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  2. Balcones Fault - Wikipedia

    en.wikipedia.org/wiki/Balcones_Fault

    Fault or Balcones Fault Zone is an area of largely normal faulting [1] in the U.S. state of Texas that runs roughly from the southwest part of the state near Del Rio to the north-central region near Dallas [2] along Interstate 35. The Balcones Fault zone is made up of many smaller features, including normal faults, grabens, and horsts. [3]

  3. Edwards Plateau - Wikipedia

    en.wikipedia.org/wiki/Edwards_Plateau

    5.35% [1] Protected. 2.26% [1] The Edwards Plateau is a geographic region forming the crossroads of Central, South and West Texas, United States. It is named in honor of Haden Edwards. [2] It is bounded by the Balcones Fault to the south and east; the Llano Uplift and the Llano Estacado to the north; and the Pecos River and Chihuahuan Desert to ...

  4. Edwards Aquifer - Wikipedia

    en.wikipedia.org/wiki/Edwards_Aquifer

    Located in South Central Texas, the Edwards Aquifer encompasses an area of approximately 4,350 square miles (11,300 km 2) that extends into parts of 11 counties. [3] The aquifer's boundaries begin at the groundwater divide in Kinney County, East of Brackettville, and extend Eastward through the San Antonio area and then Northeast where the aquifer boundary ends at the Leon River in Bell County ...

  5. Hill Country State Natural Area - Wikipedia

    en.wikipedia.org/wiki/Hill_Country_State_Natural...

    Set in the scenic hills and canyons typical of the Texas Hill Country, the preserve lies about ten miles north of the Balcones escarpment and within the Balcones Fault Zone. The elevation ranges from approximately 1,280 to 2,000 feet (390 to 610 m). The local Woodard Cave Fault runs through the property on a general east-west line.

  6. Geology of Texas - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Texas

    General geology. Texas is approximately bisected by a series of faults that trend southwest to northeast across the state, from the area of Uvalde to Texarkana. South and east of these faults, the surface exposures consist mostly of Cenozoic sandstone and shale strata that grow progressively younger toward the coast, indicative of a regression ...

  7. Geology of the Dallas–Fort Worth Metroplex - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Dallas...

    Cretaceous Formations of the Dallas-Fort Worth Metroplex Geologic map and the labeled geologic formations that lie directly beneath the surface in Dallas County Cretaceous formations of Texas Where the DFW Metroplex was located during the last super continent known as Pangea Placement of Tectonic Plates and DFW location around ≈94 million years ago The Cretaceous rocks in the DFW Metroplex ...

  8. Salado, Texas - Wikipedia

    en.wikipedia.org/wiki/Salado,_Texas

    Salado is located along the Balcones Fault, which causes the emergence of surface waters. The fault line is also a demarcation line for some species' natural ranges. For example, the California fan palm, Washingtonia filifera, occurs strictly west of Salado or the Balcones Fault. Salado Creek was selected as the first Texas Natural Landmark.

  9. Barton Springs - Wikipedia

    en.wikipedia.org/wiki/Barton_Springs

    Barton Springs is a set of four natural water springs located at Barton Creek on the grounds of Zilker Park [ 2 ] in Austin, Texas, resulting from water flowing through the Edwards Aquifer. The largest spring, Main Barton Spring (also known as Parthenia, "the mother spring"), supplies water to Barton Springs Pool, a popular recreational ...