OR – Loamy Fan 9-12 PZ
(2)
Not as above
(i)
Soils are clays with very fine particle size classes
... R010XY121OR – Droughty Clayey Fan 9-12 PZ
(ii)
Soils are typically loamy-skeletal (sometimes fine) particle size classes
... R010XY153OR – Droughty Fan 9-12 PZ
ii)
Precipitation 12 to 16 inches, xeric soil moisture regime
... R010XY125OR – Gravelly Fan 12-16 PZ
Madras Plains LRU
I.
Sites occurring on north aspect slopes
II.
Not as above
B.
Not as above or sites that are not influenced by aspect
1
Ecosites associated with buttes and often slopes greater than 40 percent
... R010XA014OR – Juniper Cinder Hills 10-12 PZ
2
Not as above
i)
Sites associated with swales, fans, or terraces
a)
Sites occur on slopes greater than 30 percent
... R010XA002OR – Juniper Shrubby Pumice Hills 8-10 PZ
ii)
Sites associated with plateaus and ridges
a)
Particle size class is clayey to fine loamy but not skeletal or ashy
... R010XA001OR – Loamy 8-10 PZ
b)
Particle size class is most often coarse to fine loamy or loamy skeletal but not clayey
1)
Particle size class is often fine to fine loamy. Soils have a water holding potential of three to six inches leading to higher annual production and higher cover of western juniper compared to Shrubby Loam 8 to 12 precipitation zone sites
... R010XA018OR – Juniper Shrubby Loam 10-12 PZ
2)
Particle size class is often coarse loamy to loamy skeletal. Soils have a water holding potential of two to four inches leading to lower annual production and lower western juniper cover than the Juniper Shrubby Loam 10 to 12 precipitation zone sites
... R010XA019OR – Shrubby Loam 8-12 PZ
Pumice Lava Plains LRU
I.
Site is on a cinder butte. Soils are ash over scoriaceous cinders
... R010XA014OR – Juniper Cinder Hills 10-12 PZ
II.
Not as above
A.
Sites occurring on north aspect slopes
1
Soil temperature regime is mesic
i.
Soils are less than 20 inches deep and contain more than 35 percent rock fragments
... R010XA025OR – Juniper Shallow North 10-12 PZ
ii.
Soils are deeper than 20 inches
B.
Not as above
1
Sites occurring on south aspect slopes. Soil temperature regime is mesic
... R010XA007OR – Juniper Pumice South 9-12 PZ
2
Not as above or sites that are not influenced by aspect
i.
Soil temperature regime is mesic
a.
Soils are very shallow or shallow
1
Soils are volcanic ash/pumice over exposed lava flows and lava blisters or small knolls dispersed across lava plains
i)
Sites occur in eight to ten inch precipitation zones
... R010XA022OR – Juniper Lava Blisters 8-10 PZ
ii)
Sites occur in 10 to 12 inch precipitation zones
... R010XA023OR – Juniper Shrubby Lava Blisters 10-12 PZ
b.
Soils are moderately deep to deep
1
Soils are loamy with less than thirty-five percent clay and greater than fifteen percent sand
i)
Particle size class is often coarse loamy to loamy skeletal. Soils have a water holding potential of two to four inches leading to lower annual production and lower western juniper cover than the Juniper Shrubby Loam 10 to 12 precipitation zone sites
... R010XA019OR – Shrubby Loam 8-12 PZ
ii)
Particle size class is often fine to fine loamy. Soils have a water holding potential of three to six inches leading to higher annual production and higher cover of western juniper compared to Shrubby Loam 8 to 12 precipitation zone sites
... R010XA018OR – Juniper Shrubby Loam 10-12 PZ
2
Soils are sandy with less than eighteen percent clay and soil textures including sand or loamy sand
i)
Sites occur in areas that receive eight to ten inches of precipitation annually
... R010XA027OR – Juniper Pumice Flat 8-10 PZ
ii)
Sites occur in areas that receive ten to twelve inches of precipitation annually
... R010XA009OR – Juniper Shrubby Pumice Flat 10-12 PZ
ii.
Soil temperature regime is frigid
a.
