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Depth to Groundwater Measured from Wells Completed in the Chicot and Evangeline (Undifferentiated) and Jasper Aquifers, Greater Houston Area, Texas, 2021

Dates

Publication Date
Start Date
2020-11-23
End Date
2021-03-11

Citation

Ramage, J.K., 2022, Depth to Groundwater Measured from Wells Completed in the Chicot and Evangeline (Undifferentiated) and Jasper Aquifers, Greater Houston Area, Texas, 2021: U.S. Geological Survey data release, https://doi.org/10.5066/P9R6CX2T.

Summary

This dataset documents the depth to groundwater measured in wells screened in the Chicot aquifer, Evangeline aquifer, Jasper aquifer, Burkeville confining unit, Catahoula confining system, or a combination of multiple hydrogeologic units in the greater Houston area, Texas for 2021. The U.S. Geological Survey prepared this dataset in cooperation with the Harris‐Galveston Subsidence District, City of Houston, Fort Bend Subsidence District, Lone Star Groundwater Conservation District, and Brazoria County Groundwater Conservation District. This dataset was created to provide resource managers, public officials, researchers, and the general public with ready access to information regarding depths to groundwater in the region. All of the [...]

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Attached Files

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Depth_to_Groundwater_Field_Measurements_2021.txt 112.97 KB text/plain

Purpose

This 2021 dataset is part of an annual assessment of the depth to groundwater in Harris, Galveston, Fort Bend, Montgomery, Brazoria, Chambers, Grimes, Liberty, San Jacinto, Walker, and Waller Counties, Texas. Most of the land-surface subsidence in the greater Houston area, Texas, occurs as a direct result of groundwater withdrawals for municipal supply, commercial and industrial use, and irrigation that depressures and dewaters the Chicot, Evangeline, and Jasper aquifers in different parts of the Houston-Galveston region, thereby causing compaction of the aquifer sediments (Gabrysch, 1979).

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9R6CX2T

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