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The Magdalena Mountains are a regionally high, mountain range in Socorro County, in west-central New Mexico in the southwestern United States. The highest point in the range is South Baldy, at 10,783 ft (3,287 m), which is also the tallest peak in Socorro County. The range runs roughly north-south and is about 18 miles (28 km) long. The range lies just south of the village of Magdalena, and about 18 miles (28 km) west of Socorro. The Magdalena Mountains are an east-tilted fault-block range, superimposed on Cenozoic calderas. The complex geologic history of the range has resulted in spectacular scenery, with unusual and eye-catching rock formations. They form part of the western edge of the Rio Grande Rift Valley, fronting the La Jencia Basin. The mountains remain isolated and natural due t

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  • Sierra de Magdalena (es)
  • Magdalena Mountains (en)
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  • La sierra de Magdalena es una sierra de gran altitud pero de escasa área que se encuentra en el condado de Socorro en el centro-oeste de Nuevo México en el sudoeste de los Estados Unidos de América. El punto más alto de la sierra en el cerro Pelado del Sur de unos 3 287 m. El cordal montañoso se ubica en dirección norte-sur por unos 28 km de longitud. La sierra se ubica al sur del pueblo de Magdalena y a 28 kilómetros de Socorro. La sierra toma su nombre del pico volcánico de su cara oeste denominado pico Magdalena en honor a María Magdalena. Una formación en forma de talo en el picacho se asemeja a la cara de una mujer.​ (es)
  • The Magdalena Mountains are a regionally high, mountain range in Socorro County, in west-central New Mexico in the southwestern United States. The highest point in the range is South Baldy, at 10,783 ft (3,287 m), which is also the tallest peak in Socorro County. The range runs roughly north-south and is about 18 miles (28 km) long. The range lies just south of the village of Magdalena, and about 18 miles (28 km) west of Socorro. The Magdalena Mountains are an east-tilted fault-block range, superimposed on Cenozoic calderas. The complex geologic history of the range has resulted in spectacular scenery, with unusual and eye-catching rock formations. They form part of the western edge of the Rio Grande Rift Valley, fronting the La Jencia Basin. The mountains remain isolated and natural due t (en)
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  • Magdalena Mountains (en)
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  • Magdalena Mountains (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Bear_on_MtTaylor_USFS.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Kaibab_Elk.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Pronghorn_-_Magdelena_Background.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Strix_occidentalis_lucida-2.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/mule_deer_fawn_in_snow.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/MountainLion_OnMtTaylor_USFS.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/2016_Pano_Magdalena_02.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/MagdalenaMtns_SawmillCanyon.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Magdalena_Mtns_Aspens.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Magdalenas_TimberPeakTrail.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/NMMap-doton-MagdalenaMtns.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Site_of_Kelly,_NM.jpg
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