Texas Gulf Coast Groundwater and Land Subsidence

Over Forty Years of Research in the Houston-Galveston Region

Well

In cooperation with Harris-Galveston Subsidence District, the City of Houston, Fort Bend County Subsidence District, Lone Star Groundwater Conservation District, and Brazoria County Groundwater Conservation District, the U.S. Geological Survey Texas Water Science Center Gulf Coast Program collects, processes, and interprets groundwater-level and aquifer-sediment-compaction data to understand the effects of groundwater withdrawal on land subsidence in the Houston-Galveston region of Texas.

Land Subsidence

Land subsidence is the gradual lowering of land-surface elevation. In the Houston-Galveston region, land subsidence is caused by compaction of fine-grained aquifer sediments (silts and clays) below the land surface due to groundwater withdrawals. Removing water from fine-grained aquifer sediments compresses the aquifer leaving less pore space available to store water resulting in the lowering (sinking or settling) of the land-surface. Most compaction that occurs as a result of groundwater withdrawals is irreversible; even if groundwater levels rise, compacted sediments and the associated land-surface lowering would remain as-is.

Consequences of land subsidence in the Houston-Galveston Region

Groundwater Withdrawals

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Groundwater
Withdrawals Begin
1836
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Groundwater Withdrawals Exceed 450 Million Gallons per Day
1975
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Extensive Groundwater Well-Monitoring Network Established
1977
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First Water-Level-Altitude Maps of Aquifers Released
1979
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Groundwater Withdrawal from Jasper Aquifer Increases
2000
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Groundwater Levels
Rise and Fall
2015

Aquifers

Gulf Coast aquifer system in the Houston-Galveston region, Texas
Gulf Coast aquifer system in the Houston-Galveston region, Texas. Click for larger image.

The primary aquifers in the Gulf Coast aquifer system in the Houston-Galveston region are the Chicot-Evangeline (undifferentiated) and Jasper, which are composed of laterally discontinuous deposits of gravel, sand, silt, and clay.

Groundwater withdrawn from the Chicot-Evangeline and Jasper aquifers has been the primary source of water for municipal supply, commercial and industrial use, and irrigation in the Houston-Galveston region since the early 1900s.

Prior to 1975, the withdrawal of groundwater from the Chicot-Evangeline aquifer was unregulated, and water levels in the aquifer were declining with associated depressuring, dewatering, and compaction resulting in subsidence.

By 1977, the withdrawals had resulted in water-level altitude declines of 350 feet below datum in the Chicot-Evangeline aquifer in southeastern Harris County, and correspondingly, by 1979, as much as 10 feet of subsidence had occurred in the Houston-Galveston region.

Regulatory Areas

Regulatory areas
Regulatory areas.

To address the issues associated with land-surface subsidence and compaction, the 64th Texas State Legislature authorized the establishment of the Harris-Galveston Subsidence District to regulate and reduce groundwater withdrawals in Harris and Galveston Counties. Subsequent to establishing the Harris-Galveston Subsidence District, the Texas State Legislature established the Fort Bend Subsidence District and two groundwater conservation districts: Lone Star Groundwater Conservation District and, most recently, Brazoria County Groundwater Conservation District in the Houston-Galveston region to provide for the regulation of groundwater withdrawals in areas within their jurisdiction.

Harris-Galveston Subsidence District

1975: Established by Texas State Legislature.

1976: First regulatory area (Area of Concentrated Emphasis, ACE) established.

1985: Divided into 8 regulatory areas by amount of groundwater reduction needed.

1992: Regulatory areas redivided into 7 areas.

1999: Regulatory areas converted into 3 primary areas.

2013: HGSD regulatory plan updated.

Fort Bend Subsidence District

1989: Established by the Texas State Legislature.

2003: Regulatory areas divided into area A, which includes the Richmond-Rosenberg subarea, and area B.

Lone Star Groundwater Conservation District

2001: Established by the Texas State Legislature.

Brazoria County Groundwater Conservation District

2005: Established by the Texas State Legislature.

