Natural Resources
Conservation Service
Major Land Resource Area 142X
Major Land Resource Area
Accessed: 04/16/2026
Description
MLRA 142 is in New York (75 percent) and Vermont (25 percent). It makes up about 7,067 square miles (18,305 square kilometers). The MLRA is made up of two broad valleys, the St. Lawrence and Champlain, that coalesce to form a broad contiguous lowland underlain by relatively thick Wisconsin till, outwash, lacustrine, and marine deposits. It adjoins Lake Champlain at the New York-Vermont border. MLRA 142 is roughly U-shaped, with the open end to the south. A distinct southern boundary occurs in New York with the physiographically dissimilar Adirondack Mountains part of MLRA 143. The eastern boundary is distinct where it contacts the physiographically dissimilar Green Mountains part of MLRA 143 in Vermont. The southwestern boundary, in New York, is distinct with the physiographically dissimilar Tug Hill Plateau (MLRA 141) but is more diffuse with small parts of MLRA 101. The southeastern part of MLRA 142 forms a relatively diffuse boundary with MLRAs 144A and 144B in New York and Vermont. The northern boundary of the MLRA is he Canadian border and the St. Lawrence River. Lake Ontario is along the western boundary. The dominant soil orders are Alfisols, Inceptisols, Spodosols, and Entisols. The soils in the area have a frigid or mesic temperature regime, an aquic or udic moisture regime, and mixed or isotic mineralogy. They are shallow to very deep, excessively drained to very poorly drained, and sandy to clayey. Most of this area is in forests or farms. The forests consist of northern hardwoods and conifers. Sawlogs and pulpwood are the main forest products. Christmas trees and maple syrup also are produced throughout the area. Dairy operations and some beef operations are common. Hay for dairy cattle is the principal crop, but small grain and corn are grown for silage in some areas. Corn for grain, soybeans, and small grains also make up a significant acreage. Potatoes are an important cash crop in some areas, and a few apple orchards are on the slopes along Lake Champlain, but the total acreage of these crops is small. Some areas are used for urban development. The major soil resource concerns on cropland are sheet, rill, and gully erosion; the content of organic matter and productivity of the soils; and surface compaction (resulting primarily from the harvest of crops under wet conditions). Some erosion results from logging practices. Conservation practices on cropland generally include conservation tillage, contour stripcropping, crop rotations, crop residue management (primarily mulch-till), cover crops, diversions, and grassed waterways. Conservation practices on forestland generally include forest stand improvement and proper construction, use, and maintenance of skid trails, water bars, access roads, and log landings.
Key publications
Geographic subunits
Land Resource Unit 1 The Frigid Soil Temperature Regime LRU is located primarily in the St. Lawrence Valley and Upper Champlain Valley portions of New York and Vermont. These soils will have a mean annual temperature is between 0 and 8°C and the difference between mean summer (June, July, August) and mean winter (December, January, February) soil temperatures is 6°C or more either at a depth of 50cm below the soil surface or at root restriction, whichever is shallower (USDA Keys to Soil Taxonomy, 13th Edition). The total area of this LRU is approximately 2,300,000 acres. This LRU will have a shorter growing season than the Mesic LRU. Species more tolerant of harsher year round temperatures will be more evident in this LRU, portraying lower species diversity.
Land Resource Unit 2 The Mesic Soil Temperature Regime LRU is located primarily in the Eastern Ontario Plain and Lower Champlain Valley portions of New York and Vermont. These soils will have a mean annual soil temperature 8°C or higher but lower than 15°C and the difference between mean summer (June, July, August) and mean winter (December, January, February) soil temperatures is 6°C or more either at a depth of 50cm below the soil surface or at root restriction, whichever is shallower (USDA Keys to Soil Taxonomy, 13th Edition). The total area of this LRU is approximately 1,900,000 acres. This LRU will have a longer growing season than the Frigid LRU. Species more tolerant of milder year round temperatures will be more evident in this LRU, portraying higher species diversity.
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F142XA001NY – Low Floodplain Frigid
F142XB001NY – Mucky Depression
F142XA002NY – Mucky Depression Frigid LRU
F142XA003NY – Acidic Peaty Depression
F142XA022NY – Rich Dry Outwash Frigid
F142XA004NY – Acidic Shallow Sandy Outwash
F142XA005NY – Acidic Sandy Outwash
F142XA006NY – Acidic Moist Outwash Frigid
F142XA007NY – Rich Moist Outwash Frigid
F142XA008NY – Wet Outwash Depression
F142XA014NY – Wet Lacustrine Depression
F142XA010NY – Acidic Lacustrine Terraces Frigid
F142XA012NY – Rich Lacustrine Terraces Frigid
F142XA021NY – Wet Till Depression
F142XA015NY – Shallow Acidic Till Upland Frigid
F142XA019NY – Acidic Moist Till Frigid
F142XA016NY – Shallow Rich Till Upland
F142XA018NY – Rich Till Upland Frigid
F142XA020NY – Rich Moist Till Frigid
F142XB004VT – Wet Outwash Depression
F142XB002VT – Dry Outwash
F142XB003VT – Moist Outwash
F142XB007VT – Wet Clayplain Depression
RX142X00B005 – Clayplain
F142XB018VT – Moist Lake Plain
F142XB019NY – Shallow Acidic Till Upland
F142XA009NY – Steep Acidic Lacustrine Slope Frigid
F142XB010NY – Shallow Rich Till Upland
F142XB012VT – Rich Till Upland
F142XB013NY – Moist Till Upland
F142XB021NY – Acidic Wet Till Depression
F142XB014NY – Rich Wet Till Depression
Long term average mean annual precipitation
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- 80 – 100cm (31 – 39in)
Long term average frost free days
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- Alluvium
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- Outwash
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Soil surface texture
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