Search results
Results from the WOW.Com Content Network
The Texas state historical marker reads "Two and one half miles east on the Packsaddle Mountain, in a battle fought August 4, 1873, Captain J. R. Moss, Stephen B. Moss, William B. Moss, Eli Lloyd, Arch Martin, Pink Ayers, E. D. Harrington, and Robert Brown routed a band of Indians thrice their number. The last Apache battle in this region."
The Texas State Historical Society states it covers all or part of 33 Texas counties, six fewer than as depicted by a US Geological Survey map, and four New Mexico counties. [2] As depicted by a US Geological Survey map, the Llano Estacado includes all or part of these Texas counties: [12] [13]
Peaks in the state of Texas [1] [2] [3] Mountain Peak Elevation Prominence Isolation Location Mountain range County; Guadalupe Peak: 8,751 ft 2667 m: 3,031 ft 924 m: 72.6 mi 116.9 km Guadalupe Mountains: Culberson: Shumard Peak: 8,635 ft 2632 m: 899 ft
Name Image Date Location County Ownership Description Attwater Prairie Chicken Preserve: 1968: Colorado: federal/US Fish & Wildlife Service Contains the only significant segment of gulf coastal prairie.
The geography of Texas is diverse and large. Occupying about 7% of the total water and land area of the U.S., [1] it is the second largest state after Alaska, and is the southernmost part of the Great Plains, which end in the south against the folded Sierra Madre Oriental of Mexico.
Black Mountain is the ninth-highest peak in the Davis Mountains and it ranks as 21st-highest in the state of Texas. [1] [2] Topographic relief is significant as the summit rises over 2,000 feet (610 m) above Big Aguja Canyon in 1.25 mile (2 km). The mountain is composed of 35 million-year-old igneous rock. [4]
Davis Mountains: 35 million years old and formed by magma from two volcanic centers Quitman Mountains: series of calderas from the Eocene period that includes volcanic rocks
Llano Uplift - geologic map. The Llano Uplift can be considered an uplift by either its pattern on a geological or structural map of the top of the Precambrian rocks. It qualifies as an uplift because it consists of an extensive Precambrian basement high that is exposed by virtue of its surface lying significantly above in elevation the surface of surrounding Precambrian basement.