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The geomorphologic unit of the study area is divided into 4 units, those are Hogback Ridge Unit, Cuesta Ridge Unit, Sinclinal Valley Unit, and Alluvial plain Unit. Based on the characteristic of meandering river with U-shaped lley, the study area is counted to old geomorphic phase with trellis patte...

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Main Author: RENGGANIS (NIM 12005064), HANNA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13512
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13512
spelling id-itb.:135122017-09-27T11:46:45Z#TITLE_ALTERNATIVE# RENGGANIS (NIM 12005064), HANNA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13512 The geomorphologic unit of the study area is divided into 4 units, those are Hogback Ridge Unit, Cuesta Ridge Unit, Sinclinal Valley Unit, and Alluvial plain Unit. Based on the characteristic of meandering river with U-shaped lley, the study area is counted to old geomorphic phase with trellis pattern. Four major stratigraphic units can be recognized which deposited since Middle Miocene up to Early Pliocene. Those are from the old to the young: Mudstone-Sandstone unit of Halang Formation, Sandstone-Mudstone unit of Halang Formation, Volcanic Breccia unit of Kumbang Formation, and Aluviall Plain. Geological structure which had developed in the study area is mainly controlled by NW-SE trending thrust fault. Tear faults were also found with relatively NESW trend as the fault orientation. 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 The geomorphologic unit of the study area is divided into 4 units, those are Hogback Ridge Unit, Cuesta Ridge Unit, Sinclinal Valley Unit, and Alluvial plain Unit. Based on the characteristic of meandering river with U-shaped lley, the study area is counted to old geomorphic phase with trellis pattern. Four major stratigraphic units can be recognized which deposited since Middle Miocene up to Early Pliocene. Those are from the old to the young: Mudstone-Sandstone unit of Halang Formation, Sandstone-Mudstone unit of Halang Formation, Volcanic Breccia unit of Kumbang Formation, and Aluviall Plain. Geological structure which had developed in the study area is mainly controlled by NW-SE trending thrust fault. Tear faults were also found with relatively NESW trend as the fault orientation.
format Final Project
author RENGGANIS (NIM 12005064), HANNA
spellingShingle RENGGANIS (NIM 12005064), HANNA
#TITLE_ALTERNATIVE#
author_facet RENGGANIS (NIM 12005064), HANNA
author_sort RENGGANIS (NIM 12005064), HANNA
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/13512
_version_ 1820736208570941440

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