Squaw Ridge Lava Field
| Squaw Ridge Lava Field | |
|---|---|
 The Squaw Ridge lava field, also known as the East lava field, is the middle of a group of three young basaltic fields located in the High Lava Plains SE of Newberry volcano. | |
| Highest point | |
| Elevation | 1,711 m (5,614 ft)[1] |
| Coordinates | 43°28′20″N 120°45′13″W / 43.47222°N 120.75361°WCoordinates: 43°28′20″N 120°45′13″W / 43.47222°N 120.75361°W[1] |
| Geography | |
| Location | Lake County, Oregon, United States |
| Geology | |
| Age of rock | Pleistocene[1] |
| Mountain type | Volcanic field[1] |
The Squaw Ridge lava field, also known as the East Lava Field, is a young basaltic field located in the U.S. state of Oregon southeast of Newberry Volcano.[1] The flow erupted from the Lava Mountain shield and is likely related to the Four Craters Lava Field, both of which were created after Mount Mazama erupted.[2]
Notable Vents[]
| Name | Elevation | Location | Last eruption |
|---|---|---|---|
| [3] | 1,711 metres (5,614 ft) | 43°28′19″N 120°45′14″W / 43.472°N 120.754°W | - |
| [3] | 1,525 metres (5,003 ft) | 43°28′N 120°44′W / 43.47°N 120.73°W | - |
See also[]
References[]
- ^ a b c d e "Lava Mountain". Global Volcanism Program. Smithsonian Institution.. Retrieved 2008-05-13.
- ^ Meigs, Andrew; Kaleb Scarberry (2009). "Geological and geophysical perspectives on the magmatic and tectonic development, High Lava Plains and northwest Basin and Range". Volcanoes to Vineyards: Geologic Field Trips through the Dynamic Landscape of the Pacific Northwest. The Geological Society of America (Field Guide 15): 447–448. doi:10.1130/2009.fld015(21).
- ^ a b "Lava Mountain: Synonyms & Subfeatures". Global Volcanism Program. Smithsonian Institution. Retrieved 2008-05-13.
 | This Lake County, Oregon state location article is a stub. You can help Wikipedia by . |
Categories:
- Volcanic fields of Oregon
- Landforms of Lake County, Oregon
- Lava fields
- Oregon geography stubs