Bandera Volcano Ice Cave

Bandera Volcano Ice Cave, also known as Zuni Ice Cave, is a lava tube cave in New Mexico with an internal temperature significantly less than above-ground summertime ambient temperature; it contains perennial ice.[1] The inside temperatures can fluctuate between −1 and 10 °C (31 and 50 °F). Some areas of the ice cave never reach above freezing. For years, local Indigenous people used the cave to store food.[1]

Zuni-Bandera Ice Cave)

Geology

The lava tube was formed during the Bandera Crater eruption sometime between 9,500 and 10,900 years ago, during one of the many basaltic eruptions in the Zuni-Bandera volcanic field over the past million years.[2][3] The crater's cinder cone is 900-feet high reaching 8,309 feet above sea level.[4]

Ice Cave and Bandera Volcano

The eruption produced numerous formations in addition to lava tubes including a cinder cone, collapse pits, spatter cones and lava spine. The type of lava is ʻAʻā which is more viscous than pāhoehoe.[1] There are many lava tubes and several ice caves in the area including Giant Ice Cave.[4] One has been developed as a commercial ice cave near the Candelaria Trading Post.[3] Lava tubes in the area, "some dating back 115,000 years, formed a network of underground tubes stretching for 17 miles — the longest such system in the continental United States."[4]

Location

The cave system is located in the El Malpais lava field within the boundaries of El Malpais National Monument. The cave's location is N34° 59.556', W108° 04.926'.

  • Ice Cold
    Ice Cold
  • Ice Cave Icicles
    Ice Cave Icicles
  • Down in the Depths
    Down in the Depths
  • Descension into the Ice Cave
    Descension into the Ice Cave

References
  1. "Overview Geology References Pahoehoe Features Lava Tubes A-a Features & Ice Cave Cinder Cone Features of the Bandera Crater flow, Including Aa Lava & Ice Caves". New Mexico Bureau of Geology and Mineral Resources. Retrieved August 5, 2020.
  2. Laughlin, A. William; Poths, Jane; Healey, Heather A.; Reneau, Steven; WoldeGabriel, Giday (February 1, 1994). "Dating of Quaternary basalts using the cosmogenic 3He and 14C methods with implications for excess 40Ar". Geology. 22 (2): 135–138. doi:10.1130/0091-7613(1994)022<0135:DOQBUT>2.3.CO;2.
  3. "Geologic Background Zuni-Bandera Volcanic Field". New Mexico Bureau of Geology and Mineral Resources. Retrieved August 5, 2020.
  4. Benanav, Michael (August 28, 2014). "Into a Lava-Lined Underworld Near Albuquerque". The New York Times. Retrieved August 5, 2020.

34.9916°N 108.0829°W / 34.9916; -108.0829

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