page_title: Magdalena Mountains
hierarchical_section_title: Magdalena Mountains
caption_attribution_description: English: The view looking southwest at Sawmill Canyon, near the Langmuir Research Site in the Magdalena Mountains.
context_page_description: 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, which is also the tallest peak in Socorro County. The range runs roughly north-south and is about 18 miles long. The range lies just south of the village of Magdalena, and about 18 miles 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 to the absence of any significant human development within or near the range.
  The range takes its name from a volcanic peak on the west side, named Magdalena Peak, after Mary Magdalene. A talus formation and shrub growth on the east slope of Magdalena Peak is said to resemble a woman's face.
context_section_description: 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 to the absence of any significant human development within or near the range.
  The range takes its name from a volcanic peak on the west side, named Magdalena Peak, after Mary Magdalene.  A talus formation and shrub growth on the east slope of Magdalena Peak is said to resemble a woman's face. According to Julyan's Place Names of New Mexico, one legend about the mountain purports that "a group of Mexicans were besieged by Apaches on the mountain, when the face of Mary Magdalene miraculously appeared, frightening the Indians away."
caption: The view looking southwest at Sawmill Canyon, near the Langmuir Research Site in the Magdalena Mountains.
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