Natural Resources
Conservation Service
Major Land Resource Area 001X
Major Land Resource Area
Accessed: 05/03/2026
Description
This long and narrow resource area stretches along the Pacific Border Province of the Pacific Mountain System in Oregon and Washington. The area is bounded by the Olympic Mountains on the north and the Klamath Mountains on the south. Most of the area consists of hills and low mountains with gentle to steep slopes. The parent materials are composed primarily of young Tertiary sedimentary rocks with some minor volcanic rocks. Glacial till and outwash deposits are found in the northern half of the area within Washington. In the far southern portion of the area, near the Klamath Mountains, the sedimentary rocks are older and some have been metamorphosed. The average annual precipitation ranges from 60 to 200 inches, increasing with elevation. The dominant soil orders in this MLRA are Andisols, Inceptisols, and Ultisols. Soil depth ranges from shallow to very deep. While most soils in the area are well drained and occur on foothills, mountain slopes and ridges, floodplain and depressional soils can range from well drained to very poorly drained. Soil textures are typically medial, loamy, or clayey. The dominant soils in the area have a mesic or frigid soil temperature regime and a udic soil moisture regime; however, soils with an aquic soil moisture regime or cryic soil temperature regime do occur.
Key publications
Geographic subunits
Land Resource Unit 1 Olympic National Park Land Resource Unit. This LRU occurs on the Olympic Peninsula in and around Olympic National Park in Washington.
Land Resource Unit 2 The North Pacific Coast Range land resource unit of MLRA 1 is located in the northwestern corner on the Olympic Peninsula and within the Olympic National Forest in Washington State. LRU 2 is bounded on the west by MLRA 4a Sitka Spruce Belt and MLRA 2 Willamette and Puget Sound Valleys to the east. LRU 2 encircles the Olympic National Park (LRU 1). Several major rivers have headwaters in this LRU or carved valleys through the landscape depositing more recent alluvium. These include the Duckabush, Elwha, Queets, Quinault, Skokomish, Sol Duc, and Wynoochee Rivers.
Land Resource Unit 3 The Central Pacific Coast Range land resource unit of MLRA 1 ranges from the Olympic Peninsula south into northern Oregon. LRU 3 is located south of the Olympic National Forest and extends to the Siletz River in Oregon. LRU 3 is bounded on the west by MLRA 4a Sitka Spruce Belt and MLRA 2 Willamette and Puget Sound Valleys to the east. Several major rivers have headwaters in this LRU or carved valleys through the landscape depositing more recent alluvium. These include the Chehalis, Columbia, Grays, Humptulips, Klaskanine, Nehalem, Satsop, Siletz, Willapa, Wilson, Wynoochee, and Yamhill Rivers.
Land Resource Unit 4 The Southern Pacific Coast Range land resource unit of MLRA 1 is located in central to southern Oregon State. The LRU extends from the Siletz River to the Rogue River and is bounded on the west by MLRA 4a Sitka Spruce Belt and MLRA 2 Willamette and Puget Sound Valleys to the east. Several major rivers carved valleys through the landscape depositing more recent alluvium. These include the Alsea, Coos, Coquille, Green, Yachats, Siletz, Siuslaw, Umpqua, and Rogue Rivers.
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Ecological site list
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i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
-
i
Key Characteristics
- Site resides in north of the Columbia River
- Mesic areas in or near the Puget Sound that were modified by Pleistocene continental or alpine glaciation - LRU A Puget Lowlands
- Area is located in San Juan or Island Counties
- Area with soils that do not meet hydric criteria
- Forested areas
- Soils that are dry between 60 and 90 consecutive days in the soil moisture control section
- Between 75 and 90 days dry in the soil moisture control section
Ecological site map
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Ecological sites
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AX001X02X001 – Mesic Udic Riparian Forest
AX001X02X003 – Mesic Aquic Forest
AX001X02X402 – Frigid Udic Forest
AX001X02X403 – Frigid Udic Moist Forest
AX001X02X410 – Mesic Udic Forest
AX001X02X411 – Mesic Udic Moist Forest
AX001X02X420 – Isofrigid Udic Forest
AX001X03X001 – Mesic Udic Riparian Forest
AX001X03X003 – Mesic Aquic Forest
AX001X03X205 – Bog or Fen
AX001X03X401 – Cryic Udic Forest
AX001X03X201 – Cryic Udic Meadow
AX001X03X402 – Frigid Udic Forest
AX001X03X410 – Mesic Udic Forest
AX001X03X411 – Mesic Udic Moist Forest
AX001X03X413 – Mesic Udic Warm Forest
AX001X04X001 – Mesic Udic Riparian Forest
AX001X04X002 – Mesic Udic Flood Plain Forest
AX001X04X003 – Mesic Aquic Forest
AX001X04X401 – Cryic Udic Forest
AX001X04X402 – Frigid Udic Forest
AX001X04X410 – Mesic Udic Forest
AX001X04X411 – Mesic Udic Moist Forest
AX001X04X412 – Mesic Udic Wet Forest
AX001X04X413 – Mesic Udic Warm Forest
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- 1200 – 1400m (3900 – 4600ft)
- 1400 – 1600m (4600 – 5200ft)
- 1600 – 1800m (5200 – 5900ft)
- 1800 – 2000m (5900 – 6600ft)
- 2000 – 2200m
- 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%
- 90 – 100%
- No filter
- Bench
- Cirque
- Colluvial apron
- Depression
- Drainageway
- Flood plain
- Fluvial terrace
- Glacial-valley wall
- Hillside or mountainside
- Knob
- Moraine
- Mountain slope
- Proglacial lake
- Proglacial lake (relict)
- Ridge
- Slide
- Stream terrace
- Structural bench
- Terrace
- Terrace--stream or lake
- Valley
- Valley train
- No filter
- Basalt
- Igneous and sedimentary
- Igneous, unspecified
- Metasedimentary, unspecified
- Sandstone and siltstone
- Sandstone, unspecified
- Sedimentary, unspecified
- Shale and siltstone
- Siltstone, unspecified
- No filter
- Alluvium
- Colluvium
- Glaciofluvial deposits
- Glaciolacustrine deposits
- Glaciomarine deposits
- Loess
- Marine deposits
- Organic, herbaceous material
- Organic, mossy material
- Outwash
- Residuum
- Till, unspecified
Soil surface texture
- No filter
- Clay loam
- Fine sandy loam
- Loam
- Loamy sand
- Sand
- Silty clay
- Silty clay loam
- Silt loam
- Sandy loam
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Ecological site keys
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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