#TITLE_ALTERNATIVE#

• Main Author: WELDY (nim : 12009078), LEONARDO
• Format: Final Project
• Language: Indonesia
• Online Access: https://digilib.itb.ac.id/gdl/view/28578
• Institution: Institut Teknologi Bandung

<p align="justify">This study is part of author's final assignment at Department of Geological Engineering Bandung Institute of Technology that aims to study the geology of <br /> <br /> <br /> <br /> Cisampih area. Research area is located in Cisampih area, Dawuan Subdistrict, Subang Regency, West Java Province with an area of 8 x 6,5 km2 with coordinates 790000 m - 798000 m and 9267500 m - 9274000 m ( UTM Zone 49 S) The geomorphology of the research area consists of three units, i.e. Ciherang Volcanic Hills Unit, Pancalikan Homocline Hills Unit and Cibodas Depositional Plain Unit The research area is within young to mature geomorphic stage. The stratigraphy of the research area divided into five unofficial litogical units. These units, from older to younger, are as follow: Claystone Unit which deposited <br /> <br /> <br /> <br /> during Late Miocene (zone N17) in Upper Bathyal environment, Claystone-Sandstone Unit which deposited during Late Miocene to early Pliocene (zone N18- N19) in Inner Neritic – Middle Neritic environment, Sandstone Unit which deposited during Late Pliocene (zone N20-N21) in inner Neritic environment, Pyroclastic Breccia Unit which deposited during Early Pleistocene, Lava Basalt Unit which <br /> <br /> <br /> <br /> deposited during Late Pleistosen and Alluvial Units which deposited during Recent in terrestrial environment. In the Late Pliocene to Pleistocene, this area was deforned and yielded geological structure as Cibodas Dextral Strike-Slip Fault.<p align="justify">