Sites with surface fragment cover over 80 percent usually consisting of small channers
... R010XA675OR – Juniper Hills 8-11 PZ
b.
Not as above
1
Sites usually found on gentler slopes associated with plains
... R010XA659OR – Juniper Pumice Plains 8-11 PZ
2
Sites occur on steeper slopes associated with hills
i)
Sites usually occur below 4600 feet in elevation
... R010XA021OR – Juniper Shallow Pumice Hills 10-12 PZ
John Day Sediments LRU
I
Soil has an abrupt textural change within 10 inches of the surface (well-developed claypan)
... R010XB024OR – JD Warm Ashy Claypan 9-12 PZ
II
Not as above
A
Soil is very shallow over highly fractured bedrock, interspersed with areas of rock outcrop
B
Not as above
1
Sites occurring on north aspect slopes and soil temperature regime is mesic
i.
Soil moisture regime is aridic
ii.
Soil moisture regime is xeric
2
Not as above
i.
Sites occurring on south aspect slopes and soil temperature regime is mesic
a.
Soil moisture regime is aridic
1
Soils are shallow
ii)
Soils have less than 35 percent clay content
... R010XB052OR – JD Droughty Shallow South 9-12 PZ
2
Soils are moderately deep to deep
ii)
Soils are not skeletal
a)
Surface texture is a very cobbly clay loam over clay subsoils
... R010XB043OR – JD Droughty Clayey South 9-12 PZ
b)
Surface texture is a loam or gravelly loam over clay subsoils
... R010XB044OR – JD Droughty South 9-12 PZ
b.
Soil moisture regime is xeric
2
Soils are moderately deep to deep
i)
Surface soils have a rock fragment volume below 35 percent
a)
Sites predominately occur above 3500 feet. Soils are loamy with surface shale volume between fifteen and thirty-five percent. Rock fragment volume typically increases with depth
... R010XB046OR – JD Shrubby Mountain South 12-16 PZ
b)
Sites predominately occur below 4000 feet. Soil surface textures are cobbly clay loams
... R010XB045OR – JD Clayey South 12-16 PZ
ii)
Surface soils have a total cobble volume between 60 and 90 percent
... R010XB048OR – JD Loamy South 12-16 PZ
ii.
Not as above or sites that are not influenced by aspect
a.
Soil temperature regime is mesic
1
Soil moisture regime is aridic
ii)
Soils are moderately deep to deep
a)
Soils contain greater than 35 percent clay
1)
Soil surface textures are clays with high shrink-swell potential
... R010XB019OR – JD Gumbo 9-12 PZ
2)
Soils have higher fragment amounts. Surface textures are stony clay loam to loam
... R010XB022OR – JD Clayey 9-12 PZ
b)
Soils contain less than thirty-five percent clay
1)
Surface soil textures are fine to coarse sandy loams. Subsoils are often gravelly to very gravelly
... R010XB025OR – JD Sandy Loam 9-12 PZ
2)
Surface soil textures are loams sometimes with an ash component
... R010XB034OR – JD Loamy 9-12 PZ
2
Soil moisture regime is xeric
ii)
Soils are moderately deep to deep
a)
Surface textures are silt loams
1)
Surface texture is most often a silt loam with no ashy textures. In the reference state, antelope bitterbrush is the dominant shrub and Idaho fescue is the dominant grass
... R010XB013OR – JD Shrubby Loam 12-16 PZ
2)
Surface texture is most often a loam sometimes with an ash influence. In the reference state, basin big sagebrush is the dominant shrub and bluebunch wheatgrass is the dominant grass
... R010XB030OR – JD Loamy 12-16 PZ
b)
Surface textures are cobbly to stony loams. Subsurface soils are very cobbly to very stony
... R010XB027OR – JD Clayey 12-16 PZ
b.
Soil temperature regime is frigid. Soil moisture regime is xeric
... R010XB083OR – JD Shrubby Shallow 12-16 PZ
John Day Mountain Foothills LRU
I.
Soil has an abrupt textural change within 10 inches of the surface (well-developed claypan)
A.
Sites occurring on north aspect slopes
... R010XB081OR – Blue Mountain Foothills, Claypan North 12-16 PZ
B.
