Foundation repair · Converse, TX

Foundation repair in Converse — new subdivisions on old Blackland clay.

Converse sits in the northeast corner of Bexar County, about fourteen miles from downtown San Antonio and right up against JBSA-Randolph. Unlike the limestone-and-clay patchwork of San Antonio proper, Converse is squarely on the flat Blackland Prairie — the USDA maps the dominant soil under most of the city as Houston Black, some of the most expansive clay in Texas.

1900s–60s1980s–90s2000s–nowSAME ANCIENT CLAY UNDER ALL THREESTABLE STRATA

That's the through-line for foundation work here: the older core near Randolph and the fast new growth toward Schertz sit on the same breathing clay, and each generation of housing meets it in its own way. We measure before we conclude anything — a lot of what looks structural in Converse is really a moisture story.

THE ORIGINAL TOWNSITE BY RANDOLPH TO THE FM 1516 AND 78244 GROWTH TOWARD SCHERTZ — A SHORT RUN NORTHEAST FROM OUR VANCE JACKSON SHOP.

What we see in Converse

The local patterns, specifically.

LOCAL PATTERN 01

Corner settlement after drought summers

The Blackland classic: a west- or south-facing corner bakes hardest and drops first. The stair-step crack cluster radiating from that corner is nearly diagnostic here.

LOCAL PATTERN 02

1970s–80s slabs near Randolph aging in

The original townsite's older, lighter slabs are now 40+ years into the clay cycle — more sensitive to the seasons than the post-2000 engineered pads out toward Schertz.

LOCAL PATTERN 03

New-section cracks in years 3–7

The FM 1516 and northeast subdivisions follow the corridor timing: pad consolidation plus a first hard drought, right as builder coverage ends. Hairlines normal; widening diagonals worth measuring.

LOCAL PATTERN 04

Drifted drainage in mature yards

Decades of beds, mulch, and patios quietly reverse the original grading in the older neighborhoods. Water standing at the slab after storms is a fixable cause we flag before it becomes a pier conversation — and where a cracked patio or walk is the culprit, our flatwork crew re-pours it to carry water away.

The local soil story: Converse rides the flat Blackland belt — deep Houston Black clay that swells hard in a wet spring and shrinks just as hard through a dry August. Without San Antonio's north-side limestone to steady it, the seasonal wet-dry cycle is the dominant story almost everywhere in town, concentrated at slab edges with the most sun and evaporation.

Straight from the soil survey

The USDA maps the dominant soil under Converse as Houston Black — very high shrink–swell (linear extensibility ≈ 12%). That’s some of the most active clay in the state — it swells in the wet and shrinks in drought, and that motion is exactly what foundation piers are built to outlast.

See the Houston Black soil series at USDA

The ground under the northeast side

Converse is flat Blackland clay — no limestone to steady it.

San Antonio's foundations sit on a three-way patchwork — limestone north, clay south and east, transition streets in between. Converse doesn't get that variety. Out here in the flat northeast corner of Bexar County, the ground is deep Blackland Prairie clay, and the USDA maps the dominant soil as Houston Black, a very-high-shrink-swell clay that can swell over an inch and shrink right back with the seasons. There's no shallow rock nearby to hold a slab edge steady, so the wet-dry cycle drives most of what we measure in town.

That actually makes diagnosis cleaner than in the city's patchwork. When one slab moves and the next-door neighbor's doesn't, the difference in Converse is rarely the underlying geology — it's lot-level detail: a downspout dumping at one corner, grading that drifted toward the house, trees drawing moisture out of one edge in a drought. Drought pulls the exposed edges down; the first big fall storm re-wets the dried clay and heaves it back unevenly. Most of the cracked drywall we're called about is that cycle, not a failing foundation — and the free measured inspection is what tells the difference.

Two generations of housing

An older core by Randolph, and a decade of new growth pushing toward Schertz.

