Understanding the seven major soil series across Riverside, San Bernardino, and southwest IE cities, and what they mean for your landscape project. Reviewed and current as of September 2026.
Call (760) 792-7627In the High Desert, the biggest soil problem is caliche, a calcium carbonate hardpan that blocks drainage. In the Inland Empire, the nemesis is expansive clay, what most homeowners simply call heavy clay soil. Bonsall and Arlington series soils contain montmorillonite clay minerals that absorb water like a sponge, swelling 4-8% in volume when wet and shrinking back when dry. This cyclical movement, called shrink-swell, is the leading cause of cracked foundations, buckled driveways, tilted retaining walls, and heaved paver patios across the IE.
During Southern California’s dry months (May through November), clay soil contracts. Cracks 1-2 inches wide and several feet deep open across yards and along foundations. When winter rains arrive (December through March), the clay absorbs moisture and swells, generating lateral pressures exceeding 5,000 pounds per square foot against retaining walls, foundation stems, and hardscape edges. A 4-inch concrete slab sitting directly on Bonsall clay will crack within 2-3 seasonal cycles.
A geotechnical engineer measures expansive potential using Atterberg limits, the Liquid Limit (LL) and Plastic Limit (PL). The difference is the Plasticity Index (PI). Bonsall series soils commonly test at PI 25-40, classified as “high” to “very high” expansion potential. Any PI above 20 requires engineered solutions for hardscaping and structures. We order geotechnical reports on every IE project where clay is suspected.
Primary soil: Ramona sandy loam (terraces), Arlington clay loam (lowlands). USDA Zone: 10a. Elevation: 840 ft. The city’s older neighborhoods near downtown and Arlington Heights sit on excellent Ramona soil, well-drained sandy loam ideal for hardscaping and plantings. Low-lying areas near the Santa Ana River and Arlanza have Arlington clay with poor drainage. The UC Riverside campus area transitions between the two. Water district: Riverside Public Utilities.
Primary soil: Ramona sandy loam (central), Hanford alluvial (south near river). USDA Zone: 10a. Elevation: 735 ft. Corona’s “Circle City” core sits on Ramona sandy loam, stable, well-drained soil that supports most landscape projects without special engineering. South Corona near the Santa Ana River transitions to Hanford alluvial deposits. The Skyline Drive foothills have Vista DG patches. Water district: City of Corona Department of Water & Power.
Primary soil: Hanford sandy loam, Ramona sandy loam. USDA Zone: 10a. Elevation: 620 ft. “Horse Town USA” sits on prime alluvial soil from the Santa Ana River corridor. Hanford sandy loam dominates, deep, fast-draining, and easy to work. The large lot sizes (2+ acres typical) and equestrian properties mean substantial landscape projects. Soil compaction from horse traffic requires re-grading and amendment before planting. Water district: Norco Department of Water.
Primary soil: Hanford sandy loam (valley floor), Vista DG (north foothills). USDA Zone: 9b-10a. Elevation: 1,237 ft. North Fontana above Sierra Avenue climbs into the San Gabriel foothills where DG Vista soils and shallow bedrock dominate. South Fontana (the old steel mill area) sits on deep Hanford alluvial deposits, some of the easiest soil to work in the IE. Caliche has been found in isolated pockets near the I-15/I-10 interchange area. Water district: Fontana Water Company.
Primary soil: Alluvial fan (sandy loam/gravel), Vista DG (north foothills). USDA Zone: 9b-10a. Elevation: 1,100-2,400 ft. The city sits on the massive Cucamonga alluvial fan, deposited by Cucamonga and Day Creeks. Soil transitions from deep sandy loam at the I-10 corridor to increasingly rocky, DG-influenced soils above Baseline Road. Properties in the Etiwanda area and near the wilderness boundary often hit granitic bedrock at 2-3 feet. Water district: Cucamonga Valley Water District.
Primary soil: Hanford sandy loam (central), Arlington clay loam (south). USDA Zone: 10a. Elevation: 990 ft. Central and north Ontario sit on excellent Hanford alluvial soil from San Antonio Creek deposits. South Ontario near the airport and Ontario Mills transitions to Arlington clay loam with heavier texture and slower drainage. The old citrus groves (now residential subdivisions) left behind amended topsoil in some neighborhoods. Water district: City of Ontario Utilities.
