Bosque Peak
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Bosque Peak
Bosque Peak is located on the western flank of the Manzano Mountains in Torrance County, New Mexico, Torrance County, New Mexico. Bosque Peak is within the Cibola National Forest and is ranked the 318th highest peak in New Mexico, and 101st by prominence. References

{{Authority control Landforms of Torrance County, New Mexico Mountains of New Mexico Mountains of Torrance County, New Mexico ...
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Gallo Peak
Gallo Peak is located in the Manzano Mountains in Torrance County, New Mexico. Gallo Peak is in Cibola National Forest, and is ranked the 222nd highest peak in New Mexico. Gallo Peak is 5 miles (8 km) due west of the town Manzano, New Mexico, Manzano and can be accessed via the Red Canyon Road, then onto the Canyon and Crest trails. References

{{Authority control Mountains of New Mexico Landforms of Torrance County, New Mexico Mountains of Torrance County, New Mexico ...
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Torrance County, New Mexico
Torrance County is a county located in the center of the U.S. state of New Mexico. As of the 2020 census, the population was 15,045. The county seat is Estancia. The geographic center of New Mexico is located in Torrance County, southwest of the Village of Willard, and in 2010, the center of population of New Mexico was located in Torrance County, near Manzano. Torrance County is included in the Albuquerque metropolitan area. Geography According to the U.S. Census Bureau, the county has a total area of , of which (0.03%) is covered by water. Most of the county is gently rolling grassland ranging from 6000 to 6200 feet in elevation. The Manzano Mountains rising to 10,098 feet on the western edge of the county provide it with its only significant topographic relief. The Manzano Wilderness area includes the highest part of the mountains. The other notable geographic feature of the county is the series of playas and seasonal lakes centering on Laguna del Perro southeast of ...
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United States Geological Survey
The United States Geological Survey (USGS), founded as the Geological Survey, is an agency of the U.S. Department of the Interior whose work spans the disciplines of biology, geography, geology, and hydrology. The agency was founded on March 3, 1879, to study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The agency also makes maps of planets and moons, based on data from U.S. space probes. The sole scientific agency of the U.S. Department of the Interior, USGS is a fact-finding research organization with no regulatory responsibility. It is headquartered in Reston, Virginia, with major offices near Lakewood, Colorado; at the Denver Federal Center; and in NASA Research Park in California. In 2009, it employed about 8,670 people. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on its hundredth anniversary, was "Earth Science in the Pub ...
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Pennsylvanian (geology)
The Pennsylvanian ( , also known as Upper Carboniferous or Late Carboniferous) is, on the International Commission on Stratigraphy, ICS geologic timescale, the younger of two period (geology), subperiods of the Carboniferous Period (or the upper of two system (stratigraphy), subsystems of the Carboniferous System). It lasted from roughly . As with most other geochronology, geochronologic units, the stratum, rock beds that define the Pennsylvanian are well identified, but the exact date of the start and end are uncertain by a few hundred thousand years. The Pennsylvanian is named after the U.S. state of Pennsylvania, where the coal Bed (geology), beds of this age are widespread. The division between Pennsylvanian and Mississippian (geology), Mississippian comes from North American stratigraphy. In North America, where the early Carboniferous beds are primarily marine limestones, the Pennsylvanian was in the past treated as a full-fledged geologic period between the Mississippian ...
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Lower Permian
The Cisuralian, also known as the Early Permian, is the first series/epoch of the Permian. The Cisuralian was preceded by the Pennsylvanian and followed by the Guadalupian. The Cisuralian Epoch is named after the western slopes of the Ural Mountains in Russia and Kazakhstan and dates between 298.9 ± 0.15 – 272.3 ± 0.5 Ma. In the regional stratigraphy of southwestern North America, the Cisuralian encompasses two series: the Wolfcampian (Asselian to mid-Artinskian) and Leonardian (mid-Artinskian to Kungurian). The series saw the appearance of beetles and flies and was a relatively stable warming period of about 21 million years. Name and background The Cisuralian is the first series or epoch of the Permian. The Cisuralian was preceded by the last Pennsylvanian epoch ( Gzhelian) and is followed by the Permian Guadalupian Epoch. The name "Cisuralian" was proposed in 1982, and approved by the International Subcommission on Permian Stratigraphy in 1996. The Cisuralian Epoch is ...
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Madera Formation
The Madera Group is a group of geologic formations in northern New Mexico. Its fossil assemblage dates the formation to the middle to late Pennsylvanian period. Description The group consists primarily of marine limestones, and it is exposed in the Sandia Mountains, the Lucero Uplift (), the western Jemez Mountains, the Sangre de Cristo Mountains, and in the Manzano Mountains. The lower section of the group tends to be a gray limestone and the upper an arkosic limestone, and these have been divided into the La Pasada Formation and Alamitos Formation in the southern Sangre de Cristo Mountains. In the Manzano Mountains, the Madera has been divided into the Los Moyos, Wild Cow, and Bursum Formations. Another proposed division in the southeastern Sangre de Cristo Mountains is into the Porvenir and Alamitos Formations. Barry Kues and Katherine Giles have recommended the division of the Madera Group into the Gray Mesa Formation and Atrasado Formation in its western and sou ...
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Manzano Mountains
The Manzano Mountains are a small mountain range in the central part of the U.S. 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 language, Spanish for "apple tree"; the mountains were named for apple orchards planted at the nearby town of Manzano, New Mexico, 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 (), at the southern end of the range. Other notable peaks include flat-topped Bosque Peak (), near the center of the range, and the twin pyramids of Mosca Peak () and Guadalupe Peak (). 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 terms of local relief and steepness; however, there are few cliffs i ...
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New Mexico
New Mexico is a state in the Southwestern United States, Southwestern region of the United States. It is one of the Mountain States of the southern Rocky Mountains, sharing the Four Corners region with Utah, Colorado, and Arizona. It also borders the state of Texas to the east and southeast, Oklahoma to the northeast, and shares Mexico-United States border, an international border with the Mexican states of Chihuahua (state), Chihuahua and Sonora to the south. New Mexico's largest city is Albuquerque, and its List of capitals in the United States, state capital is Santa Fe, New Mexico, Santa Fe, the oldest state capital in the U.S., founded in 1610 as the government seat of Santa Fe de Nuevo México, Nuevo México in New Spain. It also has the highest elevation of any state capital, at . New Mexico is the List of U.S. states and territories by area, fifth-largest of the fifty states by area, but with just over 2.1 million residents, ranks List of U.S. states and terri ...
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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, US. 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 5,0 ...
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Landforms Of Torrance County, New Mexico
A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). 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 oceanic basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure stratification, rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as berms, cliffs, hills, mounds, peninsulas, ridges, rivers, valleys, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodi ...
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Mountains Of New Mexico
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains t ...
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