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The Edwards Plateau is mainly composed of limestone and dolomite, with significant caves and underground water networks. The region is known for its unique karst topography, formed by the dissolution of soluble rocks over time. The deposition in the area includes sedimentary layers that have accumulated over millions of years, resulting in diverse geological formations.
Haden Harrison Edwards introduced 800 families into East Texas in 1825. In 1858 Edwards County is formed. The Aquifer and Plateau were named after the county by reason of their location.
The Edwards Plateau is in Texas and includes counties such as Val Verde, Edwards, Kinney, Real, Menard, Kerr, Kimble, Bandera, Uvalde, and Zavala.
British Columbia
The Cumberland Plateau generally has higher elevations than the Edwards Plateau. The Cumberland Plateau, located in the eastern United States, features elevations that can exceed 2,000 feet, while the Edwards Plateau in Texas typically ranges from about 1,200 to 2,000 feet. Therefore, in terms of average and maximum elevations, the Cumberland Plateau is the higher of the two.
Yes, the Cumberland Plateau is larger than the Edwards Plateau. The Cumberland Plateau spans approximately 8,000 square miles across parts of Kentucky, Tennessee, Virginia, and West Virginia, while the Edwards Plateau covers around 40,000 square miles primarily in Texas. However, the specific areas can vary depending on how the regions are defined. Overall, in terms of size, the Edwards Plateau is significantly larger.
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The Edwards Plateau
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