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単冠山

Hitokappu Volcano Group [Bogatyr Ridge]

成層火山 · Japan - administered by Russia · 1610m

Stokap (center) lies at the SW end of Nishihitokappuyama, an elongated chain of small volcanoes on southern Iturup Island. Nishihitokappuyama consists of a cluster of small NE-SW-trending late-Pleistocene to Holocene cones and craters. Stokap contains 8-10 cones and craters, the largest of which contains a lake. The flank of Etorofu-Atosanupuri is seen in the foreground.
Stokap (center) lies at the SW end of Nishihitokappuyama, an elongated chain of small volcanoes on southern Iturup Island. Nishihitokappuyama consists of a cluster of small NE-SW-trending late-Pleistocene to Holocene cones and craters. Stokap contains 8-10 cones and craters, the largest of which contains a lake. The flank of Etorofu-Atosanupuri is seen in the foreground. · 写真: Photo by Alexander Rybin, 2001 (Institute of Marine Geology and Geophysics, Yuzhno-Sakhalin). · Wikimedia Commons
タイプ
成層火山
Japan - administered by Russia
地域
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
標高
1610m
座標
44.857, 147.403
最終噴火
不明
テクトニクス環境
Subduction zone / Intermediate crust (15-25 km)
火山地形
Cluster
主要岩石
Andesite / Basaltic Andesite
地質学的概要

The Hitokappu Volcano Group [Bogatyr Ridge] on Iturup Island in the southern Kuriles consists of a cluster of late-Pleistocene to Holocene cones and craters extending ~14 km NE-SW. The basaltic andesite to andesitic Nishihitokappuyama (also known as Stokap) stratovolcano at the SW end of the ridge appears to be the location of the most recent eruptions, with a summit area that includes 8-10 cones and explosion craters, the largest of which contains a lake. The volcanic chain was constructed over a high Pleistocene base, whose glaciated surface is covered by lava flows from Nishihitokappuyama that reach to both the Pacific Ocean and the Sea of Okhotsk. JMA (2013) does not include this as a Holocene volcano.

Wikipedia の要約

要約が短いです。詳細は記事全文をご覧ください。

単冠山(ひとかっぷやま)は、は択捉島にある山の総称である。ロシア語ではБогатырь(ボガティル)。

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