Major Land Resource Area 236X
Bristol Bay-Northern Alaska Peninsula Lowlands
Accessed: 12/21/2024
Description
The Bristol Bay-Northern Alaska Peninsula Lowland Major Land Resource Area (MLRA 236) is located in Western Alaska. This MLRA covers approximately 19,500 square miles and is defined by an expanse of nearly level to rolling lowlands, uplands and low to moderate hills bordered by long, mountain footslopes. Major rivers include the Egegik, Mulchatna, Naknek, Nushagak, and Wood River. MLRA 236 is in the zone of discontinuous permafrost. It is primarily in areas with finer textured soils on terraces, rolling uplands and footslopes. This MLRA was glaciated during the early to middle Pleistocene. Moraine and glaciofluvial deposits cover around sixty percent of the MLRA. Alluvium and coastal deposits make up a large portion of the remaining area (Kautz et al., 2012; USDA, 2006). Climate patterns across this MLRA shift as one moves away from the coast. A maritime climate is prominent along the coast, while continental weather, commonly associated with Interior Alaska, is more influential inland. Across the MLRA, summers are general short and warm while winters are long and cold. Mean annual precipitation is 13 to 50 inches, with increased precipitation at higher elevations and areas away from the coast. Mean annual temperatures is between 30 and 36 degrees F (USDA, 2006). The Bristol Bay-Northern Alaska Peninsula MLRA is principally undeveloped wilderness. Federally managed land includes parts of the Katmai and Aniakchak National Parks, and the Alaska Peninsula, Becharof, Togiak and Alaska Maritime National Wildlife Refuges. The MLRA is sparsely populated. Principal communities include Dillingham, Naknek, and King Salmon. Commercial fishing in Bristol Bay and the Bering Sea comprises a major part of economic activity in the MLRA. Other land uses include subsistence activities (fishing, hunting, and gathering) and sport hunting and fishing (USDA, 2006).
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Ecological site list
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplains
- Mid and High Floodplains
- High Floodplains
- Ponding absent
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Key Characteristics
- Boreal Climatic Zone
- Upland
- Escarpments on Mountains and Hills
- Planar to convex slope shape
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Key Characteristics
- Boreal Climatic Zone
- Upland
- Escarpments on Mountains and Hills
- Planar to concave slope shape
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Key Characteristics
- Boreal Climatic Zone
- Upland
- All Other Mountain, Hill & Plains Landforms
- Mountains
- Rounded, non-glaciated mountains; colluvial backslopes
- Boreal Climatic Zone
- Upland
- All Other Mountain, Hill & Plains Landforms
- Hills and Plains
- All Other Landforms
- Not As Above
- Planar to Convex Slopes
- Silty, moist soils
- Undulating or rolling terrain
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Key Characteristics
- Boreal Climatic Zone
- Upland
- All Other Mountain, Hill & Plains Landforms
- Hills and Plains
- All Other Landforms
- Not As Above
- Planar to Convex Slopes
- Loess, wet soils
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Key Characteristics
- Boreal Climatic Zone
- Upland
- All Other Mountain, Hill & Plains Landforms
- Hills and Plains
- Swale and Depression Features
- Depression Features
- Boreal Climatic Zone
- Upland
- All Other Mountain, Hill & Plains Landforms
- Hills and Plains
- All Other Landforms
- Not As Above
- Planar to Concave Slopes (common near Aleknagik, often surrounded by wetlands)
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Key Characteristics
- Boreal Climatic Zone
- Upland
- All Other Mountain, Hill & Plains Landforms
- Hills and Plains
- All Other Landforms
- Adjacent to gallery forest or within a few miles of Nushagak River
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplains
- Mid and High Floodplains
- High Floodplains
- Ponding present
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Key Characteristics
- Boreal Climatic Zone
- Upland
- All Other Mountain, Hill & Plains Landforms
- Hills and Plains
- Swale and Depression Features
- Swales
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Key Characteristics
- Boreal Climatic Zone
- Upland
- All Other Mountain, Hill & Plains Landforms
- Hills and Plains
- All Other Landforms
- Not As Above
- Planar to Convex Slopes
- Silty, moist soils
- Nearly level terrain; low slope gradient, high slope length
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Terraces
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Rolling and undulating hills and plains
- Not as above
- Not as above
- Linear/Linear and Linear/Convex slopes
- Proximal to organic drainageway or depression
- Warmer climate, forested (coastal)
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Unbraided river channels at higher elevations: tributaries to Nushagak and Mulchatna Rivers, generally over 60m elevation
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Key Characteristics
- Boreal Climatic Zone
- Upland
- All Other Mountain, Hill & Plains Landforms
- Mountains
- Glaciated & Rugged Mountains
- Silty, wet soil; warm slopes
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Key Characteristics
- Boreal Climatic Zone
- Upland
- All Other Mountain, Hill & Plains Landforms
- Mountains
- Glaciated & Rugged Mountains
- Loamy, frozen soil; all aspects
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks present
-
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Mountains
- Not as above
- Depressions
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Mountains
- Rounded Mountains
- Summits, Shoulders, Upper Backslopes
- Alpine
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Mountains
- Not as above
- Slopes (Summits, Shoulders, Backslopes, Footslopes)
- Summits and Shoulders
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Mountains
- Not as above
- Slopes (Summits, Shoulders, Backslopes, Footslopes)
- Backslopes and Footslopes
- Well drained soil
- Concave to Linear slope shape
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Mountains
- Rounded Mountains
- Summits, Shoulders, Upper Backslopes
- Subalpine
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Mountains
- Not as above
- Slopes (Summits, Shoulders, Backslopes, Footslopes)
- Backslopes and Footslopes
- Well drained soil
- Convex to Linear slope shape
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Plains (non-coastal) Concave Microfeatures