Data Processing and Map Creation

Maps

Since 1977, the USGS Texas Water Science Gulf Coast Program has published regional groundwater maps for the Houston-Galveston Region, Texas. After collecting and evaluating groundwater-level data for quality control, data are incorporated into a geographic information system (GIS) and used for the construction of regional water-level altitude and regional water-level change maps.

Water-level altitude is calculated at each well by subtracting the water-level measurement (depth to water below land surface) from the referenced well land-surface altitude. The accuracy of the referenced well land-surface altitude data has improved through time and the most accurate land-surface altitude data available at the time of publication were used in the creation of each regional water-level altitude map. Up to 2020, regional water-level altitude maps were created by manually interpolating contours of water-level altitude data at observation wells in the Houston-Galveston Region. In 2021, kriging, a geostatistical interpolation method, was adopted as an effective alternative to manual contour interpolation.

Regional water-level change maps were constructed by interpreting the compiled water-level altitude data as the difference in water-level altitude at each well for the water-level data collection year and the historical year or as the difference in water-level altitude at each well for the water-level data collection year and the interpolated water-level altitude of the historic year from a modeled surface. Interpolated modeled water-level altitude surfaces were only used to compute differences when wells were destroyed or were not measured during the individual publication study period. Further information detailing the data processing and map creation for each published regional water-level altitude and regional water-level change contour map can be found in the individual year publication.

Explore Groundwater-Level and Compaction Data in the Chicot, Evangeline and Jasper Aquifers

Map viewer screenshot

USGS measures groundwater levels in over 700 wells in an 11-county area annually in the Houston-Galveston area in order to develop a regional depiction of groundwater levels. The cumulative compaction in the Chicot-Evangeline undifferentiated aquifer is measured at 13 extensometer stations in the 11-county area.

Water-level altitude, well, and compaction data have been combined in an interactive map that allows users to view annual water-level altitudes, water-level changes over time, and historical time series of compaction data.

Looking for the raw data?

Groundwater-level and compaction data are available as part of USGS data products.

