Maverick County, Texas

Survey Area TX323 Texas

The dominant drainage class is Well drained and the dominant hydrologic group is D (very slow infiltration, high runoff). The most common soil order is Aridisols — dry-climate soils with limited organic matter and often calcium carbonate accumulation. 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 Maverick County, Texas. Search your address to find the exact soil composition, drainage, and series details at your specific location.

Soil Map UnitAcresDrainageHydro GroupDwellingsSeptic
Montell clay association, 0 to 1 percent slopes 105K Moderately well drainedDVery limitedVery limited
Copita sandy clay loam, 0 to 3 percent slopes 103K Well drainedCSomewhat limitedVery limited
Elindio association, nearly level 92K Well drainedBSomewhat limitedSomewhat limited
Pryor association, undulating 82K Well drainedCVery limitedVery limited
Catarina clay, association, 0 to 5 percent slopes 67K Moderately well drainedDVery limitedVery limited
Jimenez association, rolling 60K Well drainedDVery limitedVery limited
Brundage fine sandy loam, 0 to 1 percent slopes, occasionally flooded 49K Moderately well drainedDVery limitedVery limited
Dant association, gently undulating 49K Well drainedCSomewhat limitedVery limited
Maverick association, undulating 31K Well drainedDVery limitedVery limited
Mavco association, gently undulating 22K Well drainedBSomewhat limitedSomewhat limited
Olmos very cobbly loam, 0 to 4 percent slopes 18K Well drainedDVery limitedVery limited
Zapata association, undulating 18K Well drainedDVery limitedVery limited
Copita sandy clay loam, 1 to 3 percent slopes 15K Well drainedCSomewhat limitedVery limited
Verick fine sandy loam, 1 to 5 percent slopes 14K Well drainedDVery limitedVery limited
Brystal fine sandy loam, 0 to 3 percent slopes 12K Well drainedBNot limitedSomewhat limited
Water 11K DNot ratedNot rated
Elindio silty clay loam, 1 to 3 percent slopes 8K Well drainedBSomewhat limitedSomewhat limited
Elindio silty clay loam, 0 to 1 percent slopes 7K Well drainedBSomewhat limitedSomewhat limited
Montell clay, 0 to 1 percent slopes 7K Moderately well drainedDVery limitedVery limited
Lagloria very fine sandy loam, 0 to 1 percent slopes 6K Well drainedBNot limitedSomewhat 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.

Aridisols
Dry-climate soils with low organic matter. Often have caliche layers that make excavation difficult. Low shrink-swell is good for foundations.
Mollisols
Fertile grassland soils with thick, dark topsoil. Among the best for agriculture, building, and gardening.
Inceptisols
Young but developing soils found in mountains and river terraces. Variable properties — check drainage and bedrock depth.
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.
Alfisols
Moderately weathered forest soils with clay-enriched subsoil. Productive for agriculture, generally good for building and septic.

What This Means

Building & Foundations

About 58% of soils are rated "very limited" for dwellings with basements. Specific challenges include shallow bedrock, flood-prone areas. A geotechnical assessment is recommended before building.

Septic Systems

About 79% 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

Drainage is generally favorable for gardening. Adding compost and mulch will improve fertility and water retention. Test your soil's pH before planting — most vegetables prefer 6.0-7.0.

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