Sites occurring on south aspect slopes
... R010XB096OR – Blue Mountain Foothills, Claypan South 12-16 PZ
C.
Sites that are not influenced by aspect
2
Soil moisture regime is xeric
i.
The surface soil is often three to six inches thick over a non-fractured substratum. In the reference state, little sagebrush is the dominant shrub with very low cover of antelope bitterbrush and yellow rabbitbrush
... R010XB080OR – Blue Mountain Foothills, Claypan 12-16 PZ
ii.
The surface soil is often five to ten inches thick over a fractured substratum. In the reference state, antelope bitterbrush is dominant with little sagebrush being subdominant
... R010XB082OR – JD Shrubby Claypan 12-16 PZ
II.
Not as above
A.
Soils are very shallow over highly fractured bedrock, interspersed with areas of rock outcrop
... R010XC059OR – SR Mahogany Rockland 12+ PZ
B.
Not as above
1
Soils are very shallow over lithic bedrock
i.
Sites occur below 4000 feet elevation. Surface fragment cover is typically around 60 percent and extremely gravelly subsoil
... R010XB032OR – JD Very Shallow 12-16 PZ
ii.
Sites occur above 4000 feet elevation. Surface fragment cover is typically less than 30 percent
... R010XC039OR – SR Very Shallow 12-16 PZ
2
Not as above
ii.
Not as above
a.
Sites occurring on north aspect slopes
2)
Soils are moderately deep to deep
i)
Surface soils have an ashy influence with textures being ashy loam to ashy loamy sand
... R010XB085OR – JD Mountain North 12-16 PZ
ii)
Soil surface not ash influenced
a)
Surface soils are often a shaly loam with very shaly loam to gravelly clay loam subsoils
... R010XB071OR – JD Shrubby Mountain North 12-16 PZ
b)
Surface soil textures are silt loam to clay loam and subsoils are clay loams
... R010XC066OR – SR Mountain North 12-16 PZ
b.
Not as above
1)
Sites occurring on south aspect slopes
2)
Not as above or sites that are not influenced by aspect
i)
Soils are shallow
a)
Soils are clayey. Surface textures are stony silt loams with clay loams and clays in subsoils
... R010XC037OR – SR Mountain Shallow 12-16 PZ
b)
Surfaces are very gravelly to very stony and may be ashy. Soils are loamy formed predominately from tuffaceous materials
... R010XB086OR – JD Shrubby Mountain Shallow 12-16 PZ
ii)
Soils are moderately deep to deep
a)
Family particle size class is clayey
(2)
Surface texture is gravelly loam to very stony loam
... R010XB028OR – JD Shrubby Mountain 12-16 PZ
b)
Family particle size class is loamy
(1)
Soils are moderately deep over fragmented tuffaceous bedrock. In the reference condition, curl-leaf mountain mahogany is the dominant shrub
... R010XC082OR – SR Dry Pine 14-16 PZ
(2)
Soils are moderately deep over bedrock. In the reference state, mountain big sagebrush is the dominant shrub and western juniper may be present in low amounts
... R010XC080OR – SR Mahogany Mountain Loam 14-18 PZ
Snake River Mountain Foothills LRU
I.
Soil has an abrupt textural change within 10 inches of the surface (well-developed claypan)
... R010XB029OR – Blue Mountain Foothills, Claypan 9-12 PZ
II.
Not as above
A.
Soil is very shallow to moderately deep over highly fractured bedrock with surface soils of cobbly to stony loams. Areas interspersed with rock outcrops.
1
Sites occurring on moderate to very steep slopes of 12 to 60 percent on canyon walls and mountain side slopes. Western juniper is often the dominant tree species.
... R010XC059OR – SR Mahogany Rockland 12+ PZ
2
Sites occurring on nearly level to moderately steep slopes of 2 to 20 percent on tablelands and mountain plateaus. Ponderosa pine is often the dominant tree species.
... R010XC080OR – SR Mahogany Mountain Loam 14-18 PZ
B.
Not as above
1
Soil is very shallow over lithic bedrock
i.
