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Geomorphologically, the area is divided into Sirnajaya Homoclinal Ridges, Bunijaya Homoclinal Ridges, and Terrace Plain of Cidadap River. Lithology of study area, divided into 4 units, i.e. Sandstone-Claystone, Sandstone, Tuffaceous Sandstone, and Breccias. All were sedimented in marine environment...

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Main Author: ERAS PUTRA (NIM 12005076), IQBAL
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13568
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13568
spelling id-itb.:135682017-09-27T11:46:44Z#TITLE_ALTERNATIVE# ERAS PUTRA (NIM 12005076), IQBAL Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13568 Geomorphologically, the area is divided into Sirnajaya Homoclinal Ridges, Bunijaya Homoclinal Ridges, and Terrace Plain of Cidadap River. Lithology of study area, divided into 4 units, i.e. Sandstone-Claystone, Sandstone, Tuffaceous Sandstone, and Breccias. All were sedimented in marine environment from volcanic sources at Middle to Late Miocene. Thrust fault of SW-NE direction was invoked this area. At least, there are 5 (five) significant landslides in this area. However, further analysis only taken from Cihurang’s landslide due to its huge influence to civilians. Wetness and slope angle was dominant cause of landslide based on sketch analysis, cross section and field <br /> <br /> <br /> <br /> investigations. 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 Geomorphologically, the area is divided into Sirnajaya Homoclinal Ridges, Bunijaya Homoclinal Ridges, and Terrace Plain of Cidadap River. Lithology of study area, divided into 4 units, i.e. Sandstone-Claystone, Sandstone, Tuffaceous Sandstone, and Breccias. All were sedimented in marine environment from volcanic sources at Middle to Late Miocene. Thrust fault of SW-NE direction was invoked this area. At least, there are 5 (five) significant landslides in this area. However, further analysis only taken from Cihurang’s landslide due to its huge influence to civilians. Wetness and slope angle was dominant cause of landslide based on sketch analysis, cross section and field <br /> <br /> <br /> <br /> investigations.
format Final Project
author ERAS PUTRA (NIM 12005076), IQBAL
spellingShingle ERAS PUTRA (NIM 12005076), IQBAL
#TITLE_ALTERNATIVE#
author_facet ERAS PUTRA (NIM 12005076), IQBAL
author_sort ERAS PUTRA (NIM 12005076), IQBAL
title #TITLE_ALTERNATIVE#
title_short #TITLE_ALTERNATIVE#
title_full #TITLE_ALTERNATIVE#
title_fullStr #TITLE_ALTERNATIVE#
title_full_unstemmed #TITLE_ALTERNATIVE#
title_sort #title_alternative#
url https://digilib.itb.ac.id/gdl/view/13568
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