Primary soil: Hanford sandy loam (valley), Fallbrook sandy clay loam (foothills), Bonsall clay (south). USDA Zone: 9b-10a. Elevation: 1,049 ft. The most geologically varied city in the IE. North San Bernardino climbs into the mountains on Fallbrook and Vista soils. The valley floor downtown sits on deep Hanford alluvium from the Santa Ana River. South San Bernardino near Loma Linda has pockets of Bonsall expansive clay. The San Andreas Fault runs through the city’s northern edge. Water district: San Bernardino Municipal Water Department.
Primary soil: Fallbrook sandy clay loam (dominant), Vista DG (upper elevations). USDA Zone: 9b. Elevation: 1,300-2,000 ft. Highland sits at the base of the San Bernardino Mountains. Fallbrook sandy clay loam is the workhorse soil here, well-drained with moderate clay content that holds moisture better than pure sand. Above East Highland, Vista DG takes over with shallow bedrock. The City Creek and Plunge Creek drainages deposit localized alluvial soils along their corridors. Water district: East Valley Water District.
Primary soil: Hanford sandy loam (valley), Vista DG (slopes), wind-deposited sand. USDA Zone: 9b. Elevation: 2,350 ft. Located in the San Gorgonio Pass, the windiest corridor in Southern California. Valley-floor soils are Hanford alluvial deposits from San Gorgonio Creek, but the constant wind deposits sand that buries topsoil and abrades plant tissue. Foothill slopes above I-10 have Vista DG with rapid drainage. Wind protection is the top landscaping priority here. Water district: Banning Water District.
Primary soil: Ramona sandy loam (plateaus), Fallbrook sandy clay loam (slopes). USDA Zone: 9b. Elevation: 2,650 ft. Beaumont sits on a plateau above the San Gorgonio Pass, giving it less wind exposure than neighboring Banning. The flat terrain has Ramona and similar sandy loams, stable, well-drained soils. The newer master-planned communities (Sundance, Fairway Canyon, Tournament Hills) were graded from native Ramona soil. Slopes and hills transition to Fallbrook. Water district: Beaumont-Cherry Valley Water District.
Primary soil: Bonsall expansive clay (dominant), Ramona sandy loam (ridgetops). USDA Zone: 10a. Elevation: 1,420 ft. Menifee has the highest concentration of Bonsall expansive clay in the IE. The city’s rapidly growing master-planned communities (Menifee Lakes, Audie Murphy Ranch, Heritage Lake) sit on clay with Plasticity Index values commonly exceeding 30. Cracked driveways and heaving sidewalks are widespread. Ridgetop neighborhoods have pockets of better-drained Ramona soil. Water district: Eastern Municipal Water District (EMWD).
Primary soil: Greenfield sandy loam (wine country), Bonsall clay (lowlands), Vista DG (east hills). USDA Zone: 10a. Elevation: 1,017 ft. Temecula’s wine country along Rancho California Road sits on Greenfield sandy loam, the same well-drained, mineral-rich soil that grows award-winning Tempranillo and Syrah. Old Town and areas near Murrieta Creek have heavier soils including Bonsall clay. Eastern Temecula toward the Santa Rosa Plateau transitions to Vista DG. Water district: Rancho California Water District (RCWD).
Primary soil: Greenfield sandy loam, Ramona sandy loam, Bonsall clay (south). USDA Zone: 10a. Elevation: 1,053 ft. Murrieta straddles the line between Greenfield wine country soils and Bonsall clay. Northern Murrieta and the I-215 corridor have Ramona and Greenfield sandy loams, the best soil conditions in the southwest IE. South Murrieta toward the Temecula Creek transitions to heavier Bonsall clay. The newer developments along Clinton Keith Road were graded from mixed native soils. Water district: Western Municipal Water District (WMWD).