Precipitation range is 12 to 16 inches
a.
Soil temperature regime is mesic to frigid near mesic, precipitation range is 12 to 16 inches
... R010XC041OR – SR Very Shallow Rockland 12-16 PZ
b.
Soil temperature regime is frigid to mesic near frigid.
ii.
Soil temperature regime is frigid, precipitation range is 16 to 20 inches
... R010XC040OR – SR Very Shallow 16-20 PZ
2
Not as above
i.
Sites occurring on north aspect slopes. Sites have a frigid soil temperature regime and a xeric soil moisture regime.
a.
Precipitation range is 12 to 16 inches
b.
Precipitation amount is greater than 16 inches
1
Site occurs above 5000 feet
i)
Surface soil is a silt loam over a silt loam to stony clay loam subsoil. Often occurs above 6000 feet elevation. Sites associated with higher annual production and trees such as western juniper and ponderosa pine
... R010XC069OR – SR Mountain North 16-20 PZ
ii)
Surface layer a loam to very gravelly loam over a very gravelly loam to gravelly sandy loam subsoil. Often occurring from 5000 to 6000 feet in elevation and not normally associated with tree species
... R010XC053OR – SR High Mountain Loam 18+ PZ
ii.
Not as above
a.
Sites occurring on south aspect slopes
1
Soil temperature regime is mesic and soil moisture regime is aridic
... R010XC044OR – SR South Schist 9-12 PZ
2
Soil moisture regime is xeric.
i)
Soil temperature regime is transitional between mesic and frigid.
b)
Soils are moderately deep to deep
ii)
Soil temperature regime is frigid.
a)
Site predominantly occurs on south exposures of canyon walls and the backslopes of tablelands and mountain plateaus
... R010XC051OR – SR High Mountain South 16-20 PZ
b)
Site occurs on tops and shoulders of ridges as well as north-facing mountain back slopes. Slopes may be up to 60 percent but more often range from 2 to 35 percent
... R010XC053OR – SR High Mountain Loam 18+ PZ
b.
Not as above
1
Soil temperature regime is mesic and soil moisture regime is aridic
... R010XC030OR – SR Cool 9-12 PZ
2
Soil moisture regime is xeric
i)
Soil temperature regime is transitional between mesic and frigid.
a)
Precipitation range is 12 to 16 inches
2)
Sites occur above 4000 feet
(i)
Surface texture is a silt or clay loam with very low, if any, surface fragment cover
... R010XC028OR – SR Shrubby Cool 12-16 PZ
(ii)
Surface texture is a very cobbly, very stony, or gravelly loam with approximately 10 to 20 percent surface gravel cover and 4 to 27 percent surface cobble cover
... R010XB028OR – JD Shrubby Mountain 12-16 PZ
ii)
Soil temperature regime is frigid
a)
Precipitation range is 12 to 16 inches
b)
Precipitation range is greater than 16 inches
1)
Site typically occurs between 4000 and 5700 feet on tablelands and mountain plateaus
... R010XC082OR – SR Dry Pine 14-16 PZ
2)
Site typically occurs between 6000 and 7500 feet on mountain ridges and plateaus
... R010XC070OR – SR Mountain 16-20 PZ
Snake River Warm Plains LRU
I.
Soils are very shallow over highly fractured bedrock. Ecosite identified but not developed
II.
Not as above
B.
Not as above
2
Not as above
i.
Sites occurring on north aspect slopes
a.
Soil temperature regime is mesic. Soil moisture regime is aridic
1)
Elevation typically between 3200 and 4500 feet with less than 100 frost free days. Soil temperature regime is mesic to near frigid
... R010XC065OR – SR Cool North 9-12 PZ
2)
Not as above
i)
Site predominately found on mid elevation terraces on droughty sites. Soil clay content between 18 and 35 percent
... R010XC063OR – SR Droughty North 9-12 PZ
b.
Soil temperature regime is transitional between cool mesic to frigid. Soil moisture regime is xeric
... R010XC068OR – SR Cool Mountain North 12-16 PZ
ii.
Not as above
a.
