Serintik Hujan Panas Waterfall

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Serintik Hujan Panas Waterfall

This geosite has a morphological of hills because it is located on Mount Masurai, the Tenok River flows with a base in the form of volcanic and lava breccia. This waterfall, which is composed of Andesite-basalt, is the result of tectonic activity that causes faults and forms columnar joints, and is followed by a landslide process in the body of the breccia rock to form river humps.

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