Elephant Butte Canyon
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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 ...
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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 ...
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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 ...
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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 ...
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Walnut Creek (Playas Valley, New Mexico)
Walnut Creek is an intermittent stream in Hidalgo County, New Mexico. It has its source in the Animas Mountains on the east slope of the Continental Divide at an elevation of at . Its mouth is located at an elevation of where it subsides into the 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 notewort .... References Rivers of Hidalgo County, New Mexico Rivers of New Mexico {{NewMexico-river-stub ...
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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 ...
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Landforms Of Hidalgo County, New Mexico
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, plateau ...
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Canyons And Gorges Of New Mexico
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the 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 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. Examples of mountain-type c ...
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Rivers Of New Mexico
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as Stream#Creek, creek, Stream#Brook, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to Geographical feature, geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "Burn (landform), burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from Precipitation (meteorology), precipitation through a ...
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