Available Weekly Reports
| Schmidt |

No latest activity reported for #volcano.name#.
Below is a summary of eruption dates and Volcanic Explosivity Indices (VEI).
The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.
Andreev V I, Litasov N E, Puzankov Y M, 1988. Radioactivity of the basalt-dacite and andesite suites of the Gamchen volcanotectonic structure. {Vulc Seism}, 7: 219-233 (English translation)
Erlich E N, 1985. . (pers. comm.)
Luchitsky I V (ed), 1974. {History of the Development of Relief of Siberia and the Far East. Kamchatka, Kurile and Komander Islands}. Moscow: Nauka Pub, 439 p (in Russian)
Schmidt volcano is a large 2020-m-high mid- to upper-Pleistocene shield-like volcano located north of Kronotsky volcano and SW of Gamchen volcano (Lutchitsky, 1974). A dike complex is prominent on the eroded volcano, which was constructed along a NE-trending fault zone. Following the cessation of activity at Schmidt volcano during the Pleistocene, regional basaltic volcanism produced some monogenetic cinder cones that were erupted through the eastern and NE flanks of the volcano during the Holocene (Andreev et al., 1988).