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It is a pyroclastic dike formed by invading magma into the Muro accretionary prism that forms the basis of the Kii Peninsula. You can observe how the magma has entered the cracks of the stratum in a mesh pattern, and the rocks (xenoliths) in which the surrounding strata have been incorporated into the magma. Hot springs from Susami Town to Shirahama Town are distributed along this dike.
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