Planning a well in Dallas County?

Welcome to Dallas County, Texas — DFW Well Service provides water well drilling and pump repair across Dallas County

Water Well Drilling & Service in Dallas County, Texas

Dallas County sits over the Trinity (deep, confined) aquifer system (deep, confined, downdip). Most residential wells target the Trinity Group (Paluxy, Glen Rose, Twin Mountains); depth varies meaningfully across the county and is best estimated from neighboring TWDB well records. Dallas County sits outside all groundwater conservation districts — TDLR standards govern. Local water quality consideration: Deep Trinity water in Dallas County often runs hot — roughly 90–100°F or more — and high in total dissolved solids (TDS, a measure of how mineral-heavy the water is); a Lancaster-area Trinity sample measured 2,038 mg/L TDS.

What’s Under Dallas County: a Layer-by-Layer Look

About this diagram

This cross-section shows the actual rock formations beneath Dallas County, from topsoil down to the Trinity (deep, confined) aquifer system.

Tap any layer in the image, or any layer in the list, to explore each layer and what it means for drilling a well on your property.

Isometric geological cross-section cube illustration showing Dallas County, Texas stratigraphy — Topsoil, Quaternary alluvium / terrace (Trinity River corridor only), Taylor Group (eastern Dallas County only), Austin Chalk, Eagle Ford Group, Washita and Fredericksburg confining units, Trinity Group (Paluxy, Glen Rose, Twin Mountains), and the Trinity (deep, confined) aquifer at the base.
Hover or tap a layer in the cube to see formation details.

Dallas County stratigraphy — top to bottom

Topsoil — Blackland Prairie vertisol

0–12 ft

Dark gray-black clay with heavy shrink-swell — it swells when wet and shrinks when dry.
Austin Chalk

varies

Thick chalk and limestone that forms the White Rock escarpment; water barely moves through it, so it acts as a seal, with only the occasional flow through cracks.
Eagle Ford Group

below Austin Chalk

Dark shale and mudstone; a regional barrier layer (an aquitard) that water does not pass through.
Woodbine Group

600–1,500 ft

A minor water-bearing sandstone where it is developed, layered with shale and clay. In Dallas County it sits roughly 600–1,500 ft down — far deeper than an ordinary household well reaches.
Water-quality consideration Aquifer

Dallas County Quick Facts

Primary Aquifer
Trinity (deep, confined)

Secondary: Woodbine (deep, confined)

Typical Well Depth
Varies by location

We estimate from nearby well records

Groundwater District
No GCD — TDLR standards only
Confinement
deep, confined, downdip

Water Quality Notes

  • Deep Trinity water in Dallas County often runs hot — roughly 90–100°F or more — and high in total dissolved solids (TDS, a measure of how mineral-heavy the water is); a Lancaster-area Trinity sample measured 2,038 mg/L TDS
  • Below about 1,500 ft, Woodbine water tends to exceed the EPA's secondary TDS limit
  • The upper Woodbine zone is high in iron and manganese, so it usually needs filtration
  • The Dallas County Trinity sits far downdip (far down where the layer tilts deep) from the Parker and Wise County belt where it surfaces and refills, so these wells do not replenish from local rainfall in any practical timeframe

City We Serve in Dallas County

What's Under Dallas County: the Geology Story

Drilling in Dallas County means starting in topsoil, working through Quaternary alluvium / terrace (Trinity River corridor only), Taylor Group (eastern Dallas County only), Austin Chalk, Eagle Ford Group, Woodbine Group, Washita and Fredericksburg confining units, to reach the Trinity Group (Paluxy, Glen Rose, Twin Mountains) — the producing zone for most domestic wells.

The full layer-by-layer stratigraphy is laid out under the cube above. Well depth in Dallas County varies by property location and overburden thickness; your driller can review TWDB records for neighboring wells to refine the expected completion zone before drilling.

Permits & Regulations in Dallas County

Dallas County sits outside all groundwater conservation districts. TDLR well construction standards govern, and your driller must be TDLR-licensed.

Full Dallas County permit & regulations →

Frequently Asked Questions about Dallas County Wells

What aquifer is under Dallas County?
Dallas County wells primarily produce from the Trinity (deep, confined) aquifer system (deep, confined, downdip). Woodbine (deep, confined) is a secondary target in parts of the county.
How deep are wells typically drilled in Dallas County?
Residential well depth in Dallas County varies meaningfully with property location and the producing formation, so there's no single countywide figure we can responsibly quote. Your driller can review TWDB well records for neighboring properties to estimate the expected depth before drilling, and the per-formation geology of the county is laid out on this page.
What water quality issues are common in Dallas County wells?
Deep Trinity water in Dallas County often runs hot — roughly 90–100°F or more — and high in total dissolved solids (TDS, a measure of how mineral-heavy the water is); a Lancaster-area Trinity sample measured 2,038 mg/L TDS. Below about 1,500 ft, Woodbine water tends to exceed the EPA's secondary TDS limit. The upper Woodbine zone is high in iron and manganese, so it usually needs filtration. The Dallas County Trinity sits far downdip (far down where the layer tilts deep) from the Parker and Wise County belt where it surfaces and refills, so these wells do not replenish from local rainfall in any practical timeframe. Water testing after drilling — and periodically thereafter — is recommended for every private well in the county.
Does Dallas County require a permit to drill a water well?
Dallas County has no groundwater conservation district (a GCD — the local body that would otherwise permit wells), so no local drilling permit is required; Texas TDLR well-construction standards apply instead. TDLR well construction standards still apply, and your driller must be TDLR-licensed.
What's the main producing formation in Dallas County?
The primary producing formation is the Trinity Group (Paluxy, Glen Rose, Twin Mountains) — Deep, sealed-in sand and limestone (confined — capped by rock above). This is technically the primary aquifer, but at 2,000–3,500+ ft it is out of reach for an ordinary home well; the deep Trinity wells that do exist here are usually municipal, industrial, or large-estate. State monitoring wells in the Twin Mountains sit at 2,568 ft (Well 3325202) and 3,076 ft (Well 3319101), both confined. Most Dallas County residential wells are completed in this interval.

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