#TITLE_ALTERNATIVE#

• Main Author: REZA RAMDHAN (NIM : 120 11 040), MUHAMMAD
• Format: Final Project
• Language: Indonesia
• Online Access: https://digilib.itb.ac.id/gdl/view/29316
• Institution: Institut Teknologi Bandung

<p align="justify">Mountain Malabar is B-type stratovolcano that situated at Bandung District, West <br /> Java. The aim of this study is to obtain the geologic setting and volcanostratigraphic of the northern Malabar within area of 81 km2 in 783000-792000 E and 9210000 – <br /> 9219000 S Zone 48S datum WGS 84. Methods used in this study are based on ALOS PALSAR imagery interpretation <br /> and field mapping, PALSAR (Phased Array L-Band Synthetic Aperture Radar) is active remote sensing technology which operates regardless time and weather condition, this sensors used microwave L-Band that has advantage to penetrate thick vegetation that could be reduced the acquisition of geological information in the surface. <br /> Mt. Malabar is classified into stratovolcano landform which reflected young geomorphic stage, the research area is divided into eight geomorphological unit namely Mekar Jaya Lava Dome Unit, Malabar Caldera Unit, Citiis Eruption Crater Unit, Malabar Volcanic Cone Unit, Cimaung Pyroclastic Fan Unit, Mangun Jaya Pyroclastic Slope Unit, Citiis Laharik Breccia Fan Unit, and Malabar Volcanic <br /> Plateau Unit. Stratigraphy of the research area is included to Khuluk Malabar which divided into three Gumuk namely Gumuk Malabar that consist of Malabar Andesit Lava Unit 1 (Mal1), Malabar Pyroclastic Flow Breccia Unit 1 (Map1), Malabar Pyroclastic Flow Breccia Unit 2 (Map2), Malabar Andesit Lava Unit 2 (Mal2), Malabar Andesit Lava Unit 3 (Mal3), Malabar Pyroclastic Flow Breccia Unit 3 <br /> (Map3), Malabar Andesit Lava Unit 4 (Mal4), Malabar Pyroclastic Fall Breccia Unit (Mpj). Gumuk Citiis consist of Citiis Andesit Lava Unit 1 (Cal1), Citiis Pyroclastic Flow Breccia Unit 1 (Cap1), and Citiis Laharic Breccia Unit (Clh). <br /> Gumuk Haruman consist of Haruman Andesit Lava Unit 1 (Hal1), Haruman Pyroclastic Flow Breccia Unit (Hap), and Haruman Andesit Lava Unit 2 (Hal2). Structural Geology of the research area consists of sheeting joint as primary <br /> structures and Cigereuh Dextral Fault and Citiis Sinistral Fault as secondary structures. <br /> Geological history of Mt. Malabar started with pre caldera stage at Pleistocene, followed by caldera formation that produced Gumuk Malabar, and post caldera stage that produced Gumuk Citiis and Gumuk Haruman, the last stage is <br /> compression event controlled by north-south direction main stress that caused the formation of secondary structure of the Mt. Malabar.<p align="justify">