Sites occurring on south aspect slopes, soil temperature regime is mesic and soil moisture regime is aridic
1)
Soils range from shallow to deep, occur on unstable landscape positions and have little structural development
... R010XC056OR – SR Terrace Escarpment 9-12 PZ
2)
Soils are shallow
i)
Soils are a stony loam to gravelly clay loam about six inches thick
... BX010X00C050 – Shallow South 9-12 PZ Snake River Warm Plains
ii)
Soils are generally shallow with areas of rock outcrop. The surface layer is a channery loam about three inches thick with a very channery loam subsoil
... R010XC052OR – SR Shallow South Schist 9-12 PZ
b.
Not as above or sites that are not influenced by aspect
1)
Soil temperature regime is mesic. Soil moisture regime is aridic
i)
Soils are shallow
(a)
Sites occur on gentle slopes of 2 to 12 percent on terraces, tablelands, and rolling uplands
(2)
Typically occurs between 3500 to 4200 feet in elevation
... R010XC036OR – SR Shallow Cool 9-12 PZ
(b)
Sites occur on steep slopes of 2 to 40 percent on hillsides, escarpments, and eroded hills
... R010XC057OR – SR Shallow Escarpment 9-12 PZ
ii)
Soils are moderately deep to deep
(a)
Soils are clayey. Typically, both the surface and subsoil are clays with high shrink well potentials. Soil churning is prevalent.
... R010XC018OR – SR Adobeland 9-12 PZ
(b)
Soils are not as described above
(1)
Soil clay above 35 percent
(i)
Soil temperature regime is mesic to near frigid. Typical elevation between 2700 and 4400 feet. Site averages less than 100 frost free days. Plant communities are typically dominated by Wyoming big sagebrush and Idaho fescue.
... R010XC030OR – SR Cool 9-12 PZ
(ii)
Soil temperature regime is mesic. Elevations range from 2000 to 3500 feet. Site averages approximately 140 frost free days per year. Plant communities are typically dominated by Wyoming big sagebrush and bluebunch wheatgrass
... R010XC021OR – SR Clayey 9-12 PZ
(2)
Soil clay below 35 percent
(i)
Soil clay above 18 percent
(a)
Soils are made up of greater than 40 percent silt, often contain a cambic horizon, and coarse loamy particle size class. In the reference state, wild crab apple is present
... R010XC020OR – SR Loamy 9-12 PZ
(b)
Soils are made up of less than 40 percent silt, often contain an argillic horizon, and fine to fine loamy particle size class. In the reference state, wild crab apple is not present
... BX010X00C022 – Silty 9-12 PZ Snake River Warm Plains
2)
Soil temperature regime is transitional between mesic and frigid. Soil moisture regime is xeric
... R010XC033OR – SR Cool 12-16 PZ
Areas east of the Snake River, on the Footslopes and Plains of the Big and Little Wood River
I.
Site Occurs on Uplands
A.
Slopes greater than 30 percent on northerly aspects
1
Site occurs in greater than 20 inch precipitation zones, in areas of moisture accumulating topography
... R010XA016ID – Quaking Aspen 20+ PZ POTR5
2
Site is in 12 to 16 inch precipitation zones with elevation below 7000 feet
i.
Soils are volcanic cinders
a.
Coarse cinder soils, little soil development, cryic soil temperature regime
... R010XA043ID – Cinder North 12-16 PZ PIFL2/PUTR2
b.
Somewhat finer cinder soils, greater soil development, frigid soil temperature regime
... R010XA047ID – Cindery North 12-16 PZ ARTRV-PUTR2/FEID-PSSPS
ii.
Soils are not volcanic cinders
a.
Soils are extremely bouldery loams. Large boulders are common on the surface.
... R010XA037ID – Shrubby Stony North 12-16 PZ ARTRV/FEID
b.
Soils are moderately deep to deep stony loams.
... R010XA036ID – North Slope Stony 12-16 PZ ARTRX/PSSPS
3
Site occurs in 16 to 22 inch precipitation zones
i.
Soils are deep and loamy, site occurs at an elevation between 5000 to 8800 feet
... R010XA008ID – North Slope Loamy 16-22 PZ
ii.
