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Manzano Mountains
The Manzano Mountains are a small mountain range in the central part of the US State of New Mexico. They are oriented north–south and are 30 miles long. The center of the range lies due east of the town of Belen. The name "Manzano" is Spanish for "apple tree"; the mountains were named for apple orchards planted at the nearby town of Manzano.Butterfield, Mike, and Greene, Peter, ''Mike Butterfield's Guide to the Mountains of New Mexico'', New Mexico Magazine Press, 2006, The high point of the Manzano Mountains is Manzano Peak (10,098 ft, 3,078 m), at the southern end of the range. Other notable peaks include flat-topped Bosque Peak (9,610 ft, 2,929 m), near the center of the range, and the twin pyramids of Mosca Peak (9,509 ft, 2,898 m) and Guadalupe Peak (9,450 ft, 2,880 m). The last two are the most easily recognized peaks in the range as viewed from Albuquerque. Manzano Peak and Guadalupe Peak are the most dramatic in the range in ...
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Looking South Along The Manzano Mountains From The Gavilan Trail To The Avian Lookout On 3 October 2022
Looking is the act of intentionally focusing visual perception on someone or something, for the purpose of obtaining information, and possibly to convey Interest (emotion), interest or another sentiment. A large number of Troponymy, troponyms exist to describe variations of looking at things, with prominent examples including the verbs "stare, gaze, gape, gawp, gawk, goggle, glare, glimpse, glance, peek, peep, peer, squint, leer, gloat, and ogle".Anne Poch Higueras and Isabel Verdaguer Clavera, "The rise of new meanings: A historical journey through English ways of ''looking at''", in Javier E. Díaz Vera, ed., ''A Changing World of Words: Studies in English Historical Lexicography, Lexicology and Semantics'', Volume 141 (2002), p. 563-572. Additional terms with nuanced meanings include viewing,Madeline H. Caviness, Madeline Harrison Caviness, ''Visualizing Women in the Middle Ages: Sight, Spectacle, and Scopic Economy'' (2001), p. 18. watching,John Mowitt, ''Sounds: The Ambient ...
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Albuquerque Basin
The Albuquerque Basin (or Middle Rio Grande Basin) is a structural basin and ecoregion within the Rio Grande rift in central New Mexico. It contains the city of Albuquerque. Geologically, the Albuquerque Basin is a half-graben that slopes down towards the east to terminate on the Sandia and Manzano mountains. The basin is the largest and oldest of the three major basins in the Rio Grande rift, containing sediments whose depth ranges from . The basin has a semi-arid climate, with large areas that count as desert. Paleo-Indian traces dating back 12,000 years show that the climate used to be wetter and more fertile than it is today. The Rio Grande flows through the basin from north to south, and its valley has been irrigated for at least 1,000 years. Intense irrigation began in the late nineteenth century with new dams, levees and ditches and has caused environmental problems. In times of low water levels in the Rio Grande, Albuquerque relies on groundwater for its potable ...
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Sandia Peak Tramway
The Sandia Peak Tramway is an aerial tramway located adjacent to Albuquerque, New Mexico. It stretches from the northeast edge of the city to Sandia Peak on the ridge line of the Sandia MountainsThe upper station of the tramway is at a point on the main crest of the Sandia Mountains at elevation , about south of Sandia Crest, the high point of the range. The operators of the Tramway term this point "Sandia Peak", but this is a misnomer, as this is not an official name, and it is not a "peak" in the sense of having any topographic prominence. and has the world's third longest single span. It is the longest aerial tram in the Americas, and was the longest in the world from 1966 until being surpassed in 2010 by the Wings of Tatev in Armenia. History The Sandia Peak Ski Company was cofounded by balloonist Ben Abruzzo and Robert Nordhaus (father of Nobel Prize-winning economist William Nordhaus), and Nordhaus was inspired to build a tram to the ski slope after seeing other trams ...
