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Water wells in the Edwards-Trinity (High Plains) Aquifer, Hale County, Texas

Only 26 home water wells that draw from the Edwards-Trinity (High Plains) Aquifer in Hale County, Texas have been reported since 2001, so treat this as a rough guide: the middle half are 156 to 233 feet deep (median 219 ft). It accounts for 10% of the 221 county wells the state's model covers; the main layer is the Ogallala Aquifer (50%). They run about 85 feet shallower than the county's median well (304 ft). Estimated cost of a complete well at the median depth: $8,000 to $19,500.

Checked against the state's own aquifer codes: where our method names this group, the state agrees in 70% of 4,432 wells (64% for the 571 with a screened interval on their report). Read it as the likely group, not a certain one.

This page is based on fewer than 30 wells, so it is kept out of search engines until more reports come in. Treat every figure as a rough guide.

Updated every day from Texas Water Development Board driller reports. Last update: November 11, 2026, using the state file of November 10, 2026.

All wells in Hale CountyEdwards-Trinity (High Plains) Aquifer across Texas

Which layer Hale County wells draw from

Under Abernathy, Hale County

County home wells covered by the High Plains Aquifer System model (in the last 10 years).

Home wells in Hale County

Each dot is a home well from a state driller report, colored by depth. Tap one for its details and official report. Tap an empty spot to see what is under that point.

See underground

Well depth (ft)

  • <100
  • 100
  • 200
  • 300
  • 400
  • 600
  • 800+

Dark line: Hale County

Key figures

Typical depth (middle half)
156 to 233 feet
Median depth
219 feet
Deepest 10% are past
241 feet
Wells used
26
Since 2001
Share of the county's wells
10%
All years on file
26
median 219 ft, since 2004
Confidence
Few wells (10 to 29)

Which layer Hale County wells draw from

County home wells covered by the High Plains Aquifer System model (in the last 10 years).

What this layer is

Under the Ogallala, in many places, lie Cretaceous rocks: the Antlers (Trinity) sand and the Edwards limestones. They form the Edwards-Trinity (High Plains) Aquifer around and south of Lubbock and the Edwards-Trinity (Plateau) Aquifer around Midland and Odessa, and older Cretaceous and Jurassic sandstones form the Rita Blanca Aquifer in Dallam and Hartley counties. Many home wells in Midland, Martin, Terry, Lynn and Hockley counties draw from them.

More about the Edwards-Trinity (High Plains) Aquifer

Depth over time

Too few wells per period in this layer in Hale County to compare depth over time. Since 2004, 26 home wells have been reported, with a median of 219 feet.

PeriodMedian depth (ft)Wells
2001–2005under 10 wells3
2006–2010under 10 wells1
2016–2020under 10 wells7
2021–202522414
2026under 10 wells1

Places in Hale County with wells in this layer

Common questions

How deep is a well in the Edwards-Trinity (High Plains) Aquifer in Hale County?

Only 26 home water wells that draw from the Edwards-Trinity (High Plains) Aquifer in Hale County, Texas have been reported since 2001, so treat this as a rough guide: the middle half are 156 to 233 feet deep (median 219 ft).

How many Hale County wells draw from this layer?

It accounts for 10% of the 221 county wells the state's model covers; the main layer is the Ogallala Aquifer (50%). For 85% of these wells the report says where the water enters and we use the middle of that interval; for the rest we use the bottom of the hole, which tends to read one layer too deep.

What a well costs here

At the median depth for this layer in Hale County (219 feet), a complete home well would cost roughly $8,000 to $19,500: $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 (156 to 233 feet) the range runs from $6,500 to $20,500. 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 85% of these wells the report says where the water enters and we use the middle of that interval; for the rest we use the bottom of the hole, which tends to read one layer too deep.

How well it works: In 22,814 wells in the Texas part of the state's High Plains Aquifer System model (the Panhandle, the South Plains and the Permian Basin) where the State of Texas recorded the aquifer, the formation our method says the well draws from (as grouped on these pages) is the one the state recorded in about 75% of them; when it names the Dockum (4,542 wells), the state's record agrees only about 33% of the time, and most of the others are recorded as Ogallala wells.

  • The layers come from the Texas Water Development Board's High Plains Aquifer System model, with half mile cells, read here on a grid of about 1.2 by 1.4 miles. It is a regional model, not a survey of any lot.
  • The state's model has half mile cells; we read it on a grid of about 1.2 by 1.4 miles, Texas part only. Layers from version 1.01 (2015); the 2025 extension (1.02) did not change them. It is not a survey of any lot, so we give ranges.
  • Figures go by four groups: Ogallala; Pecos Valley; Edwards-Trinity and Rita Blanca (Cretaceous rock under the Ogallala; the Rita Blanca alone matched the state 19%); Dockum (upper and lower together: the state's codes almost never say which). The Edwards-Trinity group joins three aquifers in different places (High Plains around Lubbock, Plateau around Midland and Odessa, Rita Blanca in Dallam and Hartley): county and place pages name the local one where they can.
  • Dockum: when our method names the Dockum, the state's record agrees only 33% of the time over all years (61% for wells with a screened interval, which is 93% of home wells of the last 10 years); most of the rest are recorded as Ogallala wells. The median well we put in the Dockum ends about 18 ft under the base of the Ogallala as the model draws it. So these pages say "at or just below the base of the Ogallala, in the top of the Dockum", never a certain formation. The state's own 2025 report on this model says depth alone overstates the upper Dockum.
  • "Near or below the base" means the well ends near or below the base of the Dockum, or of the Ogallala where there is no Dockum (Permian red beds; Gray, Carson, Donley, Moore and north Potter counties). Half of these wells end within about 51 ft of the base, and the state usually records them as Ogallala or Dockum wells. That is not an error: the model simply ends there.
  • For old wells without a screened interval (bottom of the hole) the method is only a little better than always saying Ogallala (65% against 58%); with an interval it is 89% against 80%. Figures over all years carry that weakness; last 10 years figures rest almost entirely on intervals.
  • 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/hale-county/edwards-trinity. License CC BY 4.0. https://doi.org/10.5281/zenodo.24126380.

Sources