Chinati Mountains

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Chinati Mountains
Highest point
Peak Chinati Peak
Elevation 7,728 ft (2,355 m)
Coordinates 29°54′N 104°28′W / 29.900°N 104.467°W / 29.900; -104.467Coordinates: 29°54′N 104°28′W / 29.900°N 104.467°W / 29.900; -104.467
Geography
Country United States
State Texas
Geology
Type of rock Igneous

The Chinati Mountains of Texas are a small range in the high desert of far West Texas near the city of Presidio. There is a pass through the mountains on Ranch to Market Road 2810, also known as Pinto Canyon Road, which connects to Farm to Market Road 170 at Ruidosa, Texas. Some believe the range derives its name from the Apache word ch'íná'itíh, which means gate or mountain pass.

The mountains are primarily composed of igneous and metamorphic rocks, and are believed to be the remains of a number of explosive volcanic caldera-building events in the remote past.[1] The mountains are generally not forested, but rather vegetated with grasses, cactus, and brush typical of the Chihuahuan Desert. The Chinatis were extensively mined for silver from the 1860s through 1910s.[2]

The highest point in the range is Chinati Peak, with an elevation of 7,728 feet (2,355 m). Chinati Peak is also the highest point in Presidio County. It serves as a major landmark for the surrounding area, and its dome-shaped hump can be seen rising prominently in the distance to the southwest from US 90 between Van Horn and Marfa. Chinati Peak is encircled by jagged desert peaks and rugged canyons.[3] The summit of Chinati Peak is broad and relatively flat, but it is surrounded by cliffs and brush-filled drainages on all sides.[3] Sierra Parda, at 7,185 feet (2,190 m), is the second-highest peak in the range.[4]

Chinati Mountains State Park, a park of about 40,000 acres encompassing part of the range, is the second largest state park in Texas. Access to the park has been extremely limited since the land was acquired. However, according to a statement by Texas Parks and Wildlife in October of 2014, public access to the park has finally been secured.[5]

References[edit]

  1. ^ Cepeda, Joseph (November 1983). Oligocene volcanism and multiple caldera formation in the Chinati Mountains, Presidio County, Texas. Austin, Texas: Bureau of Economic Geology, University of Texas at Austin. ISBN 978-99947-61-46-3. 
  2. ^ Tyler, Ron (1996). The Big Bend: a history of the last Texas Frontier. Texas A&M University Press. pp. 136–137. ISBN 978-0-89096-706-5. 
  3. ^ a b "Chinati Peak". SummitPost. Retrieved 2015-04-04. 
  4. ^ "Chinati Mountains". Texas Monthly. Retrieved 2015-04-04. 
  5. ^ "KRTS: Public Access to Chinati Mountains State Natural Area Secured". NPR. Retrieved 2015-04-04. 

External links[edit]