dbo:abstract |
Mount Karifuri (狩振岳, Karifuri-dake) is a mountain in the Hidaka Mountains of Hokkaidō, Japan. The mountain sits on the border between Minamifurano and Shimukappu. It is 1,323.2 metres (4,341.2 ft) high. It is the source of the Mu River (Hokkaidō). Mount Karifuri is split between two different rock types. The western side consists of plutonic rock formed 40–32 million years ago. The eastern side is made of metamorphic rock formed under low-to-mid pressure 50–20 million years ago. (en) Le mont Karifuri (狩振岳, Karifuri-dake) est une montagne culminant à 1 323 m d'altitude dans les monts Hidaka en Hokkaidō au Japon. Le mont Karifuri se trouve à la limite des villages de Minamifurano et Shimukappu. La prend sa source dans la montagne. Le mont Karifuri est divisé entre deux différents types de roches. Le versant occidental est constitué de roche plutonique formée il y a 40-32 millions d'années. La versant oriental se compose de roche métamorphique formée sous pression faible il y a 50 à 20 millions d'années. (fr) |
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狩振岳 (en) |
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dbr:Fold_(geology) |
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dbr:Early_Miocene dbr:Middle_Eocene |
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dbp:name |
Mount Karifuri (en) |
dbp:otherName |
狩振岳 (en) |
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http://watchizu.gsi.go.jp/watchizu.aspx%3Fb=430035&l=1424340 |
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rdfs:comment |
Mount Karifuri (狩振岳, Karifuri-dake) is a mountain in the Hidaka Mountains of Hokkaidō, Japan. The mountain sits on the border between Minamifurano and Shimukappu. It is 1,323.2 metres (4,341.2 ft) high. It is the source of the Mu River (Hokkaidō). Mount Karifuri is split between two different rock types. The western side consists of plutonic rock formed 40–32 million years ago. The eastern side is made of metamorphic rock formed under low-to-mid pressure 50–20 million years ago. (en) Le mont Karifuri (狩振岳, Karifuri-dake) est une montagne culminant à 1 323 m d'altitude dans les monts Hidaka en Hokkaidō au Japon. Le mont Karifuri se trouve à la limite des villages de Minamifurano et Shimukappu. La prend sa source dans la montagne. Le mont Karifuri est divisé entre deux différents types de roches. Le versant occidental est constitué de roche plutonique formée il y a 40-32 millions d'années. La versant oriental se compose de roche métamorphique formée sous pression faible il y a 50 à 20 millions d'années. (fr) |
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Mont Karifuri (fr) Mount Karifuri (en) |
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