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Travis Texas Form 941-SS: What You Should Know
The Comanche Peak is one of the largest known deposits of limestones in the region and the largest known limestone deposit in Texas. The peak is at one of the highest elevations in the Comanche Peak area (>14,000 feet). The Edwards Limestone is the younger, and generally younger, of the three known formations in the Comanche Peak area. The Edwards Formation was identified in 1902 by John E. Edwards and has since become the official name for the group. The Georgetown Limestone was first recognized in 1913 by James D. Gordon. A small portion of the original well base from wells drilled during the early 1920s has been excavated and identified from these strata. Elevations and water table in the Comanche Peak area, TX -- Travis County WATER DATA FOR THE COMANCHE Peak Data Analysis at USGS National Data Center for the Comanche Peak, TX USGS National Data Center for the Comanche Peak, TX The Comanche Peak is shown as: In this figure, the water table is shown as being at 624 m. This figure also shows that the Edwards Limestone has a water level of 622 m., which agrees with the reported data above. This figure shows that the waters are generally between 622 and 624 m. This figure also shows that the Edwards Limestone and Georgetown's Stone-Ribbon formation have water levels of 612 and 624 m, respectively. THIS IS THE NEWEST VERSION USGS National Data Center for the Comanche Peak, TX Using the new data from the USGS National Data Center for this project, this is the most current version of our information for the Comanche Peak area, Texas -- Travis County. The new data shows water levels at 624 m in the Edwards Limestone. This also places the Comanche Peak well base within these waters. WATER LEVELS (in meters) FOR THE EDWARDS LEVITES The new data shows the waters above 642 m (the water level noted on the original information for the Edwards) has shifted to be between 489 and 505 m. This also places the Edwards well base within water depths of these waters.
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