Converse grew from a rural crossroads into one of the fastest-growing suburbs in the metro, its population up by half since 2010, and its foundations come in two clear eras. The original townsite closest to JBSA-Randolph holds the city's oldest and most established neighborhoods — smaller, modestly priced homes under mature trees, popular with military families for the gate proximity. Many of those slabs were poured to lighter, pre-modern standards and are now decades into the clay cycle, so seasonal door sticking and corner cracking are the common calls.

The newer Converse pushes northeast toward Schertz — the FM 1516 corridor and the 78244 subdivisions like Bradbury and Mission Hills, HOA-managed neighborhoods built through the 2000s and 2010s on engineered pads. Most perform well; where cut-and-fill met native clay at a lot edge, the seam shows up a few summers later as cracks near garage returns. Out on the larger acreage tracts like Quiet Creek, drainage across a half-acre lot becomes its own variable. Whatever the era, a dated elevation map is what turns a worry into a specific answer — and Converse is a short run from our Vance Jackson shop, inspected on the same free terms as San Antonio.

Neighborhood by neighborhood

Converse foundation repair, street level.

The original townsite (near Randolph)

The city's oldest core beside JBSA-Randolph: smaller 1970s–80s homes under mature trees. Lighter, older slabs decades into the clay cycle — seasonal door sticking and corner cracking are the common findings.

FM 1516 corridor

A decade of newer residential growth on engineered pads. Classic corridor timing: pad consolidation and the first hard drought around years 3–7 bring the earliest cracks, right as builder coverage ends.

Bradbury & Mission Hills (78244)

HOA-managed subdivisions built through the 2000s and 2010s, pushing northeast toward Schertz. Lot-edge fill seams where placed pads meet native clay telegraph as cracks near garage corners.

Quiet Creek & the acreage tracts

Larger lots — often a half-acre or more — where drainage across the property is its own variable. Grading that carries storm water toward the house is the finding we flag most on these.

Older FM 78 neighborhoods

Established streets with decades of incremental landscaping and additions. Drifted drainage and joints between construction eras crack first — often fixable before piers enter the conversation.

Our work near Converse

Real foundation repair across Converse and the corridor.

Foundation repair on a Central Texas home of the kind Motmot performs in Converse, TX
Pier and excavation work on homes like those across Converse and the northeast Bexar suburbs.
Stair-step cracks in brick above a window corner, typical of the exterior foundation damage Motmot repairs near Converse
Stair-step cracks in brick above a window corner — the Blackland-clay signature Motmot inspects on homes across Converse.
Diagonal drywall crack reaching a door frame corner, photographed during a foundation evaluation
Diagonal crack running to a door frame corner, the sort of interior symptom Motmot inspectors evaluate near Converse.
Gap under a baseboard at a room corner with stretched caulk, interior evidence of slab settlement
Gap under a baseboard at a room corner — interior settlement evidence like Motmot finds on homes near Converse.

Your nearest Motmot office

San Antonio (Main Office)

4402 Vance Jackson Rd Ste 206, San Antonio, TX 78230. Call or text (210) 816-0034.

Open 24 hours

Our main shop at Vance Jackson and Loop 410 runs the San Antonio metro daily — and a second office in San Marcos covers the upper corridor.

Converse specifics

Asked by Converse homeowners.

Not worse — more uniform. Converse sits consistently on the flat Blackland clay, without San Antonio's north-side limestone, so the wet-dry cycle is the dominant story almost everywhere in town. That predictability actually makes diagnosis cleaner.
Older, lighter slabs telegraph soil movement more readily, so age raises the odds — but it doesn't decide them. Plenty of Converse homes that era are stable and just need moisture management. The elevation survey tells you which case you have.
On this Blackland clay, yes — steady perimeter moisture in drought (a soaker hose about 18 inches from the slab, run consistently) prevents the shrink-settle cycle that causes most local damage. It's the cheapest foundation repair there is.
No — the northeast Bexar cluster, Converse included, is inside our normal daily run from the Vance Jackson shop. Inspections are free, with no trip fees and no minimums.
Almost certainly not. Early cracking in young Converse homes is overwhelmingly cosmetic settling and clay seasonality meeting fresh drywall. If readings show real movement inside your structural-warranty window, a dated elevation map is the evidence you take to the builder.

Nearby

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