Select USGS Publications

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Status of Water-Level Altitudes and Long-Term and Short-Term Water-Level Changes in the Chicot and Evangeline (Undifferentiated) and Jasper Aquifers, Greater Houston Area, Texas, 2022
By Jason K. Ramage and Christopher L. Braun
Scientific Investigations Report 2023-5007
Since the early 1900s, groundwater withdrawn from the primary aquifers that compose the Gulf Coast aquifer system—the Chicot, Evangeline, and Jasper aquifers—has been an important source of water in the greater Houston area, Texas. This report, prepared by...
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Hydrogeology, Land-Surface Subsidence and Documentation of the Gulf Coast Land Subsidence and Groundwater-Flow Model, Southeast Texas, 1897-2018
By John Ellis
Professional Paper 1877
As a part of the Texas Water Development Board groundwater availability modeling program, the U.S. Geological Survey developed the Gulf Coast Land Subsidence and Groundwater-Flow model
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MODFLOW 6 model and ensemble used in the simulation of groundwater flow and land-surface subsidence in the northern part of the Gulf Coast aquifer system, 1897-2018
By Jacob E. Knight, John H. Ellis, Jeremy T. White, Michelle Sneed, Joseph D. Hughes, Jason K. Ramage, Christopher L. Braun, Andrew P. Teeple, Linzy K. Foster, Samuel H. Rendon, Justin T. Brandt, Leslie L. Duncan, Jonathan P. Traylor, and Caitlin H. Pattison
Data Release
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Status of Water-Level Altitudes and Long-Term Water-Level Changes in the Chicot and Evangeline (Undifferentiated) and Jasper Aquifers, Greater Houston Area, Texas, 2021
By Christopher L. Braun and Jason K. Ramage
Scientific Investigations Report 2022-5065
Since the early 1900s, groundwater withdrawn from the primary aquifers that compose the Gulf Coast aquifer system - the Chicot and Evangeline (undifferentiated) and Jasper aquifers - has been the primary source of water in the greater Houston area, Texas. This report, prepared by...
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Treatment of the Chicot and Evangeline Aquifers as a Single Hydrogeologic Unit and Use of Geostatistical Interpolation Methods To Develop Gridded Surfaces of Water-Level Altitudes and Water-Level Changes in the Chicot and Evangeline Aquifers (Undifferentiated) and Jasper Aquifer, Greater Houston Area, Texas, 2021
By Jason K. Ramage, Christopher L. Braun, and John H. Ellis
Scientific Investigations Report 2022-5064
The greater Houston area of Texas includes approximately 11,000 square miles and encompasses all or part of 11 counties...
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Status of Groundwater-Level Altitudes and Long-Term Groundwater-Level Changes in the Chicot, Evangeline, and Jasper Aquifers, Houston-Galveston Region, Texas, 2020
By Christopher L. Braun and Jason K. Ramage
Scientific Investigations Report 2020-5089
In 2020, groundwater-level-altitude contours for the Chicot aquifer ranged from 150 feet (ft) below the North American Vertical Datum of 1988 (hereinafter referred to as "datum") to 200 ft above datum...
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Status of Groundwater-Level Altitudes and Long-Term Groundwater-Level Changes in the Chicot, Evangeline, and Jasper Aquifers, Houston-Galveston Region, Texas, 2019
By Christopher L. Braun, Jason K. Ramage, and Sachin D. Shah
Scientific Investigations Report 2019-5089
The 1977-2019 groundwater-level-change contours for the Chicot aquifer depict a large area of decline in groundwater-level altitudes (100 ft) in northwestern Harris County...
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Status of Groundwater-Level Altitudes and Long-Term Groundwater-Level Changes in the Chicot, Evangeline, and Jasper Aquifers, Houston-Galveston Region, Texas, 2018
By Sachin D. Shah, Jason K. Ramage, and Christopher L. Braun
Scientific Investigations Report 2018-5101
The 1977-2018 groundwater-level-change contours for the Chicot aquifer depict a large area of decline in groundwater-level altitudes (120 ft) in northwestern Harris County...
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Water-Level Altitudes 2017 and WaterLevel Changes in the Chicot, Evangeline, and Jasper Aquifers and Compaction 1973-2016 in the Chicot and Evangeline Aquifers, Houston-Galveston Region, Texas
By Mark C. Kasmarek and Jason K. Ramage
Scientific Investigations Report 2017-5080
In 2017, water-level-altitude contours for the Chicot aquifer ranged from 200 feet (ft) below the North American Vertical Datum of 1988 (hereinafter referred to as "datum")...
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Water-Level Altitudes 2016 and Water-Level Changes in the Chicot, Evangeline, and Jasper Aquifers and Compaction 1973-2015 in the Chicot and Evangeline Aquifers, Houston-Galveston Region, Texas
By Mark C. Kasmarek, Jason K. Ramage, and Michaela R. Johnson
Scientific Investigations Map 3365
In 2016, water-level-altitude contours for the Chicot aquifer ranged from 200 feet (ft) below the vertical datum (North American Vertical Datum of 1988; hereinafter, datum)...
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Water-Level Altitudes 2015 and Water-Level Changes in the Chicot, Evangeline, and Jasper Aquifers and Compaction 1973-2014 in the Chicot and Evangeline Aquifers, Houston-Galveston Region, Texas
