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  2. Permian Basin (North America) - Wikipedia

    en.wikipedia.org/wiki/Permian_Basin_(North_America)

    The Permian Basin is a large sedimentary basin in the southwestern part of the United States. It is the highest producing oil field in the United States, producing an average of 4.2 million barrels of crude oil per day in 2019. This sedimentary basin is located in western Texas and southeastern New Mexico.

  3. Big Bend (Texas) - Wikipedia

    en.wikipedia.org/wiki/Big_Bend_(Texas)

    Big Bend area map Casa Grande is a prominent peak in the Chisos Mountains of the Big Bend area of west Texas. The view is from the Pinnacles Trail in Big Bend National Park . The Big Bend is part of the Trans-Pecos region in southwestern Texas , United States along the border with Mexico , north of the prominent bend in the Rio Grande for which ...

  4. Trans-Pecos - Wikipedia

    en.wikipedia.org/wiki/Trans-Pecos

    The term is considered synonymous with Far West Texas, a subdivision of West Texas. [2] The Trans-Pecos is part of the Chihuahuan Desert , the largest desert in North America . It is the most mountainous and arid portion of the state, and most of its vast area (outside the city of El Paso ) is sparsely populated.

  5. Edwards Plateau - Wikipedia

    en.wikipedia.org/wiki/Edwards_Plateau

    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 the west. [3]

  6. Top 20 Old Western Towns You Can Still Visit

    www.aol.com/18-towns-where-still-experience...

    3. Bandera, Texas. Nicknamed the "Cowboy Capital of the World," this Wild West town in southern Texas was a staging ground for the last cattle drives of the 1800s.

  7. Davis Mountains - Wikipedia

    en.wikipedia.org/wiki/Davis_Mountains

    The mountains occupy a rough square about 50 km (31 mi) on each side. The mountains are of volcanic origin composed of strata associated with eruptions of the Trans-Pecos Volcanic Field 35 million years ago. [2] The highest peak in the Davis Mountains is Mount Livermore at 2,555 m (8,383 ft) the fifth-highest peak in Texas.

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