Addington volcanic field
| Addington volcanic field | |
|---|---|
  Addington volcanic field Location within Alaska | |
 | |
| Highest point | |
| Elevation | −70 m (−230 ft)[1] |
| Coordinates | 55°26′N 134°10′W / 55.44°N 134.17°W[1] |
The Addington volcanic field is a submerged volcanic field in the U.S. state of Alaska, located about 20 km (12 mi) offshore of Cape Addington on Prince of Wales Island in the Alexander Archipelago. It is southwest of Iphigenia Bay and may have been the source of Late Pleistocene pyroclastic fall distributed throughout the Alaskan Panhandle. The Addington volcanic field is not known to have been volcanically active since the Pleistocene.[1]
See also
[edit]References
[edit]
 | This volcanology article is a stub. You can help Wikipedia by adding missing information. |
 | This Alaska location article is a stub. You can help Wikipedia by adding missing information. |