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The cape mostly comprises tuff breccia. The top layer is covered with andesitic lava from the Pliocene Epoch. Around the cape you'll see various formations eroded by the sea and amazing rhyolite dikes.
[Access] Approx. 35 min. walk from Higashihama Station on the JR San'in Main Line
This basic information is current at the time of publication and is subject to change.
Please check the official website for the latest information.