Water wells in the Southwestern Travis County Groundwater Conservation District
Home water wells inside the Southwestern Travis County Groundwater Conservation District (Travis County, Texas) vary a lot in depth: the middle half are 260 to 666 feet deep (median 410 ft, 572 wells drilled in the last 10 years), so look at the wells closest to the tract. Most draw from the Lower Trinity (76%), and 16% draw from the Middle Trinity, according to the state's Hill Country Trinity model (TWDB). Drillers reported 28 new home wells in 2025, less than half the peak of 140 in 2006. Estimated cost of a complete well at the median depth: $13,000 to $31,000.
Updated every day from Texas Water Development Board driller reports. Last update: November 11, 2026, using the state file of November 10, 2026.
Under the center of the Southwestern Travis County GCD
District boundary from TWDB's file current as of November 2019. Later changes are not shown.
Digging in…
Home wells in and around the Southwestern Travis County GCD
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.
Well depth (ft)
- <100
- 100
- 200
- 300
- 400
- 600
- 800+
Dark line: the district boundary (TWDB, 2019)
Green: aquifer mapped by the state
Key figures
- Typical depth (middle half)
- 260 to 666 feet
- Median depth
- 410 feet
- Deepest 10% are past
- 850 feet
- Water level (median)
- 310 feet
- 314 wells
- Yield (median)
- 25 gpm
- 524 wells, gallons per minute
- Wells used
- 572
- In the last 10 years
- Counties
- 1
- All years on file
- 1,907
- median 390 ft, since 1992
- Confidence
- Standard (30 or more wells)
When the wells were finished, the water stood a median 310 feet below the surface (314 wells), close to the bottom: the typical well holds only about 100 feet of water.
New home wells per year
Drillers reported 28 new home wells in 2025, less than half the peak of 140 in 2006.
Show the data table
| Year | Wells |
|---|---|
| 2002 | 76 |
| 2003 | 105 |
| 2004 | 109 |
| 2005 | 111 |
| 2006 | 140 |
| 2007 | 84 |
| 2008 | 86 |
| 2009 | 75 |
| 2010 | 61 |
| 2011 | 103 |
| 2012 | 64 |
| 2013 | 84 |
| 2014 | 86 |
| 2015 | 76 |
| 2016 | 74 |
| 2017 | 75 |
| 2018 | 93 |
| 2019 | 72 |
| 2020 | 79 |
| 2021 | 48 |
| 2022 | 56 |
| 2023 | 60 |
| 2024 | 34 |
| 2025 | 28 |
| 2026 | 22 |
Which formation the wells draw from
Most draw from the Lower Trinity (76%), and 16% draw from the Middle Trinity, according to the state's Hill Country Trinity model (TWDB). Read that as the most likely layer, not a certain one: where our method names the Lower Trinity, the state's own aquifer code agrees in about 53% of wells.
| Layer (state's model) | Share | Wells | Typical depth (ft) |
|---|---|---|---|
| Lower Trinity | 76% | 417 | 265–730 |
| Middle Trinity | 16% | 86 | 265–590 |
| Near or below the base of the Trinity | 6% | 32 | 535–888 |
| Lower TrinityTwin Mountains and Travis Peak | 1% | 6 | 226–334 |
| Upper TrinityPaluxy and Glen Rose | 1% | 4 | — |
| Washita and Fredericksburg | <1% | 1 | — |
For 97% 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
| Place | Median depth (ft) | Middle half (ft) | Wells | Main layer |
|---|---|---|---|---|
| Lakeway | 430 | 350–528 | 248 | Lower Trinity |
| Briarcliff | 280 | 240–385 | 189 | Lower Trinity |
| Lago Vista | 400 | 260–450 | 158 | Lower Trinity (Twin Mountains and Travis Peak) |
| Hudson Bend | 470 | 425–530 | 135 | Lower Trinity (Twin Mountains and Travis Peak) |
| West Lake Hills | 545 | 375–689 | 94 | Lower Trinity |
| Bee Cave | 845 | 660–892 | 79 | Lower Trinity |
| The Hills | 790 | 582–875 | 79 | Lower Trinity |
| Lost Creek | 715 | 602–825 | 42 | Lower Trinity |
| Barton Creek | 818 | 746–888 | 34 | Lower Trinity |
Counties
Depth over time
Home well depth in the district has not changed meaningfully in 20 years: the median was 375 feet in 2003 to 2007 and 432 feet in 2021 to 2025 (a difference under 10% or within the margin of error).
| Period | Median depth (ft) | Wells |
|---|---|---|
| 2001–2005 | 360 | 404 |
| 2006–2010 | 380 | 446 |
| 2011–2015 | 400 | 413 |
| 2016–2020 | 390 | 393 |
| 2021–2025 | 432 | 226 |
| 2026 | 519 | 22 |
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Common questions
How deep are wells in the Southwestern Travis County GCD?
Home water wells inside the Southwestern Travis County Groundwater Conservation District (Travis County, Texas) vary a lot in depth: the middle half are 260 to 666 feet deep (median 410 ft, 572 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?
Most draw from the Lower Trinity (76%), and 16% draw from the Middle Trinity, according to the state's Hill Country Trinity model (TWDB). Read that as the most likely layer, not a certain one: where our method names the Lower Trinity, the state's own aquifer code agrees in about 53% of wells.
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 Southwestern Travis County Groundwater Conservation District before drilling inside it.
What a well costs here
At the median depth for the district (410 feet), a complete home well would cost roughly $13,000 to $31,000: $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 666 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 97% 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/southwestern-travis-county-groundwater-conservation-district. 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)
- Groundwater Availability Model for the Hill Country portion of the Trinity Aquifer System, Texas. Jones, I.C., Anaya, R., and Wade, S.C., Texas Water Development Board, 2009, GAM v2.01 (MODFLOW-96). TWDB groundwater availability model.
- Groundwater conservation district boundaries, TWDB (current as of November 2019)
- Ground elevation: Terrain Tiles (Mapzen), Registry of Open Data on AWS
- TWDB well report viewer (each well's official report)