Geomorphologycal Study for Flood and Mass Movement Occurrence at Parang Sub Village, Paranggupito District, Wonogiri Regency

The aim of this study are knowing factors that impacts to flood and mass movement hazard at karst region. Area of this study are covering Parang Sub Village, Ngasem, Paranggupito District, Wonogiri Regency. To achieve this objective, geomorphic approaches (static, as well as dynamic environmental ge...

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Main Author: Muhammad Amin Sunarhadi
Format: Article
Language:English
Published: Muhammadiyah University Press 2016-07-01
Series:Forum Geografi
Subjects:
Online Access:http://journals.ums.ac.id/index.php/fg/article/view/4656
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spelling doaj-cf80ce0f165848ed82a6745aeda253d32020-11-24T21:06:37ZengMuhammadiyah University PressForum Geografi0852-06822460-39452016-07-011511910.23917/forgeo.v15i1.46563264Geomorphologycal Study for Flood and Mass Movement Occurrence at Parang Sub Village, Paranggupito District, Wonogiri RegencyMuhammad Amin Sunarhadi0Universitas Muhammadiyah SurakartaThe aim of this study are knowing factors that impacts to flood and mass movement hazard at karst region. Area of this study are covering Parang Sub Village, Ngasem, Paranggupito District, Wonogiri Regency. To achieve this objective, geomorphic approaches (static, as well as dynamic environmental geomorphology) were analyzed, using survey and secondary data collection. Results from this study are describe that Parang is a karst depression and had water accumulated from Parang boundaries area as upper landform. Mass movement at study area is caused by saturation of soil by water after rainfall. Supported by steep slope impact sliding mass movement. Based on the priority, to change the water running direction and will not concentrate to Parang Depresion, there are need the water-massbank stability. This bank will prevent the soil mass to stable.http://journals.ums.ac.id/index.php/fg/article/view/4656karst geomorphologyfloodmass movement
collection DOAJ
language English
format Article
sources DOAJ
author Muhammad Amin Sunarhadi
spellingShingle Muhammad Amin Sunarhadi
Geomorphologycal Study for Flood and Mass Movement Occurrence at Parang Sub Village, Paranggupito District, Wonogiri Regency
Forum Geografi
karst geomorphology
flood
mass movement
author_facet Muhammad Amin Sunarhadi
author_sort Muhammad Amin Sunarhadi
title Geomorphologycal Study for Flood and Mass Movement Occurrence at Parang Sub Village, Paranggupito District, Wonogiri Regency
title_short Geomorphologycal Study for Flood and Mass Movement Occurrence at Parang Sub Village, Paranggupito District, Wonogiri Regency
title_full Geomorphologycal Study for Flood and Mass Movement Occurrence at Parang Sub Village, Paranggupito District, Wonogiri Regency
title_fullStr Geomorphologycal Study for Flood and Mass Movement Occurrence at Parang Sub Village, Paranggupito District, Wonogiri Regency
title_full_unstemmed Geomorphologycal Study for Flood and Mass Movement Occurrence at Parang Sub Village, Paranggupito District, Wonogiri Regency
title_sort geomorphologycal study for flood and mass movement occurrence at parang sub village, paranggupito district, wonogiri regency
publisher Muhammadiyah University Press
series Forum Geografi
issn 0852-0682
2460-3945
publishDate 2016-07-01
description The aim of this study are knowing factors that impacts to flood and mass movement hazard at karst region. Area of this study are covering Parang Sub Village, Ngasem, Paranggupito District, Wonogiri Regency. To achieve this objective, geomorphic approaches (static, as well as dynamic environmental geomorphology) were analyzed, using survey and secondary data collection. Results from this study are describe that Parang is a karst depression and had water accumulated from Parang boundaries area as upper landform. Mass movement at study area is caused by saturation of soil by water after rainfall. Supported by steep slope impact sliding mass movement. Based on the priority, to change the water running direction and will not concentrate to Parang Depresion, there are need the water-massbank stability. This bank will prevent the soil mass to stable.
topic karst geomorphology
flood
mass movement
url http://journals.ums.ac.id/index.php/fg/article/view/4656
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