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Global Volcanism Program | Image GVP-10556

Maruyama cone is the low-angle peak at the left and Odokoyama on the right in this offshore view of Oki-Dogo Island. The Oki-Dogo Islands, north of the SW Honshu city of Matsue, are largely Pleistocene in age. The Daimanjisan lava flow on Oki-Dogo overlies alluvial gravel containing an ancient water jar, and the name Takuhiyama ("Burning Mountain") may reflect an oral record of an eruption. Copyrighted photo by Tadahide Ui (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/).

Maruyama cone is the low-angle peak at the left and Odokoyama on the right in this offshore view of Oki-Dogo Island. The Oki-Dogo Islands, north of the SW Honshu city of Matsue, are largely Pleistocene in age. The Daimanjisan lava flow on Oki-Dogo overlies alluvial gravel containing an ancient water jar, and the name Takuhiyama ("Burning Mountain") may reflect an oral record of an eruption.

Copyrighted photo by Tadahide Ui (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.


Oki-Dogo