Zuni-Bandera volcanic field
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| Zuni-Bandera Volcanic Field | |
|---|---|
Bandera Crater in the center is part of the Zuni-Bandera lava field. |
|
| Elevation | 8,366 ft (2,550 m)[1] |
| Location | New Mexico, USA |
| Coordinates | 34°48′00″N 108°00′00″W / 34.8°N 108°W[1] |
| Type | Volcanic field[1] |
| Age of rock | 3.8 million years |
| Last eruption | 1170 BC ± 300 years[1] |
Zuni-Bandera volcanic field (also known as Bandera lava field, Grants Malpais and Malpais volcanic field) is a volcanic field located in the state of New Mexico, United States.[1]
The volcanic field has been considered for geothermal exploitation.[2]
[edit] Notable Vents
| Name | Elevation | Coordinates | Last eruption |
| Cerro Bandera[3][4] | 2,552 metres (8,373 ft) | 35°00′N 108°06′W / 35.0°N 108.1°W | - |
| Bandera Crater[3][4] | 2,533 metres (8,310 ft) | 35°00′N 108°05′W / 35.0°N 108.08°W | 9,500-10,900 years ago[5] |
| El Calderon[3] | 2,320 metres (7,612 ft) | 34°58′N 108°01′W / 34.97°N 108.02°W | - |
| Cerro Colorado[3] | - | - | - |
| Cerro Encierro[3] | 2,298 metres (7,539 ft) | 34°53′N 108°03′W / 34.88°N 108.05°W | - |
| Hoyo De Cibola[3] | 2,380 metres (7,808 ft) | 34°53′N 108°07′W / 34.88°N 108.12°W | - |
| Cerro Hueco (Deer Mountain)[3] | 2,441 metres (8,009 ft) | - | - |
| Laguna[3] | - | - | - |
| Lost Woman[3] | 2,459 metres (8,068 ft) | 34°58′N 108°05′W / 34.97°N 108.08°W | - |
| McCarty's Flow[4][6] | 2,244 metres (7,362 ft) | 35°00′N 107°48′W / 35.0°N 107.8°W | 2,500-3,900 years ago[5] |
| Paxton Springs[3][4] | 2,490 metres (8,169 ft) | 35°04′N 108°04′W / 35.07°N 108.07°W | - |
| Cerro Rendija[3][4] | 2,494 metres (8,182 ft) | 34°57′N 108°08′W / 34.95°N 108.13°W | - |
| La Tetra (Cerro Tetra)[3] | 2,458 metres (8,064 ft) | 34°59′N 108°03′W / 34.98°N 108.05°W | - |
| El Tintero[4] | 2,201 metres (7,221 ft) | - | - |
| Twin Craters[3] | 2,423 metres (7,949 ft) | 34°59′N 108°04′W / 34.98°N 108.07°W | 15,800-17,800 years ago[5] |
[edit] See also
[edit] References
- ^ a b c d e "Zuni-Bandera". Global Volcanism Program. Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=1210-02-. Retrieved on 2008-05-30.
- ^ Laughlin, A.W.; West, F.G. (1975-12-01) (PDF). Zuni Mountains, New Mexico as a potential dry hot rock geothermal energy Site. United States Department of Energy. http://www.osti.gov/energycitations/product.biblio.jsp?osti_id=7366687. Retrieved on 2008-09-12.
- ^ a b c d e f g h i j k l m "Zuni-Bandera - Synonyms and Subfeatures". Global Volcanism Program. Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=1210-02-&volpage=synsub. Retrieved on 2007-05-07.
- ^ a b c d e f M.E. Ander; G. Heiken, J. Eichelberger, A.W. Laughlin, and S. Huestis (1981-05-01) (PDF). Geologic and geophysical investigations of the Zuni-Bandera volcanic field, New Mexico. LA-8827-MS. United States Department of Energy, Los Alamos National Laboratory. http://www.osti.gov/energycitations/product.biblio.jsp?osti_id=6516124.
- ^ a b c "Background on the Zuni-Bandera Volcanic Field" (HTML). New Mexico Bureau of Geology and Mineral Resources. http://geoinfo.nmt.edu/tour/federal/monuments/el_malpais/zuni-bandera/background.html. Retrieved on 2009-06-30.
- ^ "McCartys Flow, Zuni - Bandera Volcanic Field, New Mexico". Volcano World. http://volcano.oregonstate.edu/vwdocs/volc_images/north_america/mccartys_flow.html. Retrieved on 2007-05-08.

