Raton-Clayton volcanic field
| Raton-Clayton volcanic field | |
|---|---|
 | |
| Highest point | |
| Elevation | 1,550 to 2,700 meters (5,090 to 8,860 ft)[1] |
| Coordinates | 36°30′N 104°18′W / 36.5°N 104.3°W[1] |
| Dimensions | |
| Area | 20,000 square kilometres (7,700 sq mi)[2] |
| Geography | |
 | |
| Location | New Mexico, US |
| Topo map | USGS Folsom |
| Geology | |
| Rock age | Miocene-to-Pleistocene[1][3] |
| Mountain type | Volcanic field |
| Volcanic arc/belt | Rio Grande Rift[4][5] |
| Last eruption | 58,000 to 62,000 years ago[6] |
The Raton-Clayton volcanic field is a volcanic field located in the state of New Mexico, United States. Capulin Volcano National Monument is located in the volcanic field. It is the northeasternmost volcanic field of the Jemez Lineament and the easternmost Cenozoic volcanic field of North America.[2]
Geologic setting
[edit]The Raton-Clayton volcanic field is located at the northeastern end of the Jemez Lineament.[7] This is a zone of crustal weakness, possibly corresponding to a boundary between ancient crustal provinces.[8] The region also sits above the eastern end of the Alvarado Ridge, an enormous uplift reaching from the Colorado Plateau to the western High Plains. This is an area underlain by buoyant mantle that is welling up and melting as it decompresses.[7]
Magma rising from the mantle has found a path to the surface through the Jemez Lineament, and produced a cluster of about 125 cinder cones, domes, volcanic necks, and a single shield volcano, Sierra Grande. Volcanism began about 7.2 million years ago, and the most recent eruption was about 60,000 years ago, at Capulin Peak. Prolonged volcanism has added melted lower crust to the original basaltic magma to produce andesite, such as that of Sierra Grande, and dacite, erupted as domes such as Red Mountain.[7]
Phases of volcanism
[edit]Volcanic activity in the field has been divided into three phases. The Raton phase took place 9.1 to 3.6 million years ago and produced mostly olivine basalt. This caps numerous mesas in the area. A smaller volume of silica-rich Red Mountain dacite was also erupted toward the end of this phase. The Raton phase was followed by the Clayton phase, which took place 3.6 to 2.0 million years ago. This began in the eastern part of the field, where Clayton-phase flows sit directly on Raton-phase flows. Further west, there was a significant period of erosion between the two phases. The Clayton-phase magma was more alkaline and produced basalts containing characteristic feldspathoid minerals. The final Capulin phase began less than two million years ago, and erupted alkaline lava that is remarkably uniform in composition, with the exception of one flow from Baby Capulin. This suggests the Capulin eruptions were all from the same magma chamber.[2]
Sierra Grande, the largest volcano in the field, was active during both the Raton and Clayton phases, with flows ranging in age from 3.8 to 2.6 million years. The volcano is largely composed of two-pyroxene andesite, a rock type found almost nowhere else in the Raton-Clayton volcanic field.[2]
Notable Vents
[edit]| Name | Elevation | Location | Last eruption | |
| meters | feet | Coordinates | ||
| Baby Capulin | 2,094 | 6,870 | 36°48′55″N 103°56′10″W / 36.81528°N 103.93611°W | 44.8 ± 2.2 ka[9] |
| Capulin[4] | 2,494 | 8,182 | 36°46′57″N 103°58′11″W / 36.78250°N 103.96972°W | 54.2 ± 1.8 ka[9] |
| Robinson Mountain[10] | 2,452 | 8,045 | - | |
| Sierra Grande[1] | 2,658 | 8,720 | 36°42′20″N 103°52′34″W / 36.70556°N 103.87611°W | about 2 Ma[2] |
See also
[edit]References
[edit]- ^ a b c d Wood, Charles A.; Jűrgen Kienle (1993). Volcanoes of North America. Cambridge University Press. pp. 292–293. ISBN 0-521-43811-X.
- ^ a b c d e Ziegler, Kate E.; Ramos, Frank C.; Zimmerer, Matthew J. (2019). "Geology of Northeastern New Mexico, union and Colfax Counties, New Mexico: A Geologic Summary" (PDF). New Mexico Geological Society Field Conference Series. 70 (4): 47–54. Retrieved 1 September 2020.
- ^ "Raton-Clayton". Global Volcanism Program. Smithsonian Institution. Retrieved 2021-06-28.
- ^ a b "Capulin Mountain, New Mexico". VolcanoWorld. Retrieved 2008-09-02.
- ^ Menzies, Martin A.; Klemperer, Simon L.; Ebinger, C. J.; Baker, Joel (October 2002). Volcanic Rifted Margins (Special Paper (Geological Society of America)). Geological Society of America. p. 48. ISBN 978-0-8137-2362-4.
- ^ "geology". Capulin Volcano National Monument. National Park Service. 2006-07-25. Retrieved 2008-09-02.
- ^ a b c Baldridge, W.S. (2004). "Pliocene-Quaternary volcanism in New Mexico and a model for genesis of magmas in continental extension". In Mack, Greg H.; Giles, Katherine A. (eds.). The Geology of New Mexico: A Geologic History. New Mexico Geological Society. pp. 313–320.
- ^ Whitmeyer, Steven; Karlstrom, Karl E. (2007). "Tectonic model for the Proterozoic growth of North America". Geosphere. 3 (4): 220. doi:10.1130/GES00055.1. Retrieved 18 April 2020.
- ^ a b Ramos, Frank C.; Zimmerer, Matthew J.; Zeigler, Kate E.; Pinkerton, Sydney; Butterfield, Nick (2019). "Geochemistry of Capulin-phase Flows in the Raton-Clayton Volcanic Field" (PDF). New Mexico Geological Society Field Conference Series. 70: 139–149. Retrieved 9 September 2020.
- ^ "Robinson Mountain". TOPOZONE. Retrieved 21 July 2020.
External links
[edit]- "Raton-Clayton Volcanic Field". Capulin Volcano National Monument. National Park Service. 2008-04-14. Retrieved 2015-12-18.
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