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Water wells in the Edwards Aquifer Authority

Home water wells inside the Edwards Aquifer Authority (Uvalde, Medina, Bexar, Guadalupe and 3 more counties, Texas) vary a lot in depth: the middle half are 260 to 670 feet deep (median 450 ft, 2,802 wells drilled in the last 10 years), so look at the wells closest to the tract. The state's model covers only 21% of these wells (599); among those, 84% draw from the Middle Trinity, according to the state's Hill Country Trinity model (TWDB). Over the last three full years drillers reported about 310 new home wells a year; the peak was 401 in 2005. 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 Edwards Aquifer AuthorityDistrict boundary (Uvalde, Medina, Bexar, Guadalupe and 3 more counties) with the places that have the most home wells.San Antonio: 521 ftSan AntonioTimberwood Park: 563 ftTimberwood ParkNew Braunfels: 250 ftCross Mountain: 698 ftSt. Hedwig: 240 ftMcQueeney: 47 ftMcQueeneyGeronimo: 50 ftLuling: 260 ft50 miles

Under the center of the Edwards Aquifer Authority

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

Home wells in and around the Edwards Aquifer Authority

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)
260 to 670 feet
Median depth
450 feet
Deepest 10% are past
900 feet
Water level (median)
210 feet
2,464 wells
Yield (median)
21 gpm
2,250 wells, gallons per minute
Wells used
2,802
In the last 10 years
Counties
7
All years on file
7,588
median 460 ft, since 1993
Confidence
Standard (30 or more wells)

When the wells were finished, the water stood a median 210 feet below the surface (2,464 wells).

Map of the Edwards Aquifer AuthorityDistrict boundary (Uvalde, Medina, Bexar, Guadalupe and 3 more counties) with the places that have the most home wells.San Antonio: 521 ftSan AntonioTimberwood Park: 563 ftTimberwood ParkNew Braunfels: 250 ftCross Mountain: 698 ftSt. Hedwig: 240 ftMcQueeney: 47 ftMcQueeneyGeronimo: 50 ftLuling: 260 ft50 miles
District boundary from TWDB's file current as of November 2019. Later changes are not shown.

New home wells per year

Over the last three full years drillers reported about 310 new home wells a year; the peak was 401 in 2005.

Home wells reported per year in the Edwards Aquifer AuthorityFrom 2002 to 2026. The table below has every year.02004006002002: 1592003: 3862004: 39120042005: 4012006: 3892007: 3882008: 31720082009: 3052010: 2012011: 2322012: 27120122013: 2912014: 3912015: 2992016: 26320162017: 2182018: 2452019: 2412020: 27620202021: 3072022: 3572023: 3342024: 29720242025: 3002026: 198
Domestic wells with a depth, by the year they were finished. 2026 is still in progress.
Show the data table
YearWells
2002159
2003386
2004391
2005401
2006389
2007388
2008317
2009305
2010201
2011232
2012271
2013291
2014391
2015299
2016263
2017218
2018245
2019241
2020276
2021307
2022357
2023334
2024297
2025300
2026198

Which formation the wells draw from

The state's model covers only 21% of these wells (599); among those, 84% draw from the Middle Trinity, according to the state's Hill Country Trinity model (TWDB).

Layer (state's model)ShareWellsTypical depth (ft)
Middle Trinity84%502600–850
Lower Trinity10%57740–910
Upper Trinity7%40308–530

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.

Places with the most wells in the district

PlaceMedian depth (ft)Middle half (ft)WellsMain layer
San Antonio521392–800454Middle Trinity
Timberwood Park563475–780191Middle Trinity
New Braunfels25053–360138—
Cross Mountain698566–800114Middle Trinity
St. Hedwig240193–293105—
McQueeney4743–5289—
Geronimo5046–5675—
Luling260210–34068—
Grey Forest780700–84065Middle Trinity
Elmendorf360312–38059—
Zuehl5046–10059—
Olmos Park445274–50548—

Counties

Depth over time

Home well depth in the district has not changed meaningfully in 20 years: the median was 470 feet in 2003 to 2007 and 450 feet in 2021 to 2025 (a difference under 10% or within the margin of error).

PeriodMedian depth (ft)Wells
2001–20054801,453
2006–20104601,600
2011–20154201,484
2016–20204501,243
2021–20254501,595
2026450198

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Common questions

How deep are wells in the Edwards Aquifer Authority?

Home water wells inside the Edwards Aquifer Authority (Uvalde, Medina, Bexar, Guadalupe and 3 more counties, Texas) vary a lot in depth: the middle half are 260 to 670 feet deep (median 450 ft, 2,802 wells drilled in the last 10 years), so look at the wells closest to the tract.

Which formation do wells in the district draw from?

The state's model covers only 21% of these wells (599); among those, 84% 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 Edwards Aquifer Authority 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 (260 to 670 feet) the range runs from $9,000 to $46,500. 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 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 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/edwards-aquifer-authority. License CC BY 4.0. https://doi.org/10.5281/zenodo.24126380.

Sources