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Water wells in the Lone Star Groundwater Conservation District

Home water wells inside the Lone Star Groundwater Conservation District (Montgomery County, Texas) are typically 187 to 265 feet deep (median 215 ft, 3,664 wells drilled in the last 10 years). Most draw from the Chicot Aquifer (61%), and 29% draw from the Evangeline Aquifer, according to the state's northern Gulf Coast Aquifer model (TWDB). The split between the Chicot and the Evangeline is approximate. Over the last three full years drillers reported about 333 new home wells a year; the peak was 649 in 2011. Estimated cost of a complete well at the median depth: $8,000 to $19,500.

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 Lone Star Groundwater Conservation DistrictDistrict boundary (Montgomery County) with the places that have the most home wells.Conroe: 245 ftConroeThe Woodlands: 225 ftThe WoodlandsRoman Forest: 195 ftWoodbranch: 195 ftPatton Village: 190 ftMagnolia: 225 ftMagnoliaPinehurst: 220 ftCleveland: 220 ftCleveland10 miles

Under the center of the Lone Star GCD

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

Home wells in and around the Lone Star 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)
187 to 265 feet
Median depth
215 feet
Deepest 10% are past
355 feet
Water level (median)
66 feet
3,532 wells
Yield (median)
40 gpm
3,436 wells, gallons per minute
Wells used
3,664
In the last 10 years
Counties
1
All years on file
10,672
median 220 ft, since 1997
Confidence
Standard (30 or more wells)

When the wells were finished, the water stood a median 66 feet below the surface (3,532 wells), well above the bottom: the typical well holds about 149 feet of water.

Map of the Lone Star Groundwater Conservation DistrictDistrict boundary (Montgomery County) with the places that have the most home wells.Conroe: 245 ftConroeThe Woodlands: 225 ftThe WoodlandsRoman Forest: 195 ftWoodbranch: 195 ftPatton Village: 190 ftMagnolia: 225 ftMagnoliaPinehurst: 220 ftCleveland: 220 ftCleveland10 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 333 new home wells a year; the peak was 649 in 2011.

Home wells reported per year in the Lone Star GCDFrom 2002 to 2026. The table below has every year.02004006008002002: 2662003: 5212004: 53820042005: 6042006: 5412007: 4712008: 39820082009: 3722010: 3992011: 6492012: 42120122013: 4362014: 4532015: 4112016: 41020162017: 3712018: 3362019: 3572020: 37620202021: 4412022: 4652023: 3772024: 29720242025: 3252026: 263
Domestic wells with a depth, by the year they were finished. 2026 is still in progress.
Show the data table
YearWells
2002266
2003521
2004538
2005604
2006541
2007471
2008398
2009372
2010399
2011649
2012421
2013436
2014453
2015411
2016410
2017371
2018336
2019357
2020376
2021441
2022465
2023377
2024297
2025325
2026263

Which formation the wells draw from

Most draw from the Chicot Aquifer (61%), and 29% draw from the Evangeline Aquifer, according to the state's northern Gulf Coast Aquifer model (TWDB). The line between the Chicot and the Evangeline is drawn differently by different studies, so read that split as approximate: of the wells the state records in the Evangeline, our method finds the Evangeline for only about 51% and the Chicot for most of the rest.

Layer (state's model)ShareWellsTypical depth (ft)
Chicot61%2,244180–234
Evangeline29%1,069205–353
Jasper, Catahoula and Burkeville10%351235–350

For 96% 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
Conroe245200–349591Evangeline Aquifer
The Woodlands225200–255411Chicot Aquifer
Roman Forest195180–205382Chicot Aquifer
Woodbranch195180–201294Chicot Aquifer
Patton Village190180–200261Chicot Aquifer
Magnolia225205–255257Chicot Aquifer
Pinehurst (Montgomery County)220200–250237Chicot Aquifer
Cleveland220180–250196Chicot Aquifer
Stagecoach212200–245138Chicot Aquifer
Willis290210–365135Evangeline Aquifer
Montgomery255220–335131Evangeline Aquifer
Woodloch200180–228123Chicot Aquifer

Counties

Depth over time

Home well depth in the district has not changed meaningfully in 20 years: the median was 230 feet in 2003 to 2007 and 210 feet in 2021 to 2025 (a difference under 10% or within the margin of error).

PeriodMedian depth (ft)Wells
2001–20052302,090
2006–20102252,181
2011–20152252,370
2016–20202201,850
2021–20252101,905
2026220263

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Common questions

How deep are wells in the Lone Star GCD?

Home water wells inside the Lone Star Groundwater Conservation District (Montgomery County, Texas) are typically 187 to 265 feet deep (median 215 ft, 3,664 wells drilled in the last 10 years).

Which formation do wells in the district draw from?

Most draw from the Chicot Aquifer (61%), and 29% draw from the Evangeline Aquifer, according to the state's northern Gulf Coast Aquifer model (TWDB). The line between the Chicot and the Evangeline is drawn differently by different studies, so read that split as approximate: of the wells the state records in the Evangeline, our method finds the Evangeline for only about 51% and the Chicot for most of the rest.

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 Lone Star Groundwater Conservation District before drilling inside it.

What a well costs here

At the median depth for the district (215 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 (187 to 265 feet) the range runs from $7,000 to $22,500. 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 96% 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 14,333 wells in the area of the state's northern Gulf Coast Aquifer model (Houston and Southeast Texas) 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 83% of them, and that formation or the one next to it in at least 99%; of the 3,578 of those wells that the state records in the Evangeline, it names the Evangeline for about 51% and the Chicot for most of the rest.

  • The layers come from the Texas Water Development Board's northern Gulf Coast Aquifer model, with cells of about 0.62 mile (1 km). It is a regional model, not a survey of any lot.
  • The state's model has cells of about 3,277 ft (1 km, 0.62 mile); we read it on a grid of about 0.6 by 0.7 miles. It is not a survey of any lot, so we give ranges.
  • Figures go by three groups: Chicot, Evangeline, and Jasper and Catahoula with the Burkeville. The state's records cannot tell the Burkeville, the Jasper and the Catahoula apart at a well (alone, the Burkeville matched 33% and the Catahoula 50%), so they are never named one by one as the formation of a well or a place.
  • The line between the Chicot and the Evangeline is drawn differently by different studies. The state's records put about half of their Evangeline wells in what the model draws as the Chicot, mostly deeper wells in Harris, Montgomery, Waller, Liberty and Austin counties. Where both appear, the split is approximate.
  • "Near or below the base" means the well ends near or below the base of the Gulf Coast Aquifer (under the Catahoula: Jackson Group, Yegua and older). It is 1.3% of home wells; half of them end within about 85 ft of the base. That is not an error: the model simply ends there.
  • The model's top layer is a uniform 49 ft slab for the water table zone, not a rock unit; we merge it into the unit beneath. The model also covers Colorado, Lavaca, Fayette, Wharton and Matagorda counties (outside Groundwater Management Area 14), with the same framework. Texas part only.
  • 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/lone-star-groundwater-conservation-district. License CC BY 4.0. https://doi.org/10.5281/zenodo.24126380.

Sources