Kamen (volcano)
| Kamen | |
|---|---|
 Kamchatka volcanoes: Klyuchevskaya Sopka (top), Bezymianny (bottom), both in activity, and the Kamen (middle). | |
| Highest point | |
| Elevation | 4,585 m (15,043 ft) |
| Coordinates | 56°01′12″N 160°35′35″E / 56.02°N 160.593°E |
| Naming | |
| Native name | Камень (Russian) |
| English translation | Stone |
| Geography | |
  Kamen Location in Kamchatka Krai, Russia | |
| Location | Kamchatka, Russia |
| Parent range | Eastern Range |
| Geology | |
| Mountain type | Stratovolcano |
| Last eruption | Unknown |
Kamen (Russian: Камень, literally Stone) is a dormant stratovolcano located in the southern part of Kamchatka Peninsula, Russia, flanked by Bezymianny and Kluchevskaya. It is the second highest volcano of Kamchatka.
History
[edit]Kamen was formed over large lava plateaus in two different stages of eruptions. The first stage of eruptions was explosive and produced pyroclastic debris which mainly contained tuffs while the second stage aimed to be the opposite. This stage created lava flows which began the formation of dikes (often reaching up to 2 kilometers long and 5 meters thick) as magma moved down the volcano. These same eruption stages were also how Kamen's neighboring volcanos were formed.[1][2] As Kamen continued to age, so did the compositions within its lava. When the stratovolcano was first born, the lava it would often produce would contain mafic materials. However as Kamen grew older, it started to show a decline in these minerals.[1]
See also
[edit]References
[edit]
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- ^ a b Churikova, Tatiana G.; Gordeychik, Boris N.; Ivanov, Boris V.; Wörner, Gerhard (1 August 2013). "Relationship between Kamen Volcano and the Klyuchevskaya group of volcanoes (Kamchatka)". Journal of Volcanology and Geothermal Research. 263: 3–21. doi:10.1016/j.jvolgeores.2013.01.019.
- ^ T., Churikova; B., Gordeichik; B., Ivanov (2012). "Petrochemistry of Kamen volcano: A comparison with neighboring volcanoes of the Klyuchevskoy group". Journal of Volcanology & Seismology. 6 (3): 150–171. doi:10.1134/S0742046312030037.