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...
Main Author: | |
---|---|
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 |
id |
doaj-cf80ce0f165848ed82a6745aeda253d3 |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT muhammadaminsunarhadi geomorphologycalstudyforfloodandmassmovementoccurrenceatparangsubvillageparanggupitodistrictwonogiriregency |
_version_ |
1716765199557459968 |