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  2. Geology of Texas - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Texas

    Permian rocks are the best-known of the Texas Paleozoic. They are widespread in north Texas, where their characteristic red beds are spectacularly exposed in Palo Duro Canyon. The strata are also oil-rich where buried in west Texas, such as in the Midland and Odessa region. This crude oil-rich area is known as the Permian Basin.

  3. List of fossiliferous stratigraphic units in Texas - Wikipedia

    en.wikipedia.org/wiki/List_of_fossiliferous_str...

    This article contains a list of fossil-bearing stratigraphic units in the state of Texas, U.S. Sites. Group or Formation ... Starcke Limestone: Silurian: Stone City ...

  4. Cave Without a Name - Wikipedia

    en.wikipedia.org/wiki/Cave_Without_a_Name

    During a 1975 expedition of the Cave Without a Name, cavers mapped out over 2.7 mi (4.3 km) of caverns, making it the seventh-longest cave in Texas. Due to the great natural acoustics created by three large solution domes on the ceiling of the Throne Room, the cave is host to 12 concerts yearly with a maximum attendance of 200 people.

  5. Cambria Cavern - Wikipedia

    en.wikipedia.org/wiki/Cambria_Cavern

    Cambria Cavern was a small limestone solutional cave which was discovered on 8 February 2018 when a portion of the cave's roof collapsed, causing sinkhole opened up in a residential area in Round Rock, Texas. [2] To stabilize the road and utility lines above the cave, the cave was partially filled with concrete and sealed. [3]

  6. Buda Limestone - Wikipedia

    en.wikipedia.org/wiki/Buda_Limestone

    Buda Limestone stratigraphic column in Texas. The Buda Limestone is a geological formation in the High Plains and Trans-Pecos regions of West Texas [1] and in southern New Mexico, [2] whose strata date back to the Late Cretaceous. Pterosaur remains are among the fossils that have been recovered from the formation. [3]

  7. Guadalupe Mountains - Wikipedia

    en.wikipedia.org/wiki/Guadalupe_Mountains

    The Guadalupe Mountains are underlain by Permian aged sedimentary rocks. Although the rocks are now thousands of feet above sea level, sediments that form the rock were deposited in the Delaware Basin, which was a shallow marine coastal setting at the southern edge of what was then the North American craton. [7]

  8. Edwards Group - Wikipedia

    en.wikipedia.org/wiki/Edwards_Group

    The Edwards Group is a geologic group in Texas. It preserves fossils dating back to the Cretaceous period. A stratigraphic column at the Mount Bonnell Fault location starts with the Lower Cretaceous Trinity Group overlain by the Edwards Group. Upper Cretaceous formations follow, starting with the Del Rio Clay, Buda Limestone, and then the Eagle ...

  9. Canyon Lake Gorge - Wikipedia

    en.wikipedia.org/wiki/Canyon_Lake_Gorge

    Part of Canyon Lake Gorge. Canyon Lake Gorge is a limestone gorge in Texas, which is around 1 mile (1.6 km) long, hundreds of yards (metres) wide, and up to 50 feet (15 m) or more deep, which was exposed in 2002 when extensive flooding of the Guadalupe River led to a huge amount of water going over the spillway from Canyon Lake reservoir and removing the sediment from the gorge.

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