Soils are generally shallow to fractured bedrock or clay. Roots penetrate below 20 inches.
... R010XA010ID – North Slope Fractured 16-22 PZ
B.
Slopes greater than 30 percent on southerly aspects
1
Occurs in 16 to 22 inch precipitation zone
2
Occurs in less than 16 inch precipitation zones
i.
Soils are volcanic cinders
a.
Coarse cinder soils, little soil development... R010XA045ID – Cinder South 12-16 PUTR2/HECO26 (Draft concept)
b.
Somewhat finer cinder soils, greater soil development... R010XA048ID – Cindery South 12-16 PUTR2-ARTRV/PSSPS (Draft concept)
ii.
Soils not volcanic cinders
a.
Site occurs in association with rock outcrops and talus slopes
... R010XA030ID – South Slope Channery 11-13 PZ ARTRX/PSSPS
b.
Not as above
1)
Soils greater than 20 inches to bedrock
a)
Coarse fragments greater than 35 percent throughout the soil profile
... R010XA009ID – South Slope Gravelly 12-16 PZ
2)
Soils less than 20 inches to fractured bedrock
a)
Site occurs on exposed ridgetops... R010XA024ID – STONY WINDSWEPT RIDGE 8-16 (Draft concept)
3
Site occurs in greater than 20 inch precipitation zones, in areas of moisture accumulating topography
... R010XA016ID – Quaking Aspen 20+ PZ POTR5
C.
Slopes generally less than 30 percent, occurring on all aspects
1
Site associated with recent lava flows
ii.
Soils less than 10 inches to basalt or lava bedrock
... R010XA050ID – Very Shallow Loam 12-16 PZ ARAR8/POSE
iii.
Soils greater than 20 inches deep
a.
Site nearly devoid of vegetation, coarse cinder soils, little soil development
... R010XA046ID – Cinder Garden 12-16 PZ EROVD-LERE7
b.
Somewhat finer cinder soils, greater soil development, cryic soil temperature regime
... R010XA044ID – Cinder 12-16 PZ PIFL2/ARTRV
c.
Soils with greater soil development than on Cinder 12 to 16. Increased fine soil particles within the profile... R010XA049ID – Gravelly Loam 12-16 ARTRV/PUTR2/PSSPS (Draft concept)
2
Not as above
i.
Soils are 20 inches or less
a.
Site occurs on exposed ridgetops... R010XA024ID – STONY WINDSWEPT RIDGE 8-16 (Draft concept)
b.
Not as above
1)
Surface texture is generally loam to silt loam but may be finer
... R010XA007ID – Shallow Stony Loam 8-16 PZ
2)
Surface texture is generally clay loam to silty clay but may be coarser
... R010XA038ID – Stony Clayey 8-16 PZ ARAR8/PSSPS
ii.
Soils are greater than 20 inches deep
b.
Soils are clayey to loamy
1)
Site has large boulders on or near surface
2)
Not as above
a)
Soils are 20 to 40 inches to a duripan
(1)
Sites occur in 12 to 16 inch precipitation zones, root restricting clayey subsurface at 14 to 18 inches
... R010XA001ID – Clayey 12-16 PZ ARARL/FEID
(2)
Sites occur in 10 to 12 inch precipitation zones
... R010XA034ID – Claypan 10-12 PZ ARTR4/PSSPS-ACTH7
b)
Not as above
(1)
Site occurs in 11 to 13 inch precipitation zones
(a)
Sites occur on slopes of 1 to 15 percent at elevations 4250 to 5000 feet. Soils are moderately deep. Textures are loams and silt loams.
... R010XA033ID – Loamy 11-13 PZ ARTRX/PSSPS
(b)
Sites occur on slopes of 5 to 25 percent and elevations from 4000 to 5500 feet. Soils are moderately deep. Textures are loams and silt loams.
... R010XA026ID – Loamy 11-13 PZ ARTRW8/PSSPS
(2)
Site occurs in 12 to 16 inch precipitation zones
(a)
Sites occur on slopes from 1 to 30 percent and elevations from 4500 to 6500 feet. Soils are moderately deep to deep. Textures are loams, silt loams and gravelly silt loams
... R010XA004ID – Loamy 12-16 PZ ARTRV/FEID-PSSPS
(b)
Sites occur on slopes from 1 to 20 percent and elevations from 4000 to 5500 feet. Soils are moderately deep to deep. Surface soils are silt loams. Subsoils are silty clay loam to clay loam.