By Mark C. Kasmarek, Jason K. Ramage, Natalie A. Houston, Michaela R. Johnson, and Tiffany S. Schmidt
Scientific Investigations Map 3337
In 2015, water-level-altitude contours for the Chicot aquifer ranged from 175 feet (ft) below the vertical datum (the National Geodetic Vertical Datum of 1929 or the North American Vertical Datum of 1988; hereinafter, datum)...
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Groundwater Withdrawals 1976, 1990, and 2000-10 and Land-Surface-Elevation Changes 2000-10 in Harris, Galveston, Fort Bend, Montgomery, and Brazoria Counties, Texas
By Mark C. Kasmarek and Michaela R. Johnson
Scientific Investigations Report 2013-5034
The study area comprising Harris County and parts of Galveston, Fort Bend, Montgomery, and Brazoria Counties in southeastern Texas forms part of one of the largest areas of land-surface-elevation change in the United States...
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Investigation of Land Subsidence in the Houston-Galveston Region of Texas by Using the Global Positioning System and Interferometric Synthetic Aperture Radar, 1993-2000
By Gerald W. Bawden, Michaela R. Johnson, Mark C. Kasmarek, Justin Brandt, and Clifton S. Middleton
Scientific Investigations Report 2012-5211
Since the early 1900s, groundwater has been the primary source of municipal, industrial, and agricultural water supplies for the Houston-Galveston region, Texas...
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Estimated Land-Surface Subsidence in Harris County, Texas, 1915-17 to 2001
By Mark C. Kasmarek, Robert K. Gabrysch, and Michaela R. Johnson
Scientific Investigations Map 3097
Land-surface subsidence, or land subsidence, in Harris County, Texas, which encompasses much of the Houston area, has been occurring for decades. Land subsidence has increased the frequency and extent of flooding, damaged buildings and transportation infrastructure, and caused adverse environmental effects...
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Principal Faults in the Houston, Texas, Metropolitan Area
By Sachin D. Shah and Jennifer Lanning-Rush
Scientific Investigations Map 2874
This report, prepared by the U.S. Geological Survey in cooperation with the Harris-Galveston Coastal Subsidence District, documents and refines the locations of principal faults mapped in the Houston, Texas, metropolitan area in previous studies. Numerous subsurface faults have been documented beneath the Houston metropolitan area at depths of 3,200 to 13,000 feet...
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Evaluation of Ground-Water Flow and Land-Surface Subsidence Caused by Hypothetical Withdrawals in the Northern Part of the Gulf Coast Aquifer System, Texas
By Mark C. Kasmarek, Brian D. Reece, and Natalie A. Houston
Scientific Investigations Report 2005-5024
During 2003-04 the U.S. Geological Survey, in cooperation with the Texas Water Development Board (TWDB) and the Harris-Galveston Coastal Subsidence District (HGCSD)...
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Hydrogeology and Simulation of Ground-Water Flow and Land-Surface Subsidence in the Northern Part of the Gulf Coast Aquifer System, Texas
By Mark C. Kasmarek and James L. Robinson
Scientific Investigations Report 2004-5102
As a part of the Texas Water Development Board Ground-Water Availability Modeling program, the U.S. Geological Survey developed and tested a numerical finite-difference (MODFLOW) model to simulate ground-water flow and land-surface subsidence in the northern part of the Gulf Coast aquifer system...
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Land Subsidence in the United States
By Devin Galloway, David R. Jones, and S.E. Ingebritsen
Circular 1182
Land subsidence is a gradual settling or sudden sinking of the Earth's surface owing to subsurface movement of earth materials.Subsidence is a global problem and, in the United States, more than 17,000 square miles in 45 States, an area roughly the size of New Hampshire and Vermont combined, have...
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Ground-Water Withdrawals and Land-Surface Subsidence in the Houston-Galveston Region, Texas, 1906-80
By R.K. Gabrysch
Open-File Report 82-871
The withdrawal of large amounts of ground water in the Houston-Galveston region, Texas, has resulted in water-level declines of as much as 250 feet (76 meters) in wells completed in the Chicot aquifer and as much as 300 feet (91 meters) in wells completed in the Evangeline aquifer during 1943-77...
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Approximate Water-Level Changes in Wells in the Chicot and Evangeline Aquifers, 1977-81 and 1980-81, and Measured Compaction, 1973-81, in the Houston-Galveston Region, Texas
By R.K. Gabrysch and C.E. Ranzau, Jr.
Open-File Report 81-341
This report consists of: (1) Four maps that present data on water-level changes during 1977-81 and 1980-81 in the Chicot and Evangeline aquifers and (2) one set of graphs that present data on the compaction of subsurface materials for 1973-81...

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Contact Us

Christopher Braun
Groundwater Specialist
USGS Southeast Region
936-271-5300
clbraun@usgs.gov
Jason Ramage
Hydrologist
USGS Southeast Region
936-271-5341
jkramage@usgs.gov