Kantishna Area, Alaska

Survey Area AK643 Alaska

The dominant drainage class is Somewhat excessively drained and the dominant hydrologic group is D (very slow infiltration, high runoff). The most common soil order is Inceptisols — young soils with minimal horizon development but more than Entisols. This report summarizes the major soil map units across the survey area to help you understand what to expect when buying, building, or gardening in Kantishna Area, Alaska. Search your address to find the exact soil composition, drainage, and series details at your specific location.

Soil Map UnitAcresDrainageHydro GroupDwellingsSeptic
Kindanina-Beales-Zitziana complex, dunes, 1 to 50 percent slopes 63K Very poorly drainedDVery limitedVery limited
Iksgiza-Nenana complex, 1 to 35 percent slopes 50K Poorly drainedDVery limitedVery limited
Zitziana-Kindanina complex, 1 to 35 percent slopes 32K Somewhat excessively drainedBVery limitedVery limited
Beales-Zitziana complex, 1 to 35 percent slopes 27K Somewhat excessively drainedBVery limitedVery limited
Zitziana silt loam, 1 to 35 percent slopes 23K Somewhat excessively drainedBVery limitedVery limited
Typic Histoturbels, Terric Hemistels, and Bradway soils, 0 to 2 percent slopes 23K Very poorly drainedDVery limitedVery limited
Beales very fine sandy loam, 1 to 35 percent slopes 22K Somewhat excessively drainedBVery limitedVery limited
Koyukuk silt loam, 1 to 35 percent slopes 22K Well drainedBVery limitedVery limited
Typic Dystrocryepts-Tetlin-Saulich association, 15 to 70 percent slopes 22K Well drainedDVery limitedVery limited
Iksgiza-Terric Hemistels complex, 0 to 3 percent slopes 21K Poorly drainedDVery limitedVery limited
Saulich peat, 0 to 6 percent slopes 19K Very poorly drainedDVery limitedVery limited
Iksgiza-Beales-Zitziana complex, pitted, 1 to 50 percent slopes 19K Somewhat excessively drainedBVery limitedVery limited
Nenana-Zitziana complex, 1 to 35 percent slopes 17K Well drainedBVery limitedVery limited
Beales very fine sandy loam, 35 to 70 percent slopes 12K Somewhat excessively drainedBVery limitedVery limited
Iksgiza peat, 0 to 3 percent slopes 12K Poorly drainedDVery limitedVery limited
Typic Cryopsamments, Typic Cryaquepts, flooded, and Bradway soils, 0 to 5 percent slopes 11K Excessively drainedDVery limitedVery limited
Saulich peat, 6 to 30 percent slopes 11K Very poorly drainedDVery limitedVery limited
Iksgiza-Zitziana-Nenana complex, 1 to 35 percent slopes 10K Poorly drainedDVery limitedVery limited
Kindanina mucky silt loam, 0 to 6 percent slopes 10K Very poorly drainedDVery limitedVery limited
Water 10K Not ratedNot rated

Soil Orders in This Area

The USDA classifies every soil into one of 12 soil orders. Here are the dominant orders found in this survey area.

Inceptisols
Young but developing soils found in mountains and river terraces. Variable properties — check drainage and bedrock depth.
Gelisols
Permafrost soils. Extremely challenging for construction and septic. Found almost exclusively in Alaska.
Entisols
Young soils with little development — found on floodplains, dunes, and steep slopes. Properties vary widely by setting.

What This Means

Building & Foundations

About 97% of soils are rated "very limited" for dwellings with basements. Specific challenges include steep slopes, poor drainage in some areas, flood-prone areas, sandy or gravelly soils with low bearing capacity. A geotechnical assessment is recommended before building.

Septic Systems

About 97% of soils are rated "very limited" for septic absorption fields. The well-drained soils may actually drain too fast for standard leach fields, allowing effluent to reach groundwater. Engineered or alternative systems are frequently required. Always get a professional perc test before purchasing land that needs septic.

Gardening & Agriculture

Soils tend to drain very quickly, meaning nutrients and water don't stick around long. Raised beds with amended soil, drip irrigation, and heavy mulching will give the best results. Compost is your best friend here — it improves water retention dramatically.

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