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Albuquerque International Sunport
Albuquerque International Sunport is the primary international airport serving the U.S. state of New Mexico, the Albuquerque metropolitan area, and the larger Albuquerque– Santa Fe– Las Vegas combined statistical area. It handles around 5.4 million passengers annually and over 400 flights daily. ABQ is located in Bernalillo County, New Mexico, between the Rio Grande river and the Sandia Mountains, east of Old Town Albuquerque and Barelas, 3 miles (5 km) southeast of Downtown Albuquerque, south of the University of New Mexico and directly to the west of Sandia National Laboratories and Kirtland Air Force Base. ABQ is a focus airport for Southwest Airlines, which accounts for over half of all passengers, and is served by several major airlines, including Advanced Air , Alaska, American, Boutique Air, Delta, Frontier, JetBlue, Spirit and United; cargo airlines serving the airport are FedEx Express, UPS Airlines, Empire Airlines ( FedEx Feeder carrier) Amer ...
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Cibola National Forest
The Cibola National Forest (pronounced SEE-bo-lah) is a 1,633,783 acre (6,611.7 km2) United States National Forest in New Mexico, USA. The name Cibola is thought to be the original Zuni Indian name for their pueblos or tribal lands. The name was later interpreted by the Spanish to mean "buffalo." The forest is disjointed with lands spread across central and northern New Mexico, west Texas and Oklahoma. The Cibola National Forest is divided into four Ranger Districts: the Sandia, Mountainair, Mt. Taylor, and Magdalena. The Forest includes the San Mateo, Magdalena, Datil, Bear, Gallina, Manzano, Sandia, Mt. Taylor, and Zuni Mountains of west-central New Mexico. The Forest also manages four National Grasslands that stretch from northeastern New Mexico eastward into the Texas Panhandle and western Oklahoma. The Cibola National Forest and Grassland is administered by Region 3 of the United States Forest Service from offices in Albuquerque, New Mexico. Elevation ranges from 5 ...
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Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and ...
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Proterozoic
The Proterozoic () is a geological eon spanning the time interval from 2500 to 538.8million years ago. It is the most recent part of the Precambrian "supereon". It is also the longest eon of the Earth's geologic time scale, and it is subdivided into three geologic eras (from oldest to youngest): the Paleoproterozoic, Mesoproterozoic, and Neoproterozoic. The Proterozoic covers the time from the appearance of oxygen in Earth's atmosphere to just before the proliferation of complex life (such as trilobites or corals) on the Earth. The name ''Proterozoic'' combines two forms of ultimately Greek origin: meaning 'former, earlier', and , 'of life'. The well-identified events of this eon were the transition to an oxygenated atmosphere during the Paleoproterozoic; the evolution of eukaryotes; several glaciations, which produced the hypothesized Snowball Earth during the Cryogenian Period in the late Neoproterozoic Era; and the Ediacaran Period (635 to 538.8 Ma) which is chara ...
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Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies ( marine snow). Sedimentation may also occur as dissolved minerals precipitate ...
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Paleozoic
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in t ...
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Tijeras Canyon
Tijeras Canyon (sometimes also referred to as Tijeras Pass) is a prominent canyon in the central part of the U.S. state of New Mexico. It separates the Sandia Mountains subrange to the north from the Manzano Mountains subrange (specifically the lower "Manzanitas" subrange) to the south. These subranges are part of the larger Sandia–Manzano Mountains; Tijeras Canyon forms a pass through this range. Elevations along the bottom of the canyon range from to above sea level. The canyon drains to the west, into a large dry wash known as Tijeras Arroyo, which runs through Kirtland Air Force Base, passes just south of the Albuquerque International Airport, and then joins the Rio Grande. The arroyo heads at the historically important pass (approximately ), and this pass and the entire canyon are traversed by Interstate 40, following the path of historic U.S. Route 66. (Route 66 originally passed through Santa Fe and entered Albuquerque from the North. In 1937 Governor Arthur Hannett ...
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Rio Grande Rift
The Rio Grande rift is a north-trending continental rift zone. It separates the Colorado Plateau in the west from the interior of the North American craton on the east. The rift extends from central Colorado in the north to the state of Chihuahua, Mexico, in the south. The rift zone consists of four basins that have an average width of . The rift can be observed on location at Rio Grande National Forest, White Sands National Park, Santa Fe National Forest, and Cibola National Forest, among other locations. The Rio Grande rift has been an important site for humans for a long time, because it provides a north–south route that follows a major river. The Rio Grande follows the course of the rift from southern Colorado to El Paso, where it turns southeast and flows toward the Gulf of Mexico. Important cities, including Albuquerque, Santa Fe, Taos, Española, Las Cruces, El Paso, and Ciudad Juárez, lie within the rift. Geology The Rio Grande rift represents the easternmost ma ...
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