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Geospatial Dataset for the Geologic Framework and Hydrostratigraphy of the Edwards and Trinity Aquifers Within Northern Medina County, Texas at 1:24,000

Dates

Publication Date
Time Period
2024

Citation

Lamberts, A.P., Clark, A.K., and Morris, R.R., 2024, Geospatial dataset for the geologic framework and hydrostratigraphy of the Edwards and Trinity aquifers within northern Medina County, Texas at 1:24,000: U.S. Geological Survey data release, https://doi.org/10.5066/P9G6G8GT.

Summary

The karstic Edwards and Trinity aquifers are classified as major sources of water in south-central Texas by the Texas Water Development Board, and both are classified as major aquifers by the State of Texas. The Edwards and Trinity aquifers developed because of the original depositional history of the carbonate limestone and dolomite rocks that contain them, and the primary and secondary porosity, diagenesis, fracturing, and faulting that modified the porosity, permeability, and transmissivity of each aquifer and of the geologic units separating the aquifers. Previous studies such as those by the U.S. Geological Survey (USGS) and the Edwards Aquifer Authority (EAA) have mapped the geology, hydrostratigraphy, and structure in these [...]

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Attached Files

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Medina_GIS.zip
“GIS Data”
18.87 MB application/zip

Purpose

These digital data represent the geographical extent of the surficial hydrostratigraphic units and faulting in northern Medina county in south-central Texas. With a rapidly increasing population placing an increasing demand on water resources, the updated mapped hydrostratigraphic units are intended to aid in identifying units that likely facilitate groundwater recharge or discharge or function as a confining layer. These digital data accompany Clark and others (2024).

Rights

This work is marked with Creative Commons Zero v1.0 Universal (https://creativecommons.org/publicdomain/zero/1.0/).

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9G6G8GT

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