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The Pajarito Plateau is a volcanic plateau … The Pajarito Plateau is a volcanic plateau in north central New Mexico, United States. The plateau, part of the Jemez Mountains, is bounded on the west by the Sierra de los Valles, the range forming the east rim of the Valles Caldera, and on the east by the Puye escarpment, which rises about 300 to 400 feet (90 to 100 m) above the Rio Grande valley about a mile (1.6 km) west of the river. The Rio Grande passes through White Rock Canyon to the southeast, and the Caja del Rio (Cerros del Rio) across the river is sometimes regarded as part of the plateau. The plateau is occupied by several notable entities, including Bandelier National Monument, the town of Los Alamos and its remote suburb White Rock, and Los Alamos National Laboratory. Elevations range from about 5600 feet (1700 meters) at the river to about 7800 feet (2300 meters) where the plateau merges into the mountain range. The Pajarito Plateau is primarily composed of Bandelier Tuff, a voluminous deposit of volcanic tuff laid down in an explosive eruption — in this case, a pair of eruptions from the nearby Valles Caldera. The two ignimbrite-forming eruptions occurred about 1.6 million and 1.2 million years ago and ejected about 300 cubic kilometers of rock each. The orange-pink rock formations constituting the resulting ignimbrites are known as the Otowi and Tshirege Members of the Bandelier tuff. The tuff lies on top of a volcanic field, exposed to the east, which used to be continuous with the Caja del Rio (now across the Rio Grande). Erosion has created a maze of canyons up to 800 feet (240 meters) deep that dissect the plateau into mesas. Many of these mesas climb on the western side rather than descending on all sides, thus sometimes are referred to as potreros. Rock climbing is popular here with locals and visitors alike, and is done in the canyons on basalt cliffs that lie within and below the tuff, which itself is too soft to be climbed safely. The canyons and mesas are highly scenic and well endowed with trails, about which numerous guidebooks have been written. Some trails reach the Rio Grande; others reach the rim of the Valles Caldera. Some are long distance trails, of which a few have been used for ultramarathons and endurance rides. Popular uses include walking, dog walking, running, orienteering and rogaining, mountain biking, and horse riding. Due to constraints of geography and land ownership, both Los Alamos and White Rock are compact populated places. Outside of these, the plateau is sparsely populated and wildlife is abundant and diverse. A large elk herd that spends summers in the Jemez Mountains descends to the Pajarito Plateau during the winter, creating a significant driving hazard. Deer, black bear and coyote are common, and the plateau and mountains support a small but stable population of mountain lions, which typically flee from humans. Smaller mammals such as raccoons, skunks, and gophers are common. Parts of the Bandelier backcountry have been closed seasonally due to nesting bald eagles. The Rio Grande supports a significant migratory flyway that brings many other birds (notably sandhill cranes) to the plateau during migration seasons, and three species of hummingbirds are abundant during summer. White Rock Canyon, the major canyon containing the Rio Grande into which the plateau's canyons empty, is notorious for rattlesnakes. The Pajarito Plateau has been home to Native American communities for at least 11,000 years. Archaeological evidence indicates both seasonal and permanent use of the Plateau throughout the Paleoindian, Archaic, Developmental, Coalition, Classic, and historic periods. Ancestral Puebloans who used the Plateau have ties to modern Puebloan tribes in New Mexico.s to modern Puebloan tribes in New Mexico.
, La meseta del Pajarito es una meseta volcá … La meseta del Pajarito es una meseta volcánica en el centro-norte de Nuevo México en los Estados Unidos de América. La meseta, que es parte de la sierra de Jémez, está flanqueada al oeste por los valles de Caldera y al este por el cañón de la Peña Blanca del río Grande. La meseta está ocupada por diferentes entidades, entre las que podemos mencionar el , el pueblo de Los Álamos y su remoto suburbio White Rock y el laboratorio nacional de Los Álamos. La elevación de la meseta va desde los 1700 m en su base en el río hasta los 2300 m en el punto que la meseta se une a su cordal montañoso. La meseta del Pajarito está compuesta principalmente de ignimbrita, un depósito volcánico de una erupción explosiva; en este caso, un par erupciones del cercano Valles de Caldera. La erosión ha excavado magníficos cañones de hasta 240 metros de profundidad que cortan la meseta en pequeñas mesas. Muchas de estas mesas pueden ser escaladas en su cara occidental por lo que muchas veces se les denomina potreros.que muchas veces se les denomina potreros.
, L'altopiano di Pajarito è un altopiano di … L'altopiano di Pajarito è un altopiano di origine vulcanica nel Nuovo Messico centro-settentrionale, negli Stati Uniti. L'altopiano, parte dei monti Jemez, è delimitato a ovest dalla e ad est dal del Rio Grande. Sull'altopiano si trovano il Bandelier National Monument, la città di Los Alamos e il suo remoto sobborgo White Rock e il Los Alamos National Laboratory. Le altitudini variano da circa 1 700 al fiume a circa 2 300 metri sul livello del mare dove l'altopiano si fonde con la catena montuosa.altopiano si fonde con la catena montuosa.
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The Pajarito Plateau is a volcanic plateau … The Pajarito Plateau is a volcanic plateau in north central New Mexico, United States. The plateau, part of the Jemez Mountains, is bounded on the west by the Sierra de los Valles, the range forming the east rim of the Valles Caldera, and on the east by the Puye escarpment, which rises about 300 to 400 feet (90 to 100 m) above the Rio Grande valley about a mile (1.6 km) west of the river. The Rio Grande passes through White Rock Canyon to the southeast, and the Caja del Rio (Cerros del Rio) across the river is sometimes regarded as part of the plateau. The plateau is occupied by several notable entities, including Bandelier National Monument, the town of Los Alamos and its remote suburb White Rock, and Los Alamos National Laboratory. Elevations range from about 5600 feet (1700 meters) at tge from about 5600 feet (1700 meters) at t
, La meseta del Pajarito es una meseta volcá … La meseta del Pajarito es una meseta volcánica en el centro-norte de Nuevo México en los Estados Unidos de América. La meseta, que es parte de la sierra de Jémez, está flanqueada al oeste por los valles de Caldera y al este por el cañón de la Peña Blanca del río Grande. La meseta está ocupada por diferentes entidades, entre las que podemos mencionar el , el pueblo de Los Álamos y su remoto suburbio White Rock y el laboratorio nacional de Los Álamos. La elevación de la meseta va desde los 1700 m en su base en el río hasta los 2300 m en el punto que la meseta se une a su cordal montañoso.ue la meseta se une a su cordal montañoso.
, L'altopiano di Pajarito è un altopiano di … L'altopiano di Pajarito è un altopiano di origine vulcanica nel Nuovo Messico centro-settentrionale, negli Stati Uniti. L'altopiano, parte dei monti Jemez, è delimitato a ovest dalla e ad est dal del Rio Grande. Sull'altopiano si trovano il Bandelier National Monument, la città di Los Alamos e il suo remoto sobborgo White Rock e il Los Alamos National Laboratory. Le altitudini variano da circa 1 700 al fiume a circa 2 300 metri sul livello del mare dove l'altopiano si fonde con la catena montuosa.altopiano si fonde con la catena montuosa.
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Meseta del Pajarito
, Pajarito Plateau
, Altopiano di Pajarito
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