 | This article relies largely or entirely on a
single source. (November 2023) |
The Tumble Buttes are a group of cinder cone volcanoes in the US state of California.
The Tumble Buttes are formed by three pyroclastic cinder cones: Bear Wallow Butte, Eiler Butte, and Hall Butte. They range in elevation from 6,391 feet (1,948 m) to 7,188 feet (2,191 m). [1] The volcanoes trend north-northwest to south-southeast along a fissure. Eiler Butte marks the northern end, while Bear Wallow Butte is the southernmost cone. [1]
The Tumble Buttes last erupted between 10,000 and 15,000 years ago, making them either Pleistocene or Holocene in age. The cinder cones have erupted lava flows. [1]
Bear Wallow Butte has unvegetated lava flows on both its eastern and western flanks; Eiler Butte has produced blocky lava. [1]
- ^ a b c d "Tumble Buttes". Global Volcanism Program. Smithsonian Institution. 2013. Retrieved November 21, 2023.
40°40′50″N 121°33′10″W / 40.68056°N 121.55278°W
 | This volcanology article is a stub. You can help Wikipedia by expanding it. |
| This article relies largely or entirely on a
single source. (November 2023) |
The Tumble Buttes are a group of cinder cone volcanoes in the US state of California.
The Tumble Buttes are formed by three pyroclastic cinder cones: Bear Wallow Butte, Eiler Butte, and Hall Butte. They range in elevation from 6,391 feet (1,948 m) to 7,188 feet (2,191 m). [1] The volcanoes trend north-northwest to south-southeast along a fissure. Eiler Butte marks the northern end, while Bear Wallow Butte is the southernmost cone. [1]
The Tumble Buttes last erupted between 10,000 and 15,000 years ago, making them either Pleistocene or Holocene in age. The cinder cones have erupted lava flows. [1]
Bear Wallow Butte has unvegetated lava flows on both its eastern and western flanks; Eiler Butte has produced blocky lava. [1]
- ^ a b c d "Tumble Buttes". Global Volcanism Program. Smithsonian Institution. 2013. Retrieved November 21, 2023.
40°40′50″N 121°33′10″W / 40.68056°N 121.55278°W
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| This volcanology article is a stub. You can help Wikipedia by expanding it. |