PEMETAAN BAHAYA LONGSOR DENGAN METODE ANALITYCAL HIERARCHY PROCESS DI GUNUNG ARJUNO WELIRANG, JAWA TIMUR

Indonesia has enormous geothermal potential because most of Indonesia's territory is located in an active volcano route. One of the challenges in developing geothermal energy is that its location is located on the slopes of a Quaternary Volcanoes which is suceptible to landslides. The purpose o...

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Main Authors: Arief Rachmansyah, Ardian Baroto, Ika Meisy Putri Rahmawati
Format: Article
Language:English
Published: University of Brawijaya 2021-02-01
Series:Rekayasa Sipil
Subjects:
Online Access:https://rekayasasipil.ub.ac.id/index.php/rs/article/view/846
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spelling doaj-e6935a1eb4c84b73a92519f1fbe90cca2021-05-21T08:02:20ZengUniversity of BrawijayaRekayasa Sipil1978-56582502-63482021-02-01151697710.21776/ub.rekayasasipil.2021.015.01.10463PEMETAAN BAHAYA LONGSOR DENGAN METODE ANALITYCAL HIERARCHY PROCESS DI GUNUNG ARJUNO WELIRANG, JAWA TIMURArief Rachmansyah0Ardian BarotoIka Meisy Putri RahmawatiJurusan Teknik Sipil Fakultas Tekik Universitas BrawijayaIndonesia has enormous geothermal potential because most of Indonesia's territory is located in an active volcano route. One of the challenges in developing geothermal energy is that its location is located on the slopes of a Quaternary Volcanoes which is suceptible to landslides. The purpose of the research that has been carried out is to determine the distribution of landslide-hazard areas on the western slopes of the Arjuno-Welerang Volcano. The analysis was performed using the Analytical Hierarchy Process method based on morphological, geological and structural geological parameters. Geomorphological mapping was carried out by contour map analysis, then classified based on morphometry and morphogenesis. Geological mapping uses the principle of volcanostratigraphy, while mapping of geological structures is done by analyzing contour maps made by Digital Evalation Model and field checking. The high and very high landslide hazard zones are scattered along the fault zone, while the very high landslide hazard areas are located in the ancient crater valleyshttps://rekayasasipil.ub.ac.id/index.php/rs/article/view/846landslide hazardvolcanostratigraphyianalitycal hierarchy process
collection DOAJ
language English
format Article
sources DOAJ
author Arief Rachmansyah
Ardian Baroto
Ika Meisy Putri Rahmawati
spellingShingle Arief Rachmansyah
Ardian Baroto
Ika Meisy Putri Rahmawati
PEMETAAN BAHAYA LONGSOR DENGAN METODE ANALITYCAL HIERARCHY PROCESS DI GUNUNG ARJUNO WELIRANG, JAWA TIMUR
Rekayasa Sipil
landslide hazard
volcanostratigraphyi
analitycal hierarchy process
author_facet Arief Rachmansyah
Ardian Baroto
Ika Meisy Putri Rahmawati
author_sort Arief Rachmansyah
title PEMETAAN BAHAYA LONGSOR DENGAN METODE ANALITYCAL HIERARCHY PROCESS DI GUNUNG ARJUNO WELIRANG, JAWA TIMUR
title_short PEMETAAN BAHAYA LONGSOR DENGAN METODE ANALITYCAL HIERARCHY PROCESS DI GUNUNG ARJUNO WELIRANG, JAWA TIMUR
title_full PEMETAAN BAHAYA LONGSOR DENGAN METODE ANALITYCAL HIERARCHY PROCESS DI GUNUNG ARJUNO WELIRANG, JAWA TIMUR
title_fullStr PEMETAAN BAHAYA LONGSOR DENGAN METODE ANALITYCAL HIERARCHY PROCESS DI GUNUNG ARJUNO WELIRANG, JAWA TIMUR
title_full_unstemmed PEMETAAN BAHAYA LONGSOR DENGAN METODE ANALITYCAL HIERARCHY PROCESS DI GUNUNG ARJUNO WELIRANG, JAWA TIMUR
title_sort pemetaan bahaya longsor dengan metode analitycal hierarchy process di gunung arjuno welirang, jawa timur
publisher University of Brawijaya
series Rekayasa Sipil
issn 1978-5658
2502-6348
publishDate 2021-02-01
description Indonesia has enormous geothermal potential because most of Indonesia's territory is located in an active volcano route. One of the challenges in developing geothermal energy is that its location is located on the slopes of a Quaternary Volcanoes which is suceptible to landslides. The purpose of the research that has been carried out is to determine the distribution of landslide-hazard areas on the western slopes of the Arjuno-Welerang Volcano. The analysis was performed using the Analytical Hierarchy Process method based on morphological, geological and structural geological parameters. Geomorphological mapping was carried out by contour map analysis, then classified based on morphometry and morphogenesis. Geological mapping uses the principle of volcanostratigraphy, while mapping of geological structures is done by analyzing contour maps made by Digital Evalation Model and field checking. The high and very high landslide hazard zones are scattered along the fault zone, while the very high landslide hazard areas are located in the ancient crater valleys
topic landslide hazard
volcanostratigraphyi
analitycal hierarchy process
url https://rekayasasipil.ub.ac.id/index.php/rs/article/view/846
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