Siskiyou County, California, Central Part

Survey Area CA602 California

The dominant drainage class is Well drained and the dominant hydrologic group is C (slow infiltration, moderate runoff). The most common soil order is Mollisols — grassland soils with a thick, dark, fertile topsoil rich in organic matter. 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 Siskiyou County, California, Central Part. Search your address to find the exact soil composition, drainage, and series details at your specific location.

Soil Map UnitAcresDrainageHydro GroupDwellingsSeptic
Duzel-Jilson-Facey complex, 15 to 50 percent slopes 103K Well drainedCVery limitedVery limited
Marpa-Kinkel-Boomer, cool complex, 15 to 50 percent slopes 80K Well drainedCVery limitedVery limited
Kindig-Neuns gravelly loams, 50 to 80 percent slopes complex 47K Well drainedBVery limitedVery limited
Lassen-Kuck complex, stony, 2 to 50 percent slopes 46K Well drainedDVery limitedVery limited
Lassen-Rock outcrop-Kuck complex, 2 to 50 percent slopes 36K Well drainedDVery limitedVery limited
Jilson-Duzel gravelly loams, 5 to 50 percent slopes complex 28K Well drainedDVery limitedVery limited
Lithic Haploxerolls-Rock outcrop complex, 0 to 65 percent slopes* 24K Excessively drainedDVery limitedVery limited
Mary-Rock outcrop complex, 2 to 50 percent slopes 22K Well drainedCVery limitedVery limited
Lithic Xerorthents-Rock outcrop complex, 0 to 65 percent slopes* 21K Excessively drainedDVery limitedVery limited
Rock outcrop 17K Excessively drainedDVery limitedVery limited
Gazelle silt loam 16K Very poorly drainedB/DVery limitedVery limited
Mary stony loam, 2 to 50 percent slopes 16K Well drainedCVery limitedVery limited
Salisbury cobbly loam, 0 to 9 percent slopes 14K Well drainedDVery limitedVery limited
Settlemeyer loam, 0 to 2 percent slopes 13K Poorly drainedC/DVery limitedVery limited
Chaix-Chawanakee gravelly coarse sandy loams, 50 to 70 percent slopes complex 12K Well drainedBVery limitedVery limited
Pinehurst stony loam, 2 to 15 percent slopes 10K Well drainedCSomewhat limitedVery limited
Sheld-Iller stony sandy loams, 9 to 30 percent slopes complex 10K Well drainedBVery limitedVery limited
Plutos-Rock outcrop complex, 0 to 30 percent slopes 9K Somewhat excessively drainedAVery limitedVery limited
Pinehurst stony loam, 15 to 30 percent slopes 9K Well drainedCVery limitedVery limited
Avis-Oosen complex, 5 to 30 percent slopes 9K Somewhat excessively drainedAVery limitedVery limited

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.

Mollisols
Fertile grassland soils with thick, dark topsoil. Among the best for agriculture, building, and gardening.
Alfisols
Moderately weathered forest soils with clay-enriched subsoil. Productive for agriculture, generally good for building and septic.
Vertisols
High-clay soils that shrink and swell dramatically. Fertile but challenging for foundations and septic systems.
Entisols
Young soils with little development — found on floodplains, dunes, and steep slopes. Properties vary widely by setting.

What This Means

Building & Foundations

About 98% of soils are rated "very limited" for dwellings with basements. Specific challenges include shallow bedrock, steep slopes, poor drainage in some areas, flood-prone areas. A geotechnical assessment is recommended before building.

Septic Systems

About 100% of soils are rated "very limited" for septic absorption fields. Despite good drainage overall, limitations may stem from shallow bedrock, steep slopes, or seasonal conditions. Engineered or alternative systems are frequently required. Always get a professional perc test before purchasing land that needs septic.

Gardening & Agriculture

Well-drained soils on sloped terrain — good for most plants but watch for erosion. Terracing, contour planting, and mulching help retain moisture and topsoil. Drip irrigation is more effective than sprinklers on slopes.

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