Unincorporated areas between cities often have the most variable soils, alluvial wash deposits, caliche pockets, DG outcrops, and clay lenses can appear within a single parcel. The takeaway: Soil testing is not optional in the Inland Empire. A $25-50 basic test from UC Riverside Cooperative Extension or the IERCD can save thousands in failed hardscape, dead plants, and drainage retrofits. We run the USDA Web Soil Survey for every project address before our first site visit.
Every hardscape element, pavers, concrete, retaining walls, fire pits, sits on a base that sits on native soil. If the native soil moves, everything above it moves. In the Inland Empire, soil type determines base depth, drainage requirements, and long-term durability more than any other factor.
The Inland Empire has seven major soil series. Ramona sandy loam dominates Riverside and Corona terraces. Hanford sandy loam lines the Santa Ana River floodplain from Ontario to Norco. Greenfield sandy loam covers Temecula and Murrieta wine country. Fallbrook sandy clay loam sits on foothill areas in Highland and Banning. Vista series decomposed granite soils appear on granitic slopes throughout the region. Arlington clay loam creates drainage problems in low-lying Riverside and Ontario areas. Bonsall series expansive clay, the most challenging IE soil, causes shrink-swell damage in Menifee, Temecula, and parts of San Bernardino.
Three signs: wide cracks in your yard during dry months (sometimes 1-2 inches wide and several feet deep), sticky mud that clings to shoes after rain, and doors or windows in your home that stick seasonally as the foundation shifts. You can do a simple jar test, put soil in a mason jar with water, shake it, and let it settle for 24 hours. If the top layer (clay) makes up more than 30% of the total, you have significant clay content. For definitive results, send a sample to a soil lab for a Proctor compaction test and Atterberg limits analysis, which will give you the Plasticity Index (PI), anything over 20 is highly expansive.
Yes, but you need a deeper base than standard ICPI specs call for on stable soil. On Bonsall or Arlington clay, excavate 10-12 inches deep instead of the standard 6-8 inches. Install 6-8 inches of Class II road base compacted in 2-inch lifts to 95% Proctor density, then 1 inch of bedding sand. The thicker base acts as a buffer against shrink-swell movement. We also recommend a geotextile fabric between the native clay and the base material to prevent clay migration. French drains along the perimeter keep water from saturating the clay beneath the paver field.
It depends on your specific soil type. In sandy Ramona and Hanford soils (Riverside, Corona, Ontario), most Mediterranean and drought-tolerant plants thrive, Bougainvillea, Citrus, Lavender, Rosemary, and California Pepper trees. In clay-heavy Bonsall and Arlington soils (Menifee, parts of San Bernardino), choose plants that tolerate wet feet in winter and drought in summer, California Sycamore, Toyon, Western Redbud, and native bunch grasses. In DG Vista soils (foothill areas), desert-adapted species perform best, Desert Willow, Manzanita, Ceanothus, and Agave. The IE sits in USDA Zones 9b-10a, which is warmer than the High Desert and supports a wider range of subtropical species.
On expansive clay (Bonsall or Arlington series), the footing should extend at least 24 inches below grade, deeper than the 18-inch minimum on stable soil. The footing width should be twice the wall thickness. Use a concrete footing with #4 rebar on 16-inch centers rather than a compacted gravel base. The concrete footing resists the lateral pressure that expansive clay exerts when wet. Most IE jurisdictions require a building permit for walls over 3-4 feet, and the geotechnical report will specify the exact footing depth based on the Plasticity Index of your specific soil.
Sandy loam soils like Ramona and Hanford (found in Riverside, Corona, Norco, Ontario) are excellent for warm-season turf grasses like Bermuda and St. Augustine. They drain well and warm up quickly in spring. Clay soils like Bonsall and Arlington are more difficult, they stay waterlogged in winter (causing fungal diseases) and crack in summer (tearing root systems). On clay, consider artificial turf or drought-tolerant groundcovers instead. Regardless of soil type, the IE’s USDA Zone 9b-10a climate and 12-15 inches of annual rainfall mean you will need irrigation for any natural lawn, expect to water 3-4 days per week in summer.
