Upper Trinity (Paluxy and Glen Rose): how deep the wells are
Home water wells that draw from the upper Trinity (Paluxy and Glen Rose) in North and Central Texas are typically 200 to 400 feet deep (median 280 ft, 9,322 wells drilled in the last 10 years). In the state's model it is sandstone, limestone and marl. It carries the most weight in Tarrant County (87% of its wells), Denton County (86% of its wells) and Cooke County (62% of its wells). Estimated cost of a complete well at the median depth: $9,500 to $23,500.
Updated every day from Texas Water Development Board driller reports. Last update: November 11, 2026, using the state file of November 10, 2026.
Under Weatherford, Parker County
Dot: median. Bar: middle half (25th to 75th percentile). Counties with the most wells in this layer.
Digging in…
What this layer is
This group is the upper half of the Trinity in North and Central Texas: the Paluxy sand on top and the Glen Rose limestone and marl under it. The state's model draws them as two layers, but our check against the state's own aquifer codes shows the method cannot tell them apart reliably, so this atlas reports them together. North and west of Fort Worth the limestone gives way to sand and both become the upper part of the undivided Antlers Formation.
Units the model puts in this layer: Paluxy Formation; upper part of the Antlers Formation in the north and west; Glen Rose Formation; middle part of the Antlers Formation in the north and west.
Source of the layers: TWDB's Northern Trinity and Woodbine model, with quarter mile cells, summarized here to about 1.3 miles.
Key figures
- Typical depth (middle half)
- 200 to 400 feet
- Median depth
- 280 feet
- Deepest 10% are past
- 539 feet
- Water level (median)
- 170 feet
- 5,214 wells
- Yield (median)
- 15 gpm
- 7,261 wells, gallons per minute
- Wells used
- 9,322
- In the last 10 years
- All years on file
- 20,068
- median 260 ft, since 1998
- Confidence
- Standard (30 or more wells)
Counties where homes draw from this layer
Only counties with at least 10 wells in the layer. The share is of the county's wells that the model covers.
| County | Median depth (ft) | Wells | Share of the county's wells |
|---|---|---|---|
| Parker County | 220 | 3,795 | 54% |
| Tarrant County | 350 | 1,489 | 87% |
| Wise County | 220 | 1,261 | 36% |
| Denton County | 460 | 760 | 86% |
| Johnson County | 500 | 569 | 51% |
| Cooke County | 500 | 393 | 62% |
| Williamson County | 810 | 189 | 15% |
| Bosque County | 238 | 140 | 35% |
| Erath County | 140 | 136 | 9% |
| Hood County | 280 | 117 | 12% |
| Hill County | 500 | 107 | 30% |
| Montague County | 220 | 92 | 13% |
| Bell County | 780 | 84 | 16% |
| Grayson County | 432 | 55 | 15% |
| Hamilton County | 135 | 30 | 6% |
| Somervell County | 280 | 25 | 18% |
| Coryell County | 388 | 22 | 8% |
| Travis County | 445 | 22 | 2% |
| Burnet County | 505 | 18 | 1% |
| Lampasas County | 360 | 11 | 3% |
Places where it is the main layer
- Weatherford 300 ft
- Fort Worth 395 ft
- Peaster 220 ft
- Carter 240 ft
- Annetta 328 ft
- Annetta South 325 ft
- Azle 200 ft
- New Fairview 220 ft
- Decatur 250 ft
- Briar 200 ft
- Pecan Acres 320 ft
- Denton 522 ft
- Benbrook 400 ft
- Springtown 240 ft
- Reno 200 ft
- Rhome 272 ft
- Annetta North 240 ft
- Cresson 300 ft
- Cleburne 500 ft
- Willow Park 240 ft
- Godley 500 ft
- Hudson Oaks 220 ft
- Cedar Park 750 ft
- Ponder 460 ft
- Aurora 220 ft
- Newark 220 ft
- Aledo 250 ft
- Lakeside (Tarrant County) 208 ft
- Burleson 600 ft
- Sanger 450 ft
Where it sits among the model's layers
From top to bottom, with the median depth of the home wells that draw from each:
| Layer (state's model) | Rock | Median depth (ft) | Wells |
|---|---|---|---|
| Above the Woodbine | shale, chalk and marl | 160 | 1,739 |
| Woodbine | sandstone with shale | 260 | 1,037 |
| Washita and Fredericksburg | limestone, marl and clay | 240 | 1,050 |
| Upper Trinity (Paluxy and Glen Rose) | sandstone, limestone and marl | 280 | 9,322 |
| Lower Trinity (Twin Mountains and Travis Peak) | sandstone with shale and limestone | 340 | 12,230 |
Depth over time
Home well depth in this layer has not changed meaningfully in 20 years: the median was 250 feet in 2003 to 2007 and 260 feet in 2021 to 2025 (a difference under 10% or within the margin of error).
| Period | Median depth (ft) | Wells |
|---|---|---|
| 2001–2005 | 270 | 2,943 |
| 2006–2010 | 240 | 3,887 |
| 2011–2015 | 275 | 3,206 |
| 2016–2020 | 280 | 4,270 |
| 2021–2025 | 260 | 5,204 |
| 2026 | 280 | 553 |
Common questions
How deep is a well in the upper Trinity (Paluxy and Glen Rose)?
