Planning a well in Ellis County?

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

Water Well Drilling & Service in Ellis County, Texas

Ellis County sits over the Woodbine aquifer system (deep confined subcrop; ~100–1,400 ft beneath Ellis County). Most residential wells target the Woodbine Formation / Woodbine Aquifer; depth varies meaningfully across the county and is best estimated from neighboring TWDB well records. Drilling is regulated by the Prairielands GCD, which requires a pre-drilling permit. Local water quality consideration: A TWDB/BEG report puts the county's total dissolved solids (TDS, a measure of how mineral-heavy water is) from 310 mg/L in the alluvium to 3,040 mg/L in the Paluxy.

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

About this diagram

This cross-section shows the actual rock formations beneath Ellis County, from topsoil down to the Woodbine 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 Ellis County, Texas stratigraphy — Topsoil, Taylor Group / younger Upper Cretaceous marl, chalk, and clay, Austin Chalk, Eagle Ford Shale, Woodbine Formation / Woodbine Aquifer, Washita and Fredericksburg Groups, and the Woodbine aquifer at the base.
Hover or tap a layer in the cube to see formation details.

Ellis County stratigraphy — top to bottom

Topsoil — Blackland Prairie (Houston Black)

0–15 ft

Dark black clay that swells and shrinks with moisture (shrink-swell).
Austin Chalk

varies

Thick white chalky limestone — the near-surface bedrock across most of Ellis County. Where it is cracked or weathered it can carry a little shallow water, but that is site-specific and not a reliable household source.
Water-quality consideration
Eagle Ford Shale

below Austin Chalk

Dark gray organic shale; another regional seal that water does not pass through.
Woodbine Formation / Woodbine Aquifer

100–1,400 (variable across county) ft

The main household water source in Ellis County. Its top ranges from about 100 ft to 1,400 ft across the county (a BEG report near the SSC site puts it at 600–1,000 ft there), so depth varies a lot by location. Wells usually finish in the lower part for cleaner water. The rock is medium-to-coarse iron-rich sandstone with clay and lignite (a soft coal) seams; TWDB Report 62 lists it as a principal Ellis County water-bearing formation.
Primary aquifer target
Trinity Group: Paluxy / Glen Rose / Hensell / Hosston (= Twin Mountains)

~2,000–3,000 (Hosston/Twin Mountains) ft

The deep backup target, at roughly 2,000–3,000 ft beneath Ellis County. Going for it means real depth, and quality worsens enough eastward that the eastern third of the county rarely uses it. The Prairielands GCD names these Trinity layers Paluxy, Glen Rose, Hensell, and Hosston; the Hosston is the same sand called the Twin Mountains in north-central Texas.
Aquifer

Ellis County Quick Facts

Primary Aquifer
Woodbine

Secondary: Trinity (deep — Hosston/Twin Mountains at ~2,000–3,000 ft)

Typical Well Depth
Varies by location

We estimate from nearby well records

Groundwater District
Prairielands GCD
Confinement
deep confined subcrop; ~100–1,400 ft beneath Ellis County

Water Quality Notes

  • A TWDB/BEG report puts the county's total dissolved solids (TDS, a measure of how mineral-heavy water is) from 310 mg/L in the alluvium to 3,040 mg/L in the Paluxy
  • Most Paluxy, Woodbine, and Twin Mountains water here tops the EPA's 500 mg/L secondary TDS standard; only the alluvium stays below it
  • Water is hard, picking up minerals from the limestone and chalk above
  • Quality varies across the county — Midlothian and the northwest sit nearer where the aquifer surfaces and refills, while Ennis and the southeast lie farther downdip (deeper, where the layer tilts down), meaning deeper wells and more minerals
  • Many Ellis County properties rely on city water rather than a private well

Cities We Serve in Ellis County

What's Under Ellis County: the Geology Story

Drilling in Ellis County means starting in topsoil, working through Quaternary alluvium / terrace (Trinity River, Chambers Creek), Taylor Group / younger Upper Cretaceous marl, chalk, and clay, Austin Chalk, Eagle Ford Shale, to reach the Woodbine Formation / Woodbine Aquifer — the producing zone for most domestic wells.

The full layer-by-layer stratigraphy is laid out under the cube above. Well depth in Ellis 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 Ellis County

Ellis County wells are regulated by the Prairielands GCD. A pre-drilling permit is required before any new well is constructed. DFW Well Service submits the permit application as part of our drilling process.

Full Ellis County permit & regulations →

Frequently Asked Questions about Ellis County Wells

What aquifer is under Ellis County?
Ellis County wells primarily produce from the Woodbine aquifer system (deep confined subcrop; ~100–1,400 ft beneath Ellis County). Trinity (deep — Hosston/Twin Mountains at ~2,000–3,000 ft) is a secondary target in parts of the county.
How deep are wells typically drilled in Ellis County?
Residential well depth in Ellis 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 Ellis County wells?
A TWDB/BEG report puts the county's total dissolved solids (TDS, a measure of how mineral-heavy water is) from 310 mg/L in the alluvium to 3,040 mg/L in the Paluxy. Most Paluxy, Woodbine, and Twin Mountains water here tops the EPA's 500 mg/L secondary TDS standard; only the alluvium stays below it. Water is hard, picking up minerals from the limestone and chalk above. Quality varies across the county — Midlothian and the northwest sit nearer where the aquifer surfaces and refills, while Ennis and the southeast lie farther downdip (deeper, where the layer tilts down), meaning deeper wells and more minerals. Many Ellis County properties rely on city water rather than a private well. Water testing after drilling — and periodically thereafter — is recommended for every private well in the county.
Does Ellis County require a permit to drill a water well?
Yes. You must register a well before drilling under the Prairielands GCD's Rule 2.1, which kicks in by pumping capacity (17.36 gpm). The Prairielands GCD — the local district that permits wells — covers Ellis, Hill, Johnson, and Somervell counties. See the Ellis County permit and regulations page for the full process.
What's the main producing formation in Ellis County?
The primary producing formation is the Woodbine Formation / Woodbine Aquifer — The main household water source in Ellis County. Its top ranges from about 100 ft to 1,400 ft across the county (a BEG report near the SSC site puts it at 600–1,000 ft there), so depth varies a lot by location. Wells usually finish in the lower part for cleaner water. The rock is medium-to-coarse iron-rich sandstone with clay and lignite (a soft coal) seams; TWDB Report 62 lists it as a principal Ellis County water-bearing formation. Most Ellis County residential wells are completed in this interval.

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