- Drainageways
- Narrower than 10 meter across
- Surrounding slopes <10%
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Floodplains & Terraces
- Floodplains
- Floodplain
- Linear slope, surface water may be present
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Concave microfeatures
- Depressions
- Not adjacent to a large glacial lake
- Western Maritime Climatic Zone
- Lowlands
- Plains (non-coastal) Concave Microfeatures
- Drainageways
- Wider than 10m across
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Plains (non-coastal) Concave Microfeatures
- Depressions
-
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplain microfeature
- Levee
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplains
- Mid and High Floodplains
- Mid Floodplains
- Not in a channel
- Short or absent ponding period
- Landscape cut by deep river channel
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplains
- Mid and High Floodplains
- Mid Floodplains
- Not in a channel
- Long ponding period
-
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplains
- Mid and High Floodplains
- Mid Floodplains
- Not in a channel
- Short or absent ponding period
- Deep river channel absent
- Well drained to somewhat poorly drained, distal from flood source
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Rolling and undulating hills and plains
- Exposed convex slopes of tall, rolling landscape; lake margins
-
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Concave microfeatures
- Depressions
- Adjacent to large glacial lake
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Steep slopes less than three (3) meters in length
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Coastal Plains
- Depression on coastal plain (surface water present)
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Rolling and undulating hills and plains
- Not as above
- Not as above
- Linear/Linear and Linear/Convex slopes
- Not proximal to organic drainageway or depression
- Areas of increased out-flow
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Rolling and undulating hills and plains
- Not as above
- Not as above
- Linear/Linear and Linear/Convex slopes
- Not proximal to organic drainageway or depression
- Areas of increased in-flow
- Well drained soil
-
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Rolling and undulating hills and plains
- Not as above
- On or surrounded by peat mounds
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Mountains
- Rounded Mountains
- Lower Backslopes and Footslopes
-
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels present
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Rolling and undulating hills and plains
- Not as above
- Not as above
- Exposed slopes (convex/convex), and long (400+ meters) slopes with <1% slope gradient
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Coastal Plains
- Plains
- Presence of surface soil or rock fragments
- Surface gravel present
-
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Coastal Plains
- Plains
- Absence of surface soil or fragments
- Adjacent to tidal gut
-
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Plains (non-coastal) Concave Microfeatures
- Drainageways
- Narrower than 10 meter across
- Surrounding slopes >10%
-
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Rolling and undulating hills and plains
- Not as above
- Not as above
- Linear/Linear and Linear/Convex slopes
- Proximal to organic drainageway or depression
- Cooler climate, non-forested (Inland positions)
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Floodplains & Terraces
- Terraces
- On Nushagak River corridor (or similarly braided glacial river system)
- Linear depression on terrace
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Floodplains & Terraces
- Terraces
- Not as above
-
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Concave microfeatures
- Swales
- Circular swale
-
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplains
- Low Floodplain
- Not in a channel/depression
-
i
Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Concave microfeatures
- Swales
- Linear swale
-
i
Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplains
- Mid and High Floodplains
- Mid Floodplains
- In a channel
-
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Floodplains & Terraces
- Terraces
- On Nushagak River corridor (or similarly braided glacial river system)
- Terrace talf
-
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplains
- Mid and High Floodplains
- Mid Floodplains
- Not in a channel
- Short or absent ponding period
- Deep river channel absent
- Somewhat poorly drained, proximal to flood source
-
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplains
- Low Floodplain
- In a channel/depression
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Floodplains & Terraces
- Floodplains
- Floodplain depression
-
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Coastal Plains
- Plains
- Presence of surface soil or rock fragments
- Surface gravel absent
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Coastal Plains
- Plains
- Absence of surface soil or fragments
- Not adjacent to tidal gut
-
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Key Characteristics
- Boreal Climatic Zone
- Lowland
- Floodplain
- Braided river systems at lower elevations: along Nushagak River or other braided glacial river systems, generally below 60m elevation
- Floodplain microfeature
- Linear depression
-
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Key Characteristics
- Western Maritime Climatic Zone
- Lowlands
- Coastal Plains and Floodplains
- Floodplains & Terraces
- Floodplains
- Floodplain
- Convex slope, run off medium to high
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Escarpments
- Along drainageway or river
-
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Escarpments
- Along coastline
-
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Mountains
- Not as above
- Slopes (Summits, Shoulders, Backslopes, Footslopes)
- Backslopes and Footslopes
- Poorly drained soil
-
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Key Characteristics
- Western Maritime Climatic Zone
- Upland
- Not an escarpment
- Plains and Hills
- Surface gravels absent
- Earth hummocks absent
- Slopes otherwise
- Rolling and undulating hills and plains
- Not as above
- Not as above
- Linear/Linear and Linear/Convex slopes
- Not proximal to organic drainageway or depression
- Areas of increased in-flow
- Very poorly drained soil
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