... R010XA023ID – Loamy 12-16 PZ ARTR4/FEID
(3)
Site occurs in greater than 20 inch precipitation zone, in areas of moisture accumulating topography
... R010XA016ID – Quaking Aspen 20+ PZ POTR5
II.
Site occurs on bottomlands with slopes less than 8 percent
B.
Water table present for most of the growing season.
1
Water standing at or above the surface into late summer... R010XA040ID MARSH TYLA-SCAC3 (Draft concept)
2
Water at or near the surface at beginning of growing season and down to 10 to 20 inches at the end of the growing season.
... R010XA039ID – Wet Meadow Carex/Juncus
3
Water at or near the surface at beginning of growing season and down to 20 to 40 inches at the end of the growing season
... R010XA027ID – Meadow DECA18-CANE2
4
Water at or near the surface at beginning of the growing season and greater than 40 inches at the end of the growing season.
... R010XA028ID – Dry Meadow 8-15 PZ PONE3-PHAL2
Areas east of the Snake River, on the Upper Snake River Lava Plains and Hills
I.
Site occurs on uplands.
A.
Slopes greater than 30 percent on northerly aspects
1
Soils derived from granite
i.
Site occurs in 12 to 16 inch precipitation zones at 3000 to 4500 feet elevation
... R010XY014ID – North Slope Granitic 12-16 PZ ARTRX/FEID
ii.
Site occurs in 16 to 22 inch precipitation zones at 4000 to 5500 feet elevation
... R010XY013ID – North Slope Granitic 16-22 PZ ARTRV/FEID
2
Soils not derived from granite
i.
Site occurs in 12 to 16 inch precipitation zones at 2100 to 4000 feet elevation. Soils are moderately deep to deep loams and silt loams
... R010XY001ID – North Slope Loamy 12-16 PZ FEID-PSSPS
ii.
Site occurs in 16 to 22 inch precipitation zones at 3000 to 5500 feet elevation. Soils are deep silt loams
... R010XY005ID – North Slope Loamy 16-22 PZ ARTRV/FEID
iii.
Site occurs in 16 to 20 inch precipitation zones at 2700 to 5800 feet elevation. Soils are excessively drained coarse sandy loams to fine gravelly sandy loams over 20 inches deep
... R010XY027ID – North Slope Brush 16-20 PZ PREM/ELGLG
B.
Slopes greater than 30 percent on southerly aspects
1
Soils are not stony
i.
Soils derived from granite
a.
Site occurs in 12 to 16 inch precipitation zones at 3000 to 5000 feet elevation. Soils are moderately deep and coarse textured
... R010XY008ID – South Slope Granitic 12-16 PZ PUTR2/PSSPS
b.
Site occurs in 16 to 20 inch precipitation zones at 3000 to 6000 feet elevation. Soils are moderately deep to deep coarse sandy loams
... R010XY028ID – South Slope Granitic 16-20 PZ ARTRX/PSSPS
ii.
Soils not derived from granite
a.
Site occurs in 12 to 16 inch precipitation zones at 3000 to 4800 feet elevation. Soils are loamy derived from acid igneous alluvial or lacustrine deposits and are moderately deep to deep
... R010XY019ID – South Slope Loamy 12-16 PZ ARTRX/PSSPS
b.
Site occurs in 16 to 22 inch precipitation zones at 3000 to 5000 feet elevation. Soils are deep silt loams to silty clay loams derived from colluvium, tuff, rhyolite, basalt, and siltstone
... R010XY004ID – South Slope Loamy 16-22 PZ ARTRX/PSSPS
c.
Site occurs in 12 to 16 inch precipitation zone at 2600 to 3900 feet elevation. Soils are deep, sand to sandy loams formed from lacustrine deposits
... R010XY031ID – South Slope Sandy 12-16 PZ
2
Soils are stony
i.
