Raton-Clayton volcanic field
| Raton-Clayton volcanic field | |
|---|---|
|
|
| Highest point | |
| Elevation | 1,550 to 2,700 meters (5,090 to 8,860 ft) |
| Coordinates | 36°30′N 104°18′W / 36.5°N 104.3°WCoordinates: 36°30′N 104°18′W / 36.5°N 104.3°W |
| Geography | |
| Location | New Mexico, US |
| Topo map | USGS Folsom |
| Geology | |
| Age of rock | Pliocene to Holocene? |
| Mountain type | Volcanic field |
| Volcanic arc/belt | Rio Grande Rift |
| Last eruption | 58,000 to 62,000 years ago |
Raton-Clayton volcanic field is an extinct volcanic field located in the state of New Mexico, United States. Capulin Volcano National Monument is located in the volcanic field. It is thought to have been formed by the Raton hotspot.
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