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Ladrón Peak is an isolated, highly visible peak in central New Mexico, lying about 50 mi (80 km) southwest of Albuquerque. Ladron Peak is the only major peak in the compact range (really one large massif) known as the Sierra Ladrones, which lies between the Rio Puerco to the east and the Rio Salado to the southwest.

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  • Ladrón Peak (de)
  • Pico Ladrón (es)
  • Ladron Peak (en)
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  • Ladrón Peak ist ein einzeln gelegener, gut sichtbarer Berg in der Mitte von New Mexico etwa 80 km südwestlich von Albuquerque. Ladron Peak ist der einzige größere Gipfel in dem Sierra Ladrones genannten Gebirgsmassiv, das zwischen dem im Osten und dem im Südwesten liegt. Trotz seines vulkanartigen Aussehens und der Nähe zu Lavaströmen und kleineren Vultanen handelt es sich nicht um einen Vulkan, sondern einen Berg aus Granit aus dem Präkambrium. (de)
  • Ladrón Peak is an isolated, highly visible peak in central New Mexico, lying about 50 mi (80 km) southwest of Albuquerque. Ladron Peak is the only major peak in the compact range (really one large massif) known as the Sierra Ladrones, which lies between the Rio Puerco to the east and the Rio Salado to the southwest. (en)
  • Pico Ladrón (en inglés: Ladron Peak) es un pico aislado, muy visible en el centro de Nuevo México, en los Estados Unidos situado a cerca de 50 millas (80 km) al suroeste de Albuquerque. El Pico Ladrón es el único pico importante en la cordillera compacta (en realidad un gran macizo), conocida como la Sierra Ladrones, que se encuentra entre el río Puerco al este y el río Salado hacia el suroeste. (es)
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  • Ladrón Peak (en)
name
  • Ladrón Peak (en)
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  • Socorro County, New Mexico, U.S. (en)
range
  • Sierra Ladrones (en)
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  • 34.434813733 -107.085098083
has abstract
  • Ladrón Peak ist ein einzeln gelegener, gut sichtbarer Berg in der Mitte von New Mexico etwa 80 km südwestlich von Albuquerque. Ladron Peak ist der einzige größere Gipfel in dem Sierra Ladrones genannten Gebirgsmassiv, das zwischen dem im Osten und dem im Südwesten liegt. Trotz seines vulkanartigen Aussehens und der Nähe zu Lavaströmen und kleineren Vultanen handelt es sich nicht um einen Vulkan, sondern einen Berg aus Granit aus dem Präkambrium. (de)
  • Ladrón Peak is an isolated, highly visible peak in central New Mexico, lying about 50 mi (80 km) southwest of Albuquerque. Ladron Peak is the only major peak in the compact range (really one large massif) known as the Sierra Ladrones, which lies between the Rio Puerco to the east and the Rio Salado to the southwest. Despite its conical shape and its proximity to lava flows and small volcanoes, it is not itself a volcano, but an igneous intrusion. The core of the mountain is Precambrian granite. The peak rises dramatically from its surroundings on all sides; the summit is almost 4,500 feet (1,370 m) above the Rio Grande Valley, 10 miles (16 km) to the east. The name of the peak means "thief", and "Sierra Ladrones" means "thieves' mountains." Navajo and Apache raiding parties, and later Hispanic and Anglo rustlers, used the mountains as hideouts, hence the name. Evidence of human occupation goes back over 10,000 years, and more recent prehistoric use occurred by the Mogollon and Anasazi cultures. Today, part of the range is included in the Sevilleta National Wildlife Refuge, administered by the US Fish and Wildlife Service. The rest of the range is a mix of BLM and private land. Ecologically, Ladrón Peak is a sky island, supporting vegetation and wildlife not found in the surrounding grasslands. It is high enough to have coniferous forests on its upper slopes. Animal species include mountain lion, bear, pronghorn, elk, deer and reintroduced desert bighorn sheep. (en)
  • Pico Ladrón (en inglés: Ladron Peak) es un pico aislado, muy visible en el centro de Nuevo México, en los Estados Unidos situado a cerca de 50 millas (80 km) al suroeste de Albuquerque. El Pico Ladrón es el único pico importante en la cordillera compacta (en realidad un gran macizo), conocida como la Sierra Ladrones, que se encuentra entre el río Puerco al este y el río Salado hacia el suroeste. A pesar de su forma cónica y su proximidad a los flujos de lava y volcanes pequeños, no es en sí mismo un volcán. El núcleo de la montaña es de granito precámbrico​ El punto más alto se eleva dramáticamente de su entorno en todos los lados. La cumbre alcanza casi los 4.500 pies (1.350 m) por encima del Valle del Río Grande, a 10 millas al este. (es)
easiest route
  • off-trail hike/scramble from west side (en)
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  • POINT(-107.0850982666 34.434814453125)
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