Soil depth is moderately deep to deep
a.
Site occurs in 12 to 16 inch precipitation zones at 2000 to 3500 feet. Textures are stony loams
... R010XY011ID – South Slope Stony 12-16 PZ ARTRT/PSSPS
b.
Site occurs in 16 - 22 inch precipitation zones at 3500 to 4500 feet. Textures are stony to extremely stony loams
... R010XY021ID – Stony Loam 16-22 PZ ARTRT/PSSPS
ii.
Soil depth is shallow
a.
Site occurs in 12 to 16 inch precipitation zones at 3000 to 4500 feet. Textures are stony loams to clay loams
... R010XY016ID – Shallow South Stony 12-16 PZ ARTRX/PSSPS
b.
Site occurs in 14 to 18 inch precipitation zones at 2400 to 5000 feet. Textures are very stony loams to very gravelly clay loams
... R010XY018ID – Shallow South Stony 14-18 PZ PSSPS-POSE
c.
Site occurs in 12 to 20 inch precipitation zones at 4000 to 7500 feet. Textures are cobbly and stony clay loams. Soil depths range from 10 to 40 inches
... R010XY017ID – South Slope Clayey 12-20 PZ ARAR8/PSSPS
C.
Slopes less than 30 percent on all aspects (non-aspect)
1
Soils are not stony
i.
Site occurs in 12 to 16 inch precipitation zones at 2500 to 4500 feet. Textures are loamy
... R010XY007ID – Loamy 12-16 PZ
ii.
Site occurs in 12 to 16 inch precipitation zones at 2500 to 3200 feet. Textures are loamy fine sand to very fine sandy loam
... R010XY032ID – Loamy 12-16 PZ
iii.
Site occurs in 16 to 20 inch precipitation zones at 3000 to 4000 feet elevation. Textures are sandy loams to clay loams
... R010XY003ID – Loamy 16-22 PZ PUTR2/FEID
iv.
Site occurs in 16 to 22 inch precipitation zones at 3000 to 5000 feet. Textures are coarse sandy loams derived from granite
... R010XY022ID – Granitic 16-22 PZ PSSPS-FEID
v.
Site occurs in 8 to 16 inch precipitation zones at 2000 to 3000 feet. Textures are clay and deep vertisols
... R010XY006ID – Churning Clay 8-16 PZ ARTRX/PSSPS
2
Soils are stony
i.
Soil depth is moderately deep to deep
a.
Site occurs in 12 to 16 inch precipitation zones at 2500 to 4500 feet. Textures are stony loams
... R010XY009ID – Stony Loam 12-16 PZ ARTRT/PSSPS
b.
Site occurs in 16 to 22 inch precipitation zones at 3500 to 4500 feet. Textures are deep, stony to extremely stony, loams
... R010XY021ID – Stony Loam 16-22 PZ ARTRT/PSSPS
ii.
Soil depth is very shallow to shallow
a.
Site occurs in 12 to 20 inch precipitation zones at 2500 to 4000 feet. Soils are very shallow, stony to extremely stony loams to clay loams
... R010XY002ID – Very Shallow 12-20 PZ ARRI2/POSE
b.
Site occurs in 12 to 20 inch precipitation zones at 2500 to 4500 feet. Soils are shallow, very stony loams to very gravelly clay loams
... R010XY025ID – Shallow Stony Loam 12-20 PZ ARTRX/PSSPS
II.
Site occurs on bottomlands with slopes less than five percent.
B.
Water at or near the surface at beginning of growing season and down to 10 to 20 inches at the end of the growing season
... R010XY029ID – Wet Meadow Carex-Juncus
C.
Water at or near the surface at beginning of growing season and down to 20 to 40 inches at the end of the growing season
... R010XY023ID – Meadow DECA18-CANE2
D.
Water at or near the surface at beginning of the growing season and greater than forty inches at the end of the growing season
... R010XY024ID – Dry Meadow PONE3-PHAL2
The Ecosystem Dynamics Interpretive Tool is an information system framework developed by the USDA-ARS Jornada Experimental Range, USDA Natural Resources Conservation Service, and New Mexico State University.
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