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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] |
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] |
Rio Grande
The Rio Grande ( and ), known in Mexico as the Río Bravo del Norte or simply the Río Bravo, is one of the principal rivers (along with the Colorado River) in the southwestern United States and in northern Mexico. The length of the Rio Grande is . It originates in south-central Colorado, in the United States, and flows to the Gulf of Mexico. The Rio Grande drainage basin (watershed) has an area of ; however, the endorheic basins that are adjacent to and within the greater drainage basin of the Rio Grande increase the total drainage-basin area to . The Rio Grande with Rio Grande Valley (landform), its fertile valley, along with its tributaries, is a vital watersource for seven US and Mexican states, and flows primarily through arid and semi-arid lands. After traversing the length of New Mexico, the Rio Grande becomes the Mexico–United States border, between the U.S. state of Texas and the northern Mexican states of Chihuahua (state), Chihuahua and Coahuila, Nuevo León a ... [...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] |
Monticello, New Mexico
Monticello is an unincorporated community located in Sierra County, New Mexico, United States. Monticello is located on Alamosa Creek, northwest of Truth or Consequences. Monticello has a post office with ZIP code 87939. History Canada Alamosa What became Monticello was first some farms established by 1863 in the upper part of the valley, originally named Cañada Alamosa, through which Alamosa Creek (then called Arroyo Alamosa or Rio Alamosa) ran to the Rio Grande. These farms were owned by residents of a native New Mexican agricultural settlement named San Ygnacio de la Alamosa that had been founded in 1859. San Ygnacio de la Alamosa, commonly called Alamosa, was located at the confluence of the Arroyo Alamosa and the Rio Grande along the wagon road that ran along the west side of the river between Fort Craig and Fort Thorn. Alamosa was the town which was called ''Canada Alamosa'' in Union Army reports, that was the site of Battle of Canada Alamosa between a Confederat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cañada Viviancito
Cañada Viviancito, is a tributary arroyo of Alamosa Creek, and a side cañada in Monticello Canyon, in Sierra County, New Mexico ) , population_demonym = New Mexican ( es, Neomexicano, Neomejicano, Nuevo Mexicano) , seat = Santa Fe , LargestCity = Albuquerque , LargestMetro = Tiguex , OfficialLang = None , Languages = English, Spanish ( New Mexican), Navajo, Ker .... Its mouth is at its confluence with the creek at an elevation of within Monticello Canyon. The source of the arroyo is at an elevation of , while the head of the cañada is at an elevation of at . References Valleys of New Mexico Landforms of Sierra County, New Mexico Rivers of Sierra County, New Mexico {{NewMexico-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monticello Box
Monticello Box or Monticello Box Canyon is a narrow canyon, a gap and a box canyon in the middle of the wider valley or glen 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 .... The two wider valleys are separated by a narrower canyon, with a gap and box canyon called the Monticello Box at its head. References {{NewMexico-geo-stub Valleys of New Mexico ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Box Canyon
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] |
Gap (landform)
A gap is a geological formation that is a low point or opening between hills or mountains or in a ridge or mountain range. It may be called a col, notch, mountain pass, pass, saddle (landform), saddle, water gap, or wind gap, and geomorphology, geomorphologically is most often carved by water erosion from a freshet, stream or a river. Gaps created by freshets are often, if not normally, devoid of water through much of the year, their streams being dependent upon the meltwaters of a snow pack. Gaps sourced by small spring (hydrology), springs will generally have a small stream excepting perhaps during the most arid parts of the year. Water gaps of necessity often cut entirely through a mountain chain, barrier barrier ridge, range and riverine gaps may create canyons such as the riverine gaps of the Danube River, Lehigh River Gorge, the Colorado River's Grand Canyon and the Genesee River. Such cuttings may expose millennia of strata in the local rock column writing the geologic reco ... [...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] |
Sierra Cuchillo
Sierra Cuchillo (knife mountains) or Cuchillo Negro Mountains is a range of mountains, primarily in Sierra County and some in southern Socorro County, New Mexico. They were named for the knife-like shape of some of the peaks in the range, or for Cuchillo Negro Baishan, Spanish name Cuchillo Negro (Black Knife) (c. 1796 – May 24, 1857), was a Tchihende ( Mimbres) Apache chieftain, of the Warm Springs Apache Band during the 1830s to 1850s. Apache war-leader and chief Baishan ("Knife"), son of the ... an Apache leader in the region in the mid 19th century. References Mountain ranges of New Mexico Mountain ranges of Sierra County, New Mexico Mountain ranges of Socorro County, New Mexico {{NewMexico-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glen
A glen is a valley, typically one that is long and bounded by gently sloped concave sides, unlike a ravine, which is deep and bounded by steep slopes. Whittow defines it as a "Scottish term for a deep valley in the Highlands" that is "narrower than a strath".. The word is Goidelic in origin: ''gleann'' in Irish and Scottish Gaelic, ''glion'' in Manx. The designation "glen" also occurs often in place names. Etymology The word is Goidelic in origin: ''gleann'' in Irish and Scottish Gaelic, ''glion'' in Manx. In Manx, ''glan'' is also to be found meaning glen. It is cognate with Welsh ''glyn''. Examples in Northern England, such as Glenridding, Westmorland, or Glendue, near Haltwhistle, Northumberland, are thought to derive from the aforementioned Cumbric cognate, or another Brythonic equivalent. This likely underlies some examples in Southern Scotland. As the name of a river, it is thought to derive from the Irish word ''glan'' meaning clean, or the Welsh word ''gleindid' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Range
Black is a color which results from the absence or complete absorption of visible light. It is an achromatic color, without hue, like white and grey. It is often used symbolically or figuratively to represent darkness. Black and white have often been used to describe opposites such as good and evil, the Dark Ages versus Age of Enlightenment, and night versus day. Since the Middle Ages, black has been the symbolic color of solemnity and authority, and for this reason it is still commonly worn by judges and magistrates. Black was one of the first colors used by artists in Neolithic cave paintings. It was used in ancient Egypt and Greece as the color of the underworld. In the Roman Empire, it became the color of mourning, and over the centuries it was frequently associated with death, evil, witches, and magic. In the 14th century, it was worn by royalty, clergy, judges, and government officials in much of Europe. It became the color worn by English romantic poets, businessmen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
