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<p align="justify">Mount Malabar is a type B volcano located in Bandung, West Java. This volcano is located around the geothermal working areas which have been in <br /> operation, those are Mount Wayang-Windu Field in the south and Mount Kamojang Field in the east. Mount M...

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Main Author: PRATAMA (NIM : 12011065), ADITYA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/25031
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:25031
spelling id-itb.:250312018-05-09T11:55:05Z#TITLE_ALTERNATIVE# PRATAMA (NIM : 12011065), ADITYA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/25031 <p align="justify">Mount Malabar is a type B volcano located in Bandung, West Java. This volcano is located around the geothermal working areas which have been in <br /> operation, those are Mount Wayang-Windu Field in the south and Mount Kamojang Field in the east. Mount Malabar is also upstream in South Bandung. <br /> However, some geological observations related to these potentials have not been conducted The area of study is located in the eastern part of Mount Malabar with total <br /> area of 78 km2. The aim of this study is to determine the geological conditions, geomorphology, geological structure, volcanostratigraphy, geological history, <br /> potential of natural resources, and geological hazards in the study area. <br /> This study was conducted in four stages: prelimination study, field observation, laboratory analysis and data processing, and report writing. Total of 140 outcrop data and 128 shear fracture data were processed to obtain geological map of the study area. <br /> Morphology of study area is dominated by morphology of ridges, valleys, slopes and plains with radial flow pattern and dendritic. The area of study was divided into 12 units of geomorphology and have young to old geomorphic stages. <br /> Observation to the topographic map scale of 1: 50,000 and 1: 100,000 showed that the area of study consists of three khuluks and five gumuks: Khuluk Baleendah, Khuluk Kendang, Khuluk Malabar, Gumuk Tikukur, Gumuk Kendang, Gumuk Malabar, Gumuk Citiis, and Gumuk Gambung. Meanwhile, the <br /> area of study consist of 18 units of rock. The primary and secondary structure found in area of study respectively are sheeting joints and horizontal faults: the sinistral Citiis fault, the sinistral Gambung faults, and dextral Gambung faults. <br /> The geological history of the study area was divided into six stages: The third phase of Mount Baleendah magmatism activity, Mount Kendang, Mount Malabar, Mount Gambung, tectonic activity with major NE-SW, also weathering and erosion that have been occured. <br /> The area of study has three potential of natural resources and geological hazard, those are potential of Mount Malabar as local recharge, potential of springs as clean water needs, potential of land using for agriculture and <br /> plantations, as well as the danger of landslides.<p align="justify"> text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description <p align="justify">Mount Malabar is a type B volcano located in Bandung, West Java. This volcano is located around the geothermal working areas which have been in <br /> operation, those are Mount Wayang-Windu Field in the south and Mount Kamojang Field in the east. Mount Malabar is also upstream in South Bandung. <br /> However, some geological observations related to these potentials have not been conducted The area of study is located in the eastern part of Mount Malabar with total <br /> area of 78 km2. The aim of this study is to determine the geological conditions, geomorphology, geological structure, volcanostratigraphy, geological history, <br /> potential of natural resources, and geological hazards in the study area. <br /> This study was conducted in four stages: prelimination study, field observation, laboratory analysis and data processing, and report writing. Total of 140 outcrop data and 128 shear fracture data were processed to obtain geological map of the study area. <br /> Morphology of study area is dominated by morphology of ridges, valleys, slopes and plains with radial flow pattern and dendritic. The area of study was divided into 12 units of geomorphology and have young to old geomorphic stages. <br /> Observation to the topographic map scale of 1: 50,000 and 1: 100,000 showed that the area of study consists of three khuluks and five gumuks: Khuluk Baleendah, Khuluk Kendang, Khuluk Malabar, Gumuk Tikukur, Gumuk Kendang, Gumuk Malabar, Gumuk Citiis, and Gumuk Gambung. Meanwhile, the <br /> area of study consist of 18 units of rock. The primary and secondary structure found in area of study respectively are sheeting joints and horizontal faults: the sinistral Citiis fault, the sinistral Gambung faults, and dextral Gambung faults. <br /> The geological history of the study area was divided into six stages: The third phase of Mount Baleendah magmatism activity, Mount Kendang, Mount Malabar, Mount Gambung, tectonic activity with major NE-SW, also weathering and erosion that have been occured. <br /> The area of study has three potential of natural resources and geological hazard, those are potential of Mount Malabar as local recharge, potential of springs as clean water needs, potential of land using for agriculture and <br /> plantations, as well as the danger of landslides.<p align="justify">
format Final Project
author PRATAMA (NIM : 12011065), ADITYA
spellingShingle PRATAMA (NIM : 12011065), ADITYA
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author_facet PRATAMA (NIM : 12011065), ADITYA
author_sort PRATAMA (NIM : 12011065), ADITYA
title #TITLE_ALTERNATIVE#
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url https://digilib.itb.ac.id/gdl/view/25031
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