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Limpia Canyon
Limpia Canyon is a deep valley or canyon in the Davis Mountains of Jeff Davis County, Texas. It was cut by Limpia Creek and is its path southeastward from the northeastern slope of Mount Livermore at , past Fort Davis and Wild Rose Pass, to its mouth at an elevation of on the eastern edge of the Davis Mountains. History Limpia Canyon was the route of the San Antonio-El Paso Road out of the Pecos River The Pecos River ( es, Río Pecos) originates in north-central New Mexico and flows into Texas, emptying into the Rio Grande. Its headwaters are on the eastern slope of the Sangre de Cristo mountain range in Mora County north of Pecos, New Mexico ... Valley into the Davis Mountains. References Landforms of Jeff Davis County, Texas San Antonio–El Paso Road {{JeffDavisCountyTX-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Davis Mountains
The Davis Mountains, originally known as Limpia Mountains, are a range of mountains in West Texas, located near Fort Davis, after which they are named. The fort was named for then United States Secretary of War and later Confederate President Jefferson Davis. They are a popular site for camping and hiking and the region includes Fort Davis National Historic Site and Davis Mountains State Park. The historical and architectural value of the fort, alongside the rugged natural environment of the park are a significant destination for tourism in Texas. Most of the land in the Davis Mountains is under private ownership as ranch land, but The Nature Conservancy owns or has conservation easements on more than . Description Rather than being a single coherent range, the Davis Mountains are an irregular jumble of isolated peaks and ridges separated by flatter areas. The mountains occupy a rough square about on each side. The mountains are of volcanic origin composed of strata associat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jeff Davis County, Texas
Jeff Davis County is a county in the U.S. state of Texas. As of the 2020 census, its population was 1,996. Its county seat is Fort Davis. The county is named for Jefferson Davis, who served as the 23rd United States Secretary of War in the 1850s, and as President of the Confederate States of America. Jeff Davis County is recognizable for its unique shape; it is a pentagon that has no north–south nor east–west boundaries, save for a six-mile line serving as its southern boundary. It is the only county in the United States that touches a foreign country (Mexico) at a single point. Jeff Davis is one of the nine counties that compose the Trans-Pecos region of West Texas. The county contains the Texas Davis Mountains American Viticultural Area. About are "under vine". The McDonald Observatory, owned by the University of Texas at Austin, is located near Fort Davis. History Native Americans Prehistoric peoples camped at Phantom Lake Spring, in present-day northeastern Jef ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limpia Creek
Limpia Creek, originally known as the Rio Limpia, is a stream that heads in Jeff Davis County, Texas and its mouth is in Pecos County, Texas. Limpa is the Spanish word for "clear or clean water". The creek has its head in the Davis Mountains at an elevation of 7,160 feet, at location on the northeast slope of Mount Livermore. The creek flows 42 miles down Limpia Canyon past Fort Davis and Wild Rose Pass to the canyon mouth, where it turns eastward to its mouth at its confluence with Barrilla Draw, where it disappears into the ground at an elevation of . History Limpia Creek was a water and forage stop on the San Antonio-El Paso Road for freighters, and stage companies like the San Antonio-San Diego Mail Line that had a stop at a camp 32 miles west of Hackberry Pond and 18.86 miles from Fort Davis. The Butterfield Overland Mail located their Limpia Station near the mouth Limpia Canyon 18 miles from Fort Davis, 10 miles west of Barela Springs Station farther down Limpia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Livermore (Texas)
Mount Livermore is a summit in the Davis Mountains in Jeff Davis County, Texas. It reaches an elevation of , and is the fourth highest and most isolated peak in Texas. The peak was named for Major William Livermore who used it as a point of observations and placed a base monument atop it. In October and November 1884, Major Livermore, of the Engineer Corps, was in charge of a military expedition in making a map of western Texas. When reaching the top of the bare rock he called it "Old Baldy", named after a general officer called Baldy Smith. Baldy Peak is an alternate name. The Livermore Cache An extensive cache of arrow points and fragments was excavated by Susan Janes, who moved to Fort Davis with her husband in 1893. In 1895 the Janeses' son Charles, and Tom Merrill found a cairn A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fort Davis, Texas
Fort Davis is an unincorporated community and census-designated place (CDP) in Jeff Davis County, Texas, United States. The population was 1,201 at the 2010 census, up from 1,050 at the 2000 census. It is the county seat of Jeff Davis County. History It was the site of Fort Davis, established in 1854 on the San Antonio–El Paso Road through west Texas and named after Jefferson Davis, who was then the Secretary of War under President Franklin Pierce. It was reestablished in 1867 following the civil war. Geography Fort Davis is located in southeastern Jeff Davis County at the southeast foot of the Davis Mountains. Texas State Highway 17 (State Street) passes through the center of town, leading northeast to Interstate 10 at Balmorhea and southwest to Marfa. Texas State Highway 118 joins Highway 17 through the center of Fort Davis, but leads northwest through the Davis Mountains to I-10 and southeast to Alpine. According to the United States Census Bureau, the CDP has a total a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wild Rose Pass
Wild Rose Pass is a gap in the Davis Mountains in Jeff Davis County, Texas. It lies at an elevation of . History Wild Rose Pass was where travelers on the San Antonio-El Paso Road passed into the uplands of West Texas West Texas is a loosely defined region in the U.S. state of Texas, generally encompassing the arid and semiarid lands west of a line drawn between the cities of Wichita Falls, Abilene, and Del Rio. No consensus exists on the boundary betwee ..., bypassing a narrows in Limpia Canyon on its way to Fort Davis. The site today Wild Rose Pass is today along the route of Texas State Highway 17 northeast of Fort Davis, Texas. References {{coord, 30, 42, 52, N, 103, 46, 57, W, display=title Mountain passes of Texas Landforms of Jeff Davis County, Texas San Antonio–El Paso Road ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pecos River
The Pecos River ( es, Río Pecos) originates in north-central New Mexico and flows into Texas, emptying into the Rio Grande. Its headwaters are on the eastern slope of the Sangre de Cristo mountain range in Mora County north of Pecos, New Mexico, at an elevation of over 12,000 feet (3,700 m). The river flows for 926 miles (1,490 km) before reaching the Rio Grande near Del Rio. Its drainage basin encompasses about 44,300 square miles (115,000 km2).Largest Rivers of the United States USGS The name "Pecos" derives from the (Native American language) term for the |
Landforms Of Jeff Davis County, Texas
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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