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Geology and tsunami exposure of Pandeglang, Banten, Indonesia

As the study area is prone to geological hazard phenomena geological information of Pandeglang, Banten should be updated frequently with the latest data and findings. In geology world, geological map is very crucial to researchers as it contain various geological data such as stratigraphy, structure...

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Main Author: Wan Nur ‘Afifa Wan Mustapa
Format: Undergraduate Final Project Report
Language:English
Published: 2020
Online Access:http://discol.umk.edu.my/id/eprint/4385/1/Wan%20Nur%20%60Afifa%20Binti%20Wan%20Mustapa.pdf
http://discol.umk.edu.my/id/eprint/4385/
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spelling my.umk.eprints.43852022-05-23T22:39:28Z http://discol.umk.edu.my/id/eprint/4385/ Geology and tsunami exposure of Pandeglang, Banten, Indonesia Wan Nur ‘Afifa Wan Mustapa As the study area is prone to geological hazard phenomena geological information of Pandeglang, Banten should be updated frequently with the latest data and findings. In geology world, geological map is very crucial to researchers as it contain various geological data such as stratigraphy, structure, features and rock unit. The study area bounded by coordinate latitude of S 06°19'06.01" to S 06°21'48.60" and longitude of E 105°49'06.17" to E 105°51'48.70". This research aims to provide an updated geological map of research area with scale 1:25000 and to produce tsunami exposure map with complete classification of tsunami exposure in Pandeglang, Banten. In order to generate geological map, exposure map and other thematic maps geological mapping is conducted. During field studies, geological data such as geomorphology, lithology, tsunami exposure and others been collected along with sampling and traversing. From the analysis and interpretation made, the study area is primarily composed of two lithologies which are Upper Banten Tuff and Alluvium. Sandstone fragment that found at the river is believed belong to Bojongmanik Formation. Three different types of exposure zone due to recent tsunami are constructed. Secondary data shows run up distance and flow depth of the tsunami are 274 m and 390 m respectively. Pandeglang is prone area to tsunami and other geological phenomena due to its geological position. 2020 Undergraduate Final Project Report NonPeerReviewed text en http://discol.umk.edu.my/id/eprint/4385/1/Wan%20Nur%20%60Afifa%20Binti%20Wan%20Mustapa.pdf Wan Nur ‘Afifa Wan Mustapa (2020) Geology and tsunami exposure of Pandeglang, Banten, Indonesia. Final Year Project thesis, Universiti Malaysia Kelantan. (Submitted)
institution Universiti Malaysia Kelantan
building Perpustakaan Universiti Malaysia Kelantan
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Malaysia Kelantan
content_source UMK Institutional Repository
url_provider http://umkeprints.umk.edu.my/
language English
description As the study area is prone to geological hazard phenomena geological information of Pandeglang, Banten should be updated frequently with the latest data and findings. In geology world, geological map is very crucial to researchers as it contain various geological data such as stratigraphy, structure, features and rock unit. The study area bounded by coordinate latitude of S 06°19'06.01" to S 06°21'48.60" and longitude of E 105°49'06.17" to E 105°51'48.70". This research aims to provide an updated geological map of research area with scale 1:25000 and to produce tsunami exposure map with complete classification of tsunami exposure in Pandeglang, Banten. In order to generate geological map, exposure map and other thematic maps geological mapping is conducted. During field studies, geological data such as geomorphology, lithology, tsunami exposure and others been collected along with sampling and traversing. From the analysis and interpretation made, the study area is primarily composed of two lithologies which are Upper Banten Tuff and Alluvium. Sandstone fragment that found at the river is believed belong to Bojongmanik Formation. Three different types of exposure zone due to recent tsunami are constructed. Secondary data shows run up distance and flow depth of the tsunami are 274 m and 390 m respectively. Pandeglang is prone area to tsunami and other geological phenomena due to its geological position.
format Undergraduate Final Project Report
author Wan Nur ‘Afifa Wan Mustapa
spellingShingle Wan Nur ‘Afifa Wan Mustapa
Geology and tsunami exposure of Pandeglang, Banten, Indonesia
author_facet Wan Nur ‘Afifa Wan Mustapa
author_sort Wan Nur ‘Afifa Wan Mustapa
title Geology and tsunami exposure of Pandeglang, Banten, Indonesia
title_short Geology and tsunami exposure of Pandeglang, Banten, Indonesia
title_full Geology and tsunami exposure of Pandeglang, Banten, Indonesia
title_fullStr Geology and tsunami exposure of Pandeglang, Banten, Indonesia
title_full_unstemmed Geology and tsunami exposure of Pandeglang, Banten, Indonesia
title_sort geology and tsunami exposure of pandeglang, banten, indonesia
publishDate 2020
url http://discol.umk.edu.my/id/eprint/4385/1/Wan%20Nur%20%60Afifa%20Binti%20Wan%20Mustapa.pdf
http://discol.umk.edu.my/id/eprint/4385/
_version_ 1763303406827470848
score 13.211869

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