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USGS · fs20173090

Characterizing the subsurface geology in and around the U.S. Army Camp Stanley Storage Activity, south-central Texas

Abstract

Several U.S. Geological Survey projects, supported by the National Cooperative Geologic Mapping Program, have used multi-disciplinary approaches over a 14-year period to reveal the surface and subsurface geologic frameworks of the Edwards and Trinity aquifers of central Texas and the Arbuckle-Simpson aquifer of south-central Oklahoma. Some of the project achievements include advancements in hydrostratigraphic mapping, three-dimensional subsurface framework modeling, and airborne geophysical surveys as well as new methodologies that link geologic and groundwater flow models. One area where some of these milestones were achieved was in and around the U.S. Army Camp Stanley Storage Activity, located in north­western Bexar County, Texas, about 19 miles north­west of downtown San Antonio.

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 29.675° to 29.7417° latitude; -98.7° to -98.5917° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

Charles D. Blome, Allan K. Clark. 2018-02-15. Characterizing the subsurface geology in and around the U.S. Army Camp Stanley Storage Activity, south-central Texas. https://doi.org/10.3133/fs20173090

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Divisions of geologic time—Major chronostratigraphic and geochronologic units

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