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Investor Presentaiton

CONCLUSIONS • The Menoreh Hills are a dome-shaped physiographic zone, stratigraphy from the oldest to the youngest is Nanggulan Formations, Kaligesing-Dukuh Formation, Jonggrangan Formation, Sentolo Formation, and Quaternary Deposits. • Because the morphology and topography generally display steep to very steep slopes, composed of rocks with quite high weathering rates, controlled by geological structures in the form of joints and faults, and added by high average rainfall, then the area is prone to landslides. CONFERENCE ON EARTH The most common type of mass movement in the Menoreh Hills is landslide. The specific characteristics of landslide in the study area are generally showing the sliding plane which is not an ideal circular shape, but is a plane that is the boundary between soil and fresh rock, or combinati of circular plane and boundary between soil and fresh rocks. Yogyakarta, 3 October 2019 INTERNAL SCIENCE, ICEMINE 2019 MINERAL AND ENERGY 6
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