Pengaruh Struktur Geologi Terhadap Potensi Geodiversitas Di Daerah Sungai Klawing, Kabupaten Purbalingga-Jawa Tengah
Abstract: The Klawing River is
located in Purbalingga Regency, in the central part of Central Java. The
headwater of the river is in northern area of Bobotsari and flows to Serayu
River as the main river. The Klawing and its tributaries cut Tertiary rocks in
the mountains of North Serayu, which includes Kumbang and Tapak Formation, and
Quaternary volcanic rocks of Slamet volcano. Morphology around the river is
formed of volcanic mountains in the west, the steep hills sloping folds in the
north and undulating plains at the east and south. Alluvial plain is produced
around the Klawing river. This sediment is form terraces morphology around the
main river. The main geological structures that develop in the research area is
a bedding plane or the slope of the rock layers. This structure produces a
typical potential distribution pattern of primary jasper at the igneous lava as
well as the andesite rock mine potential. Homocline hills ranks as an object of
geology is also controlled by geological structure. Geological structure of the
young rocks in the study area is a horizontal bedding plane. This structure
controls the distribution of sediment deposition in the secondary jasper at the
terrace steps around the river.
Penulis: Asmoro Widagdo, Budi
Brahmantyo
Kode Jurnal: jptindustridd140621
