Columnar Joint of Mount Tungkat
Columnar Joint of Mount Tungkat With a diameter of ± 1 m, it is located on the bank of the
Nilo Sungsang Hotspring
Nilo Sungsang Hotspring In this geosite there is a geological phenomenon in the form of hotspring flowing out of the
Fumarol Grao Sakti
Fumarol Grao Sakti Geyser is that emit sulfur smoke as a result of geothermal boiling activity of the earth. The
Sungai Hitam Waterfall
Sungai Hitam Waterfall Period II eruption at 21,000 after the formation of the Masurai Caldera which partially
Serintik Hujan Panas Waterfall
Serintik Hujan Panas Waterfall This geosite has a morphological of hills because it is located on Mount Masurai,
Mukus Waterfall
Mukus Waterfall The morphology of this geosite is in the form of structural hills. The walls of the waterfall which
Lempisang Waterfall
Lempisang Waterfall The waterfall wall is an Ignimbrite resulting from the Masurai Caldera eruption 33,000 years
Sigerincing Waterfall
Sigerincing Waterfall This geosite is located on the Siau river, which is morphologically still included in the
Dukun Betuah Waterfall
Dukun Betuah Waterfall This geosite is still in the morphological stretch of the highlands. In this geosite there
Lake Telago Biru
Lake Telago Biru Small phreatic eruptions have occurred within and near the wall of Masurai Caldera. Its different
Lake Depati Empat
Lake Depati Empat This lake was formed due to tectonic activity which resulted in slight faults and straits. From
Kumbang and Mabuk Crater Lake Complex
Kumbang and Mabuk Crater Lake Complex The caldera has a diameter of 7 km, with the east side of the caldera wall
Lake Pauh
Lake Pauh As a result of volcanic activity, it is composed of volcanic tuff breccia rock units, which consist of
Tiangko Crystal Cave
Tiangko Crystal Cave The karst landscape forms this cave. In addition, it has a high pre-historic archaeological
Sengering Stream Sink Cave
Sengering Stream Sink Cave The karst landscape in the form of meta-limestone interspersed with limestone shale and
Sengayau Cave Complex
Sengayau Cave Complex The karst landscape in the form of meta-limestone interspersed with limestone shale and above
Granitoid Rock of Air Batu
Granitoid Rock of Air Batu Is aIs a rock unit that is generally eroded and faulted, and strongly weathered; broke
Conglomerate of Teluk Wang Formation
Conglomerate of Teluk Wang Formation This high cliff which is on the banks of the Merangin River in the form of a
Mengkarang Fossilized Brachiopods
Mengkarang Fossilized Brachiopods This black shale which contains tuffaceous fossils of marine origin such as
Muara Karing Leaf Fossil
Muara Karing Leaf Fossil The Karing River is a small river that connecting directly into the Merangin River, the
Teluk Gedang Wood Fossil
Teluk Gedang Wood Fossil In this geosite, we get the characteristics of Jambi flora fossils that are 290 to 300