Fig. 10From: “Volcanism in the Chugoku region: a review for the first UNESCO field school on Geoenvironmental disaster reduction”Late Miocene deposits of the Takashibiyama formation at Cape Kukedo, central Shimane Peninsula, showing a cross section through the pyroclastic successions of a submarine seamount. A steeply dipping dike is crosscutting the volcaniclastic unitsBack to article page