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Water wells in the Barton Springs/Edwards Aquifer Conservation District

Home water wells inside the Barton Springs/Edwards Aquifer Conservation District (Hays, Travis and Caldwell counties, Texas) are typically 373 to 765 feet deep (median 450 ft, 224 wells drilled in the last 10 years). The state's model covers only 9% of these wells (20); among those, 90% draw from the Middle Trinity, according to the state's Hill Country Trinity model (TWDB). Drillers reported 18 new home wells in 2025, less than half the peak of 63 in 2004. Estimated cost of a complete well at the median depth: $14,000 to $33,500.

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

Map of the Barton Springs/Edwards Aquifer Conservation DistrictDistrict boundary (Hays, Travis and Caldwell counties) with the places that have the most home wells.Austin: 570 ftAustinManchaca: 400 ftManchacaKyle: 400 ftKyleShady Hollow: 400 ftShady HollowRollingwood: 440 ftBuda: 400 ftBudaHays: 400 ftSan Leanna: 400 ft10 miles

Under the center of the Barton Springs/Edwards Aquifer CD

District boundary from TWDB's file current as of November 2019. Later changes are not shown.

Home wells in and around the Barton Springs/Edwards Aquifer CD

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: the district boundary (TWDB, 2019)

Key figures

Typical depth (middle half)
373 to 765 feet
Median depth
450 feet
Deepest 10% are past
960 feet
Water level (median)
228 feet
209 wells
Yield (median)
20 gpm
160 wells, gallons per minute
Wells used
224
In the last 10 years
Counties
3
All years on file
762
median 450 ft, since 1996
Confidence
Standard (30 or more wells)

When the wells were finished, the water stood a median 228 feet below the surface (209 wells).

Map of the Barton Springs/Edwards Aquifer Conservation DistrictDistrict boundary (Hays, Travis and Caldwell counties) with the places that have the most home wells.Austin: 570 ftAustinManchaca: 400 ftManchacaKyle: 400 ftKyleShady Hollow: 400 ftShady HollowRollingwood: 440 ftBuda: 400 ftBudaHays: 400 ftSan Leanna: 400 ft10 miles
District boundary from TWDB's file current as of November 2019. Later changes are not shown.

New home wells per year

Drillers reported 18 new home wells in 2025, less than half the peak of 63 in 2004.

Home wells reported per year in the Barton Springs/Edwards Aquifer CDFrom 2002 to 2026. The table below has every year.0204060802002: 302003: 422004: 6320042005: 502006: 482007: 442008: 3120082009: 322010: 202011: 262012: 2020122013: 262014: 532015: 332016: 2120162017: 232018: 352019: 272020: 1520202021: 192022: 272023: 242024: 2020242025: 182026: 11
Domestic wells with a depth, by the year they were finished. 2026 is still in progress.
Show the data table
YearWells
200230
200342
200463
200550
200648
200744
200831
200932
201020
201126
201220
201326
201453
201533
201621
201723
201835
201927
202015
202119
202227
202324
202420
202518
202611

Which formation the wells draw from

The state's model covers only 9% of these wells (20); among those, 90% draw from the Middle Trinity, according to the state's Hill Country Trinity model (TWDB).

Layer (state's model)ShareWellsTypical depth (ft)
Middle Trinity90%18685–848
Upper Trinity5%1—
Lower Trinity5%1—

For 90% of these wells the report says where the water enters (the screen or the open hole), and we use the middle of that interval.

Places with the most wells in the district

PlaceMedian depth (ft)Middle half (ft)WellsMain layer
Austin570430–800337Lower Trinity
Manchaca400400–41373—
Kyle400350–58061—
Shady Hollow400352–40550—
Rollingwood440360–63045At or just below the base of the Woodbine (Washita and Fredericksburg)
Buda400400–40434—
Hays400400–41030—
San Leanna400383–42023—
Mountain City400370–40516—

Counties

Depth over time

Home well depth in the district has not changed meaningfully in 20 years: the median was 510 feet in 2003 to 2007 and 445 feet in 2021 to 2025 (a difference under 10% or within the margin of error).

PeriodMedian depth (ft)Wells
2001–2005505187
2006–2010485175
2011–2015400158
2016–2020500121
2021–2025445108
202643011

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Common questions

How deep are wells in the Barton Springs/Edwards Aquifer CD?

Home water wells inside the Barton Springs/Edwards Aquifer Conservation District (Hays, Travis and Caldwell counties, Texas) are typically 373 to 765 feet deep (median 450 ft, 224 wells drilled in the last 10 years).

Which formation do wells in the district draw from?

The state's model covers only 9% of these wells (20); among those, 90% draw from the Middle Trinity, according to the state's Hill Country Trinity model (TWDB).

What does a groundwater conservation district do?

In Texas, districts are the local authority over groundwater: they can require registration or permits for new wells, set spacing from other wells and property lines, and limit pumping. Each district writes its own rules, so ask the Barton Springs/Edwards Aquifer Conservation District before drilling inside it.

What a well costs here

At the median depth for the district (450 feet), a complete home well would cost roughly $14,000 to $33,500: $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 (373 to 765 feet) the range runs from $12,000 to $52,500. 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 whose coordinates fall inside the district boundary. 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 90% 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 2,665 wells in the Texas Hill Country 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 76% of them, and that layer or the one next to it in at least 98%.

  • The layers come from the Texas Water Development Board's Hill Country Trinity model, with 1 mile cells. 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.
  • "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/districts/barton-springs-edwards-aquifer-conservation-district. License CC BY 4.0. https://doi.org/10.5281/zenodo.24126380.

Sources