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Fryingpan Canyon
Fryingpan Canyon, a valley in the Cookes Range, in Luna County, New Mexico. Its mouth lies at 4715 feet (1437m), at its confluence with Starvation Draw. Its source lies at 5560 feet, at , in the Cookes Range, on the east slope of Rattlesnake Ridge Rattlesnake Ridge, known as daʔšədabš to the Snoqualmie people, is the ridge of Rattlesnake Mountain located south of North Bend, Washington, United States. The western end is near the intersection of State Route 18 and I-90 in Snoqualmie, W ... at its eastern end. References History of Luna County, New Mexico Landforms of Luna County, New Mexico Canyons and gorges of New Mexico Cooke's Wagon Road {{NewMexico-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between hills or 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 glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these 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 areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cookes Range
The Cookes Range (Cooke's Range, Cooks Range or Cook's Range) is a small, 17-mi (27 km) long mountain range in northern Luna County, New Mexico, which extends slightly north into southeastern Grant County. The range is a southern continuation of the Mimbres Mountains, itself the southeast portion of the extensive north–south running Black Range. The Cookes Range is surrounded by lower elevation areas of the northwest Chihuahuan Desert. Description Cookes Range is about 17 mi long, and about 8 mi at its widest. The range is a basin and range north-south trending uplift with a center-north section intruded by granodiorite which forms Cookes Peak, . Cookes Peak is at the head of OK Canyon, which exits the range eastwards. South of OK Canyon is a transverse ridgeline, across the range west to east, named Rattlesnake Ridge. One other larger peak occurs in the mountains and hills in the southern part of the range, Massacre Peak, at . Other outlying lower elevation hil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Luna County, New Mexico
Luna County is a county located in the U.S. state of New Mexico. As of the 2010 census, the population was 25,095. Its county seat is Deming. This county abuts the Mexican border. Luna County comprises the Deming, NM Micropolitan Statistical Area. History Luna County was formed from parts of Grant County and Doña Ana County by the New Mexico Legislature on March 16, 1901. It was named for Solomon Luna, a politician who advocated for independence of the county, following a strong rivalry between the cities of Deming and Silver City, both of which were at the time in Grant County. Before dawn on March 16, 1916, Mexican revolutionary Pancho Villa led several hundred of his rebel soldiers across the Mexican border into the southern county village of Columbus. The invaders raided and burned much of the town, causing many residents to flee to the desert. Although the raid completely surprised everyone in the town, it also awakened 350 United States Army soldiers at Camp F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Starvation Draw
Starvation Draw, a valley in the Cookes Range, in Luna County, New Mexico. Its mouth lies at an elevation of 4291 feet (1308m). Its source lies at an elevation of 5800 feet, at , in the Cookes Range, on the south slope of Rattlesnake Ridge Rattlesnake Ridge, known as daʔšədabš to the Snoqualmie people, is the ridge of Rattlesnake Mountain located south of North Bend, Washington, United States. The western end is near the intersection of State Route 18 and I-90 in Snoqualmie, W .... References Landforms of Luna County, New Mexico Valleys of New Mexico {{NewMexico-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rattlesnake Ridge (Luna County, New Mexico)
Rattlesnake Ridge, known as daʔšədabš to the Snoqualmie people, is the ridge of Rattlesnake Mountain located south of North Bend, Washington, United States. The western end is near the intersection of State Route 18 and I-90 in Snoqualmie, Washington, and runs southeast about or by trail. It is the highest and easternmost of the Issaquah Alps (although Cedar Butte in the gap between Rattlesnake Mountain and the Cascade front at Mount Washington is considered by Harvey Manning to be a quasi-Alp). A maze of abandoned logging roads and constructed trails have been strung together to provide a footpath from the Snoqualmie Point trailhead at Exit 27 on I-90 all the way to the Rattlesnake Lake trailhead near Exit 32. Rattlesnake Ledge is a rock outcropping and viewpoint 1160 feet above Rattlesnake Lake. Rattlesnake Ledge is a very popular hike destination. The Rattlesnake Ledge Trail makes up the eastern 2 mile segment of the Rattlesnake Ridge or Rattlesnake Mountain Trail. S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
History Of Luna County, New Mexico
History (derived ) is the systematic study and the documentation of the human activity. The time period of event before the invention of writing systems is considered prehistory. "History" is an umbrella term comprising past events as well as the memory, discovery, collection, organization, presentation, and interpretation of these events. Historians seek knowledge of the past using historical sources such as written documents, oral accounts, art and material artifacts, and ecological markers. History is not complete and still has debatable mysteries. History is also an academic discipline which uses narrative to describe, examine, question, and analyze past events, and investigate their patterns of cause and effect. Historians often debate which narrative best explains an event, as well as the significance of different causes and effects. Historians also debate the nature of history as an end in itself, as well as its usefulness to give perspective on the problems of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Luna 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, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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