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Spring Canyon (Alamosa Creek)
Spring Canyon is a canyon and tributary creek of Alamosa Creek in Socorro County, New Mexico. Its source is at an elevation if , in the San Mateo Mountains to the north of Monticello Canyon Monticello Canyon, originally known in Spanish as the Cañada Alamosa (Glen of the Cottonwoods), is a valley or glen drained by Alamosa Creek in Sierra County and Socorro County, New Mexico. Its mouth is at an elevation of , in Sierra County. It ... at . Its mouth is at an elevation if near its creek,s confluence with Alamosa Creek. References Valleys of New Mexico Landforms of Socorro County, New Mexico {{NewMexico-geo-stub ... [...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] |
Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alamosa Creek
Alamosa Creek, also known as Alamosa Arroyo and Alamosa River, is a tributary stream of the Rio Grande in Socorro and Sierra County, New Mexico. Alamosa Creek has its source at at an elevation of 7600 ft / 2,316 meters on the western slope of the San Mateo Mountains in Soccoro. Its mouth was originally at its confluence with the Rio Grande, before that river was flooded by the Elephant Butte Reservoir created by the Elephant Butte Dam. Its mouth is now on the western edge of that reservoir at the mouth of Monticello Canyon Monticello Canyon, originally known in Spanish as the Cañada Alamosa (Glen of the Cottonwoods), is a valley or glen drained by Alamosa Creek in Sierra County and Socorro County, New Mexico. Its mouth is at an elevation of , in Sierra County. It .... References Rivers of Socorro County, New Mexico Rivers of Sierra County, New Mexico Rivers of New Mexico {{NewMexico-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Socorro County, New Mexico
Socorro County is a county in the U.S. state of New Mexico. As of the 2010 census, the population was 17,866. The county seat is Socorro. The county was formed in 1852 as one of the original nine counties of New Mexico Territory. Socorro was originally the name given to a Native American village (''see'': Puebloan peoples) by Don Juan de Oñate in 1598. Having received vitally needed food and assistance from the native population, Oñate named the pueblo ''Socorro'' ("succor" in English). Socorro County is home to multiple scientific research institutions including New Mexico Institute of Mining and Technology, the National Radio Astronomy Observatory and its associated Very Large Array, the Magdalena Ridge Observatory, and the Langmuir Laboratory for Atmospheric Research. Federal public lands in Socorro County include parts of the Cibola National Forest, the Bosque del Apache National Wildlife Refuge, the Sevilleta National Wildlife Refuge, the Bureau of Land Management ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
San Mateo Mountains (Socorro County, New Mexico)
The San Mateo Mountains are a mountain range in Socorro County, in west-central New Mexico in the southwestern United States. The highest point in the range is West Blue Mountain, at 10,336 ft (3,151 m). The range runs roughly north-south and is about 40 miles (64 km) long. It lies about 25 miles (40 km) north-northwest of the town of Truth or Consequences and about 30 miles (48 km) southwest of Socorro. They should not be confused with the identically named range in Cibola and McKinley counties, north of this range. Most of the San Mateo Mountains are within the Magdalena Ranger District of the Cibola National Forest. There are two designated wilderness areas in the range, the Apache Kid Wilderness and the Withington Wilderness . There are three Inventoried Roadless Areas (IRA) within the San Mateos: the Apache Kid Contiguous IRA (67,570 acres), the San Jose IRA (16,957 acres), and the White Cap IRA (8,039). Geology The San Mateo Mountains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monticello Canyon
Monticello Canyon, originally known in Spanish as the Cañada Alamosa (Glen of the Cottonwoods), is a valley or glen drained by Alamosa Creek in Sierra County and Socorro County, New Mexico. Its mouth is at an elevation of , in Sierra County. Its head is at at an elevation of in the San Mateo Mountains, within the Cibola National Forest, in Socorro County. Monticello Canyon is a valley divided into three distinct parts. One is the upper cañada (valley or glen) that lies between the San Mateo Mountains on the north and east (where it has its head), and the Black Range to the west and the Sierra Cuchillo on the southwest. The second lower valley is one the original Spanish settlers named, Cañada Alamosa. It ran from the widened mouth of the canyon southeasterly to the Rio Grande. The two valleys are separated by a narrower canyon, with a gap and box canyon called the Monticello Box at its head at . That canyon cuts down through and divides the San Mateo Mountains to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of New Mexico
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] |
