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Cowboy Rim
Cowboy Rim is a cliff that runs along the Continental Divide A continental divide is a drainage divide on a continent such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea, or else is endorheic, not ... in the Animas Mountains of Hidalgo County, New Mexico. It runs west from a point at to its highpoint is at an elevation of at just east of Elephant Butte. Here Cowboy Rim overlooks the Gillespie Creek valley below it to the north, and the Continental Divide runs along this section of the rim, then turns of to the south-southwest from the highpoint, along a ridge west of Elephant Butte Canyon. Cowboy Rim continues eastward to Elephant Butte then turns south-southeastward to . This section of the Rim overlooks the Playas Valley below it to the east. References {{coord, 31, 36, 36, N, 108, 39, 31, W, display=title Cliffs of New Mexico Landforms of Hidalgo Count ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliff
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also fea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Continental Divide
A continental divide is a drainage divide on a continent such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea, or else is endorheic, not connected to the open sea. Every continent on earth except Antarctica (which has no known significant, definable free-flowing surface rivers) has at least one continental drainage divide; islands, even small ones like Killiniq Island on the Labrador Sea in Canada, may also host part of a continental divide or have their own island-spanning divide. The endpoints of a continental divide may be coastlines of gulfs, seas or oceans, the boundary of an endorheic basin, or another continental divide. One case, the Great Basin Divide, is a closed loop around an endoreic basin. The endpoints where a continental divide meets the coast are not always definite since the exact border between adjacent bodies of water is usually not clearly defined. The I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Animas Mountains
The Animas Mountains are a small mountain range in Hidalgo County, within the " Boot-Heel" region of far southwestern New Mexico, in the United States. They extend north–south for about 30 miles (50 km) along the Continental Divide,Since both of the neighboring valleys are closed drainage basins, the designation of the Continental Divide in this region is somewhat arbitrary. from near the town of Animas to a few miles north of the border with Mexico. The range is about 12 miles (20 km) wide at its widest. The highest point of the range is the southern summit of the mile-long Animas Peak massif, . (Animas Peak itself is the slightly lower north summit, 8,531 ft/2,600 m.) The Animas Mountains lie between the Animas Valley on the west and the Playas Valley on the east. Nearby ranges include the Peloncillo Mountains (Hidalgo County), across the Animas Valley, and the Big Hatchet and Little Hatchet Mountains, across the Playas Valley. Butterfield, Mike, and Greene ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hidalgo County, New Mexico
Hidalgo County ( es, Condado de Hidalgo) is the southernmost county of the U.S. state of New Mexico. As of the 2010 census, the population was 4,894. The county seat and largest city is Lordsburg. A bill creating Hidalgo from the southern part of Grant County was passed on February 25, 1919, taking effect at the beginning of 1920. The county was named for the town north of Mexico City where the Treaty of Guadalupe Hidalgo was signed,Herrera, Mary (Secretary of State) (2008) ''New Mexico Blue Book 2007-2008'' Office of the Secretary of State, Santa Fe, New Mexico, page 226 which in turn was named for Miguel Hidalgo y Costilla, the priest who is known as the "Father of Mexican Independence." The county is located on the Mexico–United States border. Geography According to the U.S. Census Bureau, the county has a total area of , of which is land and (0.3%) is water. The southern part of the county, the part bounded on the east and south by Mexico, is known as the Bootheel. Adj ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elephant Butte (Hidalgo County, New Mexico)
Elephant Butte is a summit in Hidalgo County, New Mexico Hidalgo County ( es, Condado de Hidalgo) is the southernmost county of the U.S. state of New Mexico. As of the 2010 census, the population was 4,894. The county seat and largest city is Lordsburg. A bill creating Hidalgo from the southern part .... It lies at an elevation of , on the Cowboy Rim of the Animas Mountains. References Mountains of New Mexico Landforms of Hidalgo County, New Mexico Mountains of Hidalgo County, New Mexico {{NewMexico-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gillespie Creek (New Mexico)
Gillespie Creek is an intermittent stream or arroyo Arroyo often refers to: * Arroyo (creek), an intermittently dry creek Arroyo may also refer to: People * Arroyo (surname) Places United States ;California * Arroyo Burro Beach, a public beach park in Santa Barbara County, California * Arroyo ... in Hidalgo County, New Mexico. Gillespie Creek is 11 miles long, that heads in the Animas Mountains at , and flows northeasterly until it ends in the Playas Valley, at an elevation of . Its waters in flood would reach Playas Lake. Its mouth is located 24 miles south southeast of Animas. Bennett Creek is a tributary that has its confluence with Gillespie Creek at an elevation of . References Rivers of Hidalgo County, New Mexico Rivers of New Mexico {{NewMexico-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elephant Butte Canyon
Elephant Butte Canyon or Lawhorn Canyon is a 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 tenden ... in the Animas Mountains of Hidalgo County, New Mexico. Its stream is a tributary of Walnut Creek. Its mouth is located at elevation 5,535 feet / 1,687 feet at its confluence with Walnut Creek, just below Lawhorn Tank. Its source is located at 3.5 miles north northeast of its mouth at an elevation of on the southwest slope of Elephant Butte. References {{authority control Landforms of Hidalgo County, New Mexico Canyons and gorges of New Mexico Rivers of New Mexico Rivers of Hidalgo County, New Mexico ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Playas Valley
The Playas Valley is a lengthy and narrow 60-mi (97-km) long, valley located in Hidalgo County, New Mexico in the Bootheel Region; the extreme south of the valley lies in Chihuahua. Playas, NM is located in the northeast. The valley is noteworthy for the Playas Lake, (dry lake) in the north. The Continental Divide of the Americas forms its western border in a series of three linear mountain ranges, and the divide forms the water divide as the northern border of the Playas Valley. The valley disappears southward into regions of the northwest Chihuahuan Desert of Chihuahua, Mexico. Regions of the desert extend northward to foothills of various mountain ranges, canyons, washes, or other landforms. Description The Playas Valley is linear, and north–south trending and surrounded by mountain ranges, except on the south, where the flatlands merge into the Chihuahuan Desert. ''West'' *Pyramid Mountains *Animas Mountains *San Luis Mountains ''East'' *Little Hatchet Mountains *Big ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliffs Of New Mexico
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
