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Virginia City is a ghost town in southwest Bailey County, Texas, United States. It was located 2 miles southeast of the present intersection of Farm Roads 298 and 1731 in southwest Bailey County, 25 miles southwest of Muleshoe. It was platted on March 13, 1909, by Matthew C. Vaughn and Samuel D. McCloud.
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Texas has been the leading state in petroleum production since discovery of the Spindletop oil field in 1901. [11] As of October 2017, the State of Texas (if treated as its own nation) is the 7th largest oil producing nation in the world, with production totaling approximately 3.78 million barrels (600 thousand cubic meters ) per day of oil ...
The Northern Plains' climate is semi-arid and is prone to drought, annually receiving between 16 and 32 inches (410 and 810 mm) of precipitation, and average annual snowfall ranging between 15 and 30 inches (380 and 760 mm), with the greatest snowfall amounts occurring in the Texas panhandle and areas near the border with New Mexico.
The most complex Natural Region, it includes Sand Hills, the Stockton Plateau, desert valleys, wooded mountain slopes and desert grasslands. The Basin and Range Province is in West Texas, west of the Pecos River, beginning with the Davis Mountains on the east and the Rio Grande to its west and south. The Trans-Pecos region is the only part of ...
The East Texas iron ore belt spans several counties, including Cherokee, Upshur, Camp, Gregg, Harrison, and others. The geology of the region is dominated by the Weches greensand, which consists of glauconitic sand and clay. This greensand is underlain by various sedimentary formations, including the Queen City sand member and the Sparta sand.
The Texas Hill Country is a geographic region of Central and South Texas, forming the southeast part of the Edwards Plateau. Given its location, climate, terrain, and vegetation, the Hill Country can be considered the border between the American South and Southwest . [ 1 ]
Ward Mountain is located on the west side of the Chisos Mountains in Big Bend National Park. The mountain is composed of rhyolite (volcanic rock) and Chisos Formation which formed during the Oligocene period. [4] [5] Topographic relief is significant as the summit rises 2,500 feet (762 m) above Cottonwood Creek near Ward Spring in 1.25 miles (2 ...