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Water wells in the Central Texas Groundwater Conservation District

Home water wells inside the Central Texas Groundwater Conservation District (Burnet County, Texas) are typically 260 to 460 feet deep (median 350 ft, 2,618 wells drilled in the last 10 years). Most draw from the lower Trinity (Twin Mountains and Travis Peak, 71%), and 28% end near or below the base of the Trinity, according to the state's Northern Trinity and Woodbine model (TWDB). Drillers reported 206 new home wells in 2025, less than half the peak of 422 in 2021. Estimated cost of a complete well at the median depth: $11,500 to $27,500.

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 Central Texas Groundwater Conservation DistrictDistrict boundary (Burnet County) with the places that have the most home wells.Burnet: 305 ftBurnetKingsland: 120 ftKingslandBuchanan Dam: 144 ftBuchanan DamBertram: 420 ftBertramMarble Falls: 245 ftMarble FallsGranite Shoals: 100 ftHorseshoe Bay: 171 ftBriggs: 550 ftBriggs10 miles

Under the center of the Central Texas GCD

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

Home wells in and around the Central Texas 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.

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 460 feet
Median depth
350 feet
Deepest 10% are past
560 feet
Water level (median)
216 feet
1,210 wells
Yield (median)
30 gpm
2,029 wells, gallons per minute
Wells used
2,618
In the last 10 years
Counties
1
All years on file
5,579
median 310 ft, since 1979
Confidence
Standard (30 or more wells)

When the wells were finished, the water stood a median 216 feet below the surface (1,210 wells).

Map of the Central Texas Groundwater Conservation DistrictDistrict boundary (Burnet County) with the places that have the most home wells.Burnet: 305 ftBurnetKingsland: 120 ftKingslandBuchanan Dam: 144 ftBuchanan DamBertram: 420 ftBertramMarble Falls: 245 ftMarble FallsGranite Shoals: 100 ftHorseshoe Bay: 171 ftBriggs: 550 ftBriggs10 miles
District boundary from TWDB's file current as of November 2019. Later changes are not shown.

New home wells per year

Drillers reported 206 new home wells in 2025, less than half the peak of 422 in 2021.

Home wells reported per year in the Central Texas GCDFrom 2002 to 2026. The table below has every year.02004006002002: 1142003: 2572004: 21420042005: 2822006: 2962007: 2122008: 24920082009: 2532010: 1272011: 1522012: 17720122013: 1342014: 1642015: 1562016: 14920162017: 1882018: 2052019: 2552020: 30920202021: 4222022: 4192023: 2322024: 22920242025: 2062026: 132
Domestic wells with a depth, by the year they were finished. 2026 is still in progress.
Show the data table
YearWells
2002114
2003257
2004214
2005282
2006296
2007212
2008249
2009253
2010127
2011152
2012177
2013134
2014164
2015156
2016149
2017188
2018205
2019255
2020309
2021422
2022419
2023232
2024229
2025206
2026132

Which formation the wells draw from

Most draw from the lower Trinity (Twin Mountains and Travis Peak, 71%), and 28% end near or below the base of the Trinity, according to the state's Northern Trinity and Woodbine model (TWDB).

Layer (state's model)ShareWellsTypical depth (ft)
Lower TrinityTwin Mountains and Travis Peak71%1,329305–500
Near or below the base of the Trinity28%516340–491
Upper TrinityPaluxy and Glen Rose1%19365–540

For 95% 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
Burnet305220–380302Near or below the base of the Trinity
Kingsland12066–180298—
Buchanan Dam144100–200187—
Bertram420364–461116Lower Trinity (Twin Mountains and Travis Peak)
Marble Falls245140–34593—
Granite Shoals10074–14086—
Horseshoe Bay171100–20574—
Briggs550510–57467Lower Trinity (Twin Mountains and Travis Peak)
Buchanan Lake Village155100–25854—
Tow145100–18944—
Highland Haven8071–12041—
Meadowlakes18072–28538—

Counties

Depth over time

New home wells in the district are deeper than 20 years ago: the median went from 260 feet (2003 to 2007) to 350 feet (2021 to 2025), 35% more. Deeper wells do not always mean the water dropped: a driller may be going for another layer, better water or more reserve.

PeriodMedian depth (ft)Wells
2001–2005260910
2006–20102601,137
2011–2015297783
2016–20203401,106
2021–20253501,508
2026360132

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Common questions

How deep are wells in the Central Texas GCD?

Home water wells inside the Central Texas Groundwater Conservation District (Burnet County, Texas) are typically 260 to 460 feet deep (median 350 ft, 2,618 wells drilled in the last 10 years).

Which formation do wells in the district draw from?

Most draw from the lower Trinity (Twin Mountains and Travis Peak, 71%), and 28% end near or below the base of the Trinity, according to the state's Northern Trinity and Woodbine 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 Central Texas Groundwater Conservation District before drilling inside it.

What a well costs here

At the median depth for the district (350 feet), a complete home well would cost roughly $11,500 to $27,500: $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 460 feet) the range runs from $9,000 to $34,000. 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 95% 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/districts/central-texas-groundwater-conservation-district. License CC BY 4.0. https://doi.org/10.5281/zenodo.24126380.

Sources