The UC Riverside Cooperative Extension offers soil testing services and interpretation for homeowners. The Inland Empire Resource Conservation District (IERCD) runs periodic free soil testing programs. For construction projects requiring geotechnical analysis (retaining walls, foundations, large hardscape installations), hire a licensed geotechnical engineer who will perform Proctor compaction tests, Atterberg limits, and sieve analysis. Commercial labs like Alluvial Soil Lab also serve the IE region. A basic pH and nutrient test costs $25-50; a full geotechnical report runs $1,500-3,000.
Expansive clay soil is the primary cause. Bonsall and Arlington series soils swell when wet and shrink when dry, creating cyclical ground movement that standard 4-inch residential slabs cannot withstand. In neighborhoods built on these soils, common in Menifee, parts of Temecula, south San Bernardino, and low-lying Ontario, you will see cracked driveways, buckled sidewalks, and foundation issues. The fix for new concrete is a thicker slab (5-6 inches), #4 rebar on 12-inch centers instead of wire mesh, control joints every 8 feet, and a 4-6 inch compacted gravel sub-base to buffer the clay movement. Proper grading to direct water away from the slab is equally important.
Only when the clay is sodium-affected, which a soil test identifies (look for an SAR above 13). Most Inland Empire clay is expansive montmorillonite, not sodic, so bagged gypsum does very little. Composted organic matter worked into the top 12 inches, drainage that routes water away from the clay, and clay-tolerant plants outperform gypsum in almost every IE yard.
For heavy clay, tall fescue blends tolerate the slow drainage better than most warm-season grasses. For sandy, fast-draining soil in full sun, hybrid Bermuda performs well on less water. Where the soil fights every option, artificial turf sidesteps soil quality entirely and stays green through both extremes, which is why turf conversions are common on the toughest IE lots.
Ramona sandy loam terraces, Arlington clay lowlands. USDA Zone 10a. RPU water district. From Canyon Crest to La Sierra, soil changes dramatically across neighborhoods.
Riverside LandscapingRamona sandy loam core, Hanford alluvial near the river, Vista DG in the foothills. Zone 10a. Well-drained soil for most projects.
Corona LandscapingHanford and Ramona sandy loam, prime alluvial soil from the Santa Ana River. Zone 10a. Large equestrian lots with substantial landscape potential.
Norco LandscapingHanford sandy loam (valley), Vista DG (north foothills). Zone 9b-10a. South Fontana has deep, easy-to-work alluvial deposits.
Fontana LandscapingCucamonga alluvial fan soils, sandy loam at I-10, increasingly rocky DG above Baseline. Zone 9b-10a. Bedrock at 2-3 ft in north areas.
Rancho Cucamonga LandscapingHanford sandy loam (central/north), Arlington clay loam (south near airport). Zone 10a. Former citrus groves left amended topsoil in some areas.
Ontario LandscapingMost geologically varied IE city. Hanford alluvium (valley), Fallbrook clay loam (foothills), Bonsall clay (south). Zone 9b-10a. San Andreas Fault at north edge.
San Bernardino LandscapingFallbrook sandy clay loam at the mountain base. Vista DG at upper elevations. Zone 9b. Shallow bedrock above East Highland limits excavation depth.
Hanford alluvial (valley), Vista DG (slopes), wind-deposited sand. Zone 9b. San Gorgonio Pass wind is the top landscape factor here.
Ramona sandy loam on plateaus, Fallbrook on slopes. Zone 9b. Less wind than Banning. Good soil conditions in newer developments.
Highest concentration of Bonsall expansive clay in the IE. PI values often exceed 30. Cracked driveways and heaving sidewalks are common across master-planned communities.
Greenfield sandy loam in wine country, Bonsall clay in lowlands, Vista DG in east hills. Zone 10a. Soil varies dramatically within the city.
Temecula LandscapingGreenfield and Ramona sandy loams (north), Bonsall clay (south toward Temecula Creek). Zone 10a. North Murrieta has the best soil in the southwest IE.
Unincorporated areas have the most variable soils. Always test before building. We run USDA Web Soil Survey for every project address before our first site visit.
IE LandscapingOur team has built hundreds of landscapes across every soil type in the Inland Empire. We test your soil, engineer the right base, and build to last, not just to look good on day one.
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