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Water wells in the Fort Bend Subsidence District

Home water wells inside the Fort Bend Subsidence District (Fort Bend County, Texas) are typically 205 to 320 feet deep (median 260 ft, 2,017 wells drilled in the last 10 years). All the wells the model covers draw from the Chicot Aquifer, according to the state's northern Gulf Coast Aquifer model (TWDB). Over the last three full years drillers reported about 189 new home wells a year; the peak was 366 in 2006. Estimated cost of a complete well at the median depth: $9,000 to $22,000.

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 Fort Bend Subsidence DistrictDistrict boundary (Fort Bend County) with the places that have the most home wells.Fresno: 177 ftFresnoRosenberg: 250 ftRosenbergArcola: 183 ftArcolaMissouri City: 323 ftSienna: 320 ftNeedville: 285 ftNeedvilleFairchilds: 285 ftFairchildsPleak: 240 ftPleak10 miles

Under the center of the Fort Bend Subsidence District

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

Home wells in and around the Fort Bend Subsidence District

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)
205 to 320 feet
Median depth
260 feet
Deepest 10% are past
365 feet
Water level (median)
60 feet
1,934 wells
Yield (median)
60 gpm
1,290 wells, gallons per minute
Wells used
2,017
In the last 10 years
Counties
1
All years on file
5,751
median 260 ft, since 2000
Confidence
Standard (30 or more wells)

When the wells were finished, the water stood a median 60 feet below the surface (1,934 wells), well above the bottom: the typical well holds about 200 feet of water.

Map of the Fort Bend Subsidence DistrictDistrict boundary (Fort Bend County) with the places that have the most home wells.Fresno: 177 ftFresnoRosenberg: 250 ftRosenbergArcola: 183 ftArcolaMissouri City: 323 ftSienna: 320 ftNeedville: 285 ftNeedvilleFairchilds: 285 ftFairchildsPleak: 240 ftPleak10 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 189 new home wells a year; the peak was 366 in 2006.

Home wells reported per year in the Fort Bend Subsidence DistrictFrom 2002 to 2026. The table below has every year.01002003004002002: 472003: 3242004: 35420042005: 3622006: 3662007: 2452008: 26220082009: 1922010: 1892011: 2332012: 20920122013: 2082014: 2592015: 2562016: 24020162017: 1612018: 1712019: 2112020: 25720202021: 2672022: 2172023: 2002024: 17920242025: 1882026: 132
Domestic wells with a depth, by the year they were finished. 2026 is still in progress.
Show the data table
YearWells
200247
2003324
2004354
2005362
2006366
2007245
2008262
2009192
2010189
2011233
2012209
2013208
2014259
2015256
2016240
2017161
2018171
2019211
2020257
2021267
2022217
2023200
2024179
2025188
2026132

Which formation the wells draw from

All the wells the model covers draw from the Chicot Aquifer, according to the state's northern Gulf Coast Aquifer model (TWDB).

Layer (state's model)ShareWellsTypical depth (ft)
Chicot100%2,017205–320

For 92% 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
Fresno177121–350392Chicot Aquifer
Rosenberg250220–300370Chicot Aquifer
Arcola183120–363369Chicot Aquifer
Missouri City323165–400285Chicot Aquifer
Sienna320100–380281Chicot Aquifer
Needville285240–345279Chicot Aquifer
Fairchilds285230–350275Chicot Aquifer
Pleak240220–300154Chicot Aquifer
Richmond312270–340129Chicot Aquifer
Beasley268225–270103Chicot Aquifer
Fulshear250217–32094Chicot Aquifer
Cinco Ranch280254–31890Chicot Aquifer

Counties

Depth over time

Home well depth in the district has not changed meaningfully in 20 years: the median was 260 feet in 2003 to 2007 and 245 feet in 2021 to 2025 (a difference under 10% or within the margin of error).

PeriodMedian depth (ft)Wells
2001–20052521,108
2006–20102661,254
2011–20152531,165
2016–20202801,040
2021–20252451,051
2026245132

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Common questions

How deep are wells in the Fort Bend Subsidence District?

Home water wells inside the Fort Bend Subsidence District (Fort Bend County, Texas) are typically 205 to 320 feet deep (median 260 ft, 2,017 wells drilled in the last 10 years).

Which formation do wells in the district draw from?

All the wells the model covers draw from the Chicot Aquifer, according to the state's northern Gulf Coast Aquifer 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 Fort Bend Subsidence District before drilling inside it.

What a well costs here

At the median depth for the district (260 feet), a complete home well would cost roughly $9,000 to $22,000: $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 (205 to 320 feet) the range runs from $7,500 to $25,500. 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 92% 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/fort-bend-subsidence-district. License CC BY 4.0. https://doi.org/10.5281/zenodo.24126380.

Sources