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Wimberley is located in western Hays County 38 miles (61 km) via road southwest of Austin and 58 miles (93 km) northeast of San Antonio.. According to the United States Census Bureau, the city has an area of 9.0 square miles (23.2 km 2), all land.
The system has been explored and mapped by cave divers of the Jacob's Well Exploration Project and has been shown to consist of two principal conduits. One passageway measures approximately 4,500 feet (1,400 m) from the surface with a maximum depth of 137 feet (42 m), and a secondary one extends approximately 1,000 feet (300 m) in length from the point where it diverges from the main conduit.
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 Southeast and Southwest . [ 1 ]
Packsaddle Mountain is a laccolith set in the Chihuahuan Desert where it is a landmark along Highway 118 which skirts the eastern base of the mountain. The mountain is composed of a core of intrusive igneous rock that forced up and breached the roof of light-colored Late Cretaceous sedimentary rock of the Boquillas Formation and the Pen Formation, leaving the strata tilted around the ...
Mount Ol' Baldy is the sole mountain located in Garner State Park. The main trail up the mountain is the most popular trail in Garner State Park and spans nearly 500 feet in elevation. [3] [4] The climb is generally considered to be difficult, due to its steep and rocky terrain. [2] [4] Panoramic outlook near the peak of Mount Old Baldy.
Hays County, Texas – Racial and ethnic composition Note: the US Census treats Hispanic/Latino as an ethnic category. This table excludes Latinos from the racial categories and assigns them to a separate category.
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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 ...