Dukun Betuah Waterfall

Dukun Betuah Waterfall

This geosite is still in the morphological stretch of the highlands. In this geosite there are rocks resulting from the eruption of the Pre-Masurai Caldera in the form of basalt scoria commonly found around this location, then followed by a layer of sandy tuff, and andesite-basalt lava deposits that form sheet joints. The formation of these sheet joints is the result of the phase of tectonic activity in this area.

Location