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THE RELATIONSHIP OF GEOLOGICAL CONDITIONS BETWEEN THE NGARAI SIANOK - MANINJAU GEOPARK AND THE SILOKEK GEOPARK Faculty of Earth Sciences and Technology, Bandung Institute of Technology Jalan Ganesha 10, Bandung 40132, Indonesia Abstract Ngarai Sianok - Maninjau Geopark and Silokek Geopark are one of the national geoparks in West Sumatra Province, as it is known that this Sumatran fault extends from the Bay in Lampung to the northern part of Aceh, is a dextral slip fault and has undergone a 25-30 km. Formed as a result of the subduction of the Indo-Australian Plate which moves relative to the North under the Eurasian Plate, thus forming an oblique mechanism. One of the relationships between the Great Sumatran Fault is by looking at evidence from the geosites in the Sianok - Maninjau Geopark and the Silokek Geopark. What is visible is the formation of the Ngarai Sianok (Sianok Valley), which is the influence of a shear fault and creates a pull-apart basin negative flower structure, this section is part of the Sianok segment. Keywords: Ngarai Sianok, Maninjau, Silokek, Geopark, Great Sumatran Fault, UNESCO Topic: Solid Earth Sciences |
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