Search results
Results from the WOW.Com Content Network
Dermatophyllum secundiflorum is a species of flowering shrub or small tree in the family Fabaceae [2] that is native to the Southwestern United States (Texas, New Mexico) and Mexico (Chihuahua and Coahuila south to Hidalgo, Puebla, and Querétaro). [3] Its common names include Texas mountain laurel, Texas mescalbean, frijolito, and frijolillo. [2]
Kit Mountain is part of the Chisos Mountains where it is set in the Chihuahuan Desert and Big Bend National Park.The mountain is composed chiefly of Burro Mesa Formation tuff (volcanic rock) overlaying Chisos Formation which formed 29 million years ago during the Oligocene period. [4]
The mountain was the site of the Packsaddle Mountain Fight with 21 Apache Tribesmen on August 4, 1873 and was the last major Indian battle in the area. The fight on Packsaddle Mountain was precipitated when a woman from the Moss Ranch (in what is now Llano County) came into the ranch house with an arrow sticking out of her side.
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
Nugent Mountain is located in Big Bend National Park and the Chisos Mountains. The mountain is composed of intrusive igneous rock which formed during the Oligocene period. [5] Although modest in elevation, topographic relief is significant as the summit rises 1,600 feet (488 m) above the Rio Grande Village Road in one mile (1.6 km).
Goat Mountain is part of the Chisos Mountains where it is set in Big Bend National Park and the Chihuahuan Desert. The top of the mountain is composed of Burro Mesa Rhyolite (volcanic rock) which formed 29 million years ago during the Oligocene period.
Crown Mountain is located in Big Bend National Park and the Chisos Mountains. It ranks as the sixth-highest peak in this park, mountain range, and county, but only the 34th-highest in Texas. [1] [2] The mountain is composed of volcanic rock of the Chisos Formation which formed during the Paleogene period. [4]
The mountain is a soda microsyenite volcanic plug which formed 34 million years ago when it intruded three Late Cretaceous marine sedimentary formations which included the Boquillas Formation and the Pen Formation. [6] Based on the Köppen climate classification, Bee Mountain is located in a hot arid climate zone with hot summers and mild ...