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Global Volcanism Program | Image GVP-10529

Snow mantles the western flanks of Omurayama scoria cone in the Izu-Tobu volcano group. Omuroyama formed about 5,000 years ago. The volcanic field formed over a broad, plateau-like area of more than 400 km2 on the E side of the Izu Peninsula. About 70 monogenetic volcanoes formed during the last 140,000 years, and chemically similar submarine cones are located offshore. Copyrighted photo by Akira Takada (Japanese Quaternary Volcanoes database, RIODB, http://riodb02.ibase.aist.go.jp/strata/VOL_JP/EN/index.htm and Geol Surv Japan, AIST, http://www.gsj.jp/).

Snow mantles the western flanks of Omurayama scoria cone in the Izu-Tobu volcano group. Omuroyama formed about 5,000 years ago. The volcanic field formed over a broad, plateau-like area of more than 400 km2 on the E side of the Izu Peninsula. About 70 monogenetic volcanoes formed during the last 140,000 years, and chemically similar submarine cones are located offshore.

Copyrighted photo by Akira Takada (Japanese Quaternary Volcanoes database, RIODB, http://riodb02.ibase.aist.go.jp/strata/VOL_JP/EN/index.htm and Geol Surv Japan, AIST, http://www.gsj.jp/).

Copyrighted image used with permission. All Rights Reserved. Contact photographer for any usage requests.

Keywords: scoria cone


Izu-Tobu