Home water wells that draw from the upper Trinity (Paluxy and Glen Rose) in North and Central Texas are typically 200 to 400 feet deep (median 280 ft, 9,322 wells drilled in the last 10 years).
What is the upper Trinity (Paluxy and Glen Rose)?
This group is the upper half of the Trinity in North and Central Texas: the Paluxy sand on top and the Glen Rose limestone and marl under it. The state's model draws them as two layers, but our check against the state's own aquifer codes shows the method cannot tell them apart reliably, so this atlas reports them together. North and west of Fort Worth the limestone gives way to sand and both become the upper part of the undivided Antlers Formation.
How deep does the water stand in these wells?
When the wells were finished, the water stood a median 170 feet below the surface (5,214 wells).
What a well in this layer costs
At the median depth for this layer (280 feet), a complete home well would cost roughly $9,500 to $23,500: $25 to $60 per foot for drilling, casing and seal, plus $2,500 to $6,500 for the pump, pressure tank, controls and hookup at the well. Across the whole middle half of depths (200 to 400 feet) the range runs from $7,500 to $30,500. This is TerraFunded's estimate from published Texas prices, not a quote, and it leaves out trenching and the line to the house. Get prices from at least two licensed drillers.
How these numbers are made
We count new and replacement domestic (home) wells with a valid depth on their report. We use the last 10 years when there are at least 30 wells; otherwise all since 2001. The median is the middle well and the middle half runs from the 25th to the 75th percentile.
To tell which layer a well draws from, we take the ground elevation at its location, subtract the depth of the interval where water enters (or the bottom of the hole when the report does not give one) and see which layer of the state's model that point falls in.
For 98% of these wells the report says where the water enters (the screen or the open hole), and we use the middle of that interval.
How well it works: In 7,977 wells in the area of the state's Northern Trinity and Woodbine model (North and Central Texas) where the State of Texas recorded the aquifer, our estimate of the formation the well draws from names the same layer of the state's model in about 74% of them, and that layer or the one next to it in at least 95%; among the 3,130 of those wells that the state places in a Trinity layer (Paluxy to Hosston) it is about 56%.
- The layers come from the Texas Water Development Board's Northern Trinity and Woodbine model, with quarter mile cells, summarized here to about 1.3 miles. It is a regional model, not a survey of any lot: between one model point and the next, the real depth of each layer can differ.
- In this model every layer is at least 30 feet thick, even where the real rock is thinner or missing. Thin layers and the edges of the model are approximate.
- Inside the Trinity this atlas does not name single model layers: it groups the Paluxy and Glen Rose (upper Trinity) and groups the Hensell, Pearsall and Hosston (lower Trinity, Twin Mountains and Travis Peak), because the check against the state's codes shows the method cannot separate them reliably.
- "Near or below the base of the Trinity" means the well reaches the bottom of the model or passes it, often by tens of feet. Older rock that the model does not include may lie there.
- We never use the model's water levels. The water level on this page is the one each driller measured when the well was finished.
These are depths of real wells drilled nearby, not a promise about any property. Groundwater can change over short distances and with drought. A licensed water well driller can tell you what to expect on a specific tract.
Read the full methodology · Download the data (CSV, CC BY 4.0)
How to cite
TerraFunded (2026). Texas Well Atlas: Underground. From Texas Water Development Board driller reports and groundwater availability models (data as of November 10, 2026). https://terrafunded.com/wells/formations/paluxy-glen-rose. License CC BY 4.0. https://doi.org/10.5281/zenodo.24126380.
Sources
- Submitted Driller's Reports database, Texas Water Development Board (TWDB) (file of November 10, 2026)
- Hydrogeology and Documentation of the Northern Trinity and Woodbine Aquifer System Groundwater Availability Model (NTGAM). Ellis, J., Prieto-Estrada, A., Osborne, A., Deeds, N., White, J., and Keester, M. (INTERA Incorporated), for the North Texas Groundwater Conservation District and Groundwater Management Area 8, 2025, GAM v3.01. TWDB groundwater availability model.
- Ground elevation: Terrain Tiles (Mapzen), Registry of Open Data on AWS
- TWDB well report viewer (each well's official report)
