Pyroclastic cone 1245 m / 4085 ft
Eastern Alaska, United States, 63.72°N / -141.63°WCurrent status
: (probably) extinct (0 out of 5) | ReportsPrindle volcano books
Typical eruption style
Prindle volcano eruptions
: None during the past 10,000 years
Less than few million years ago (Pleistocene)
No recent earthquakes
|Time||Mag. / Depth||Distance||Location|
Prindle volcano is a small isolated basaltic cinder cone and lava flow in an area of metamorphic and granitic terrain. The cone formed sometime between the early Pleistocene and the about 1900 years before present White River ash that overlies the lava flow; Foster (in Wood and Kienle 1990) considered Prindle to be of Pleistocene age.
---Source: Smithsonian / GVP volcano information
See also: Sentinel hub
| Landsat 8
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