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Karangkemiri Village Landslide Potential Risk Mapping Based on Integrating Litho-structure and Morphology

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@article{IJASEIT12189,
   author = {FX Anjar Tri Laksono and Muhammad Rifki Fauzan and Asmoro Widagdo and János Kovács},
   title = {Karangkemiri Village Landslide Potential Risk Mapping Based on Integrating Litho-structure and Morphology},
   journal = {International Journal on Advanced Science, Engineering and Information Technology},
   volume = {12},
   number = {2},
   year = {2022},
   pages = {681--689},
   keywords = {Susceptibility; litho-structure; landslide, Karangkemiri; Cilacap.},
   abstract = {The Karangkemiri Village, Jeruklegi District, Cilacap Regency, Central Java Province, has a high risk of rock-mass movement. This is proven by the occurrence of a landslide in March 2020. The susceptibility of landslides is influenced by eight factors: slope, lithology, land cover, elevation, loading, rainfall, distance from rivers, and roads. Therefore, a landslide potential risk map is needed as a disaster mitigation effort. The integration between litho-structure and morphology was applied to understand the distribution of landslides vulnerability in Karangkemiri Village. The Analytical Hierarchy Process (AHP) method was adopted to find the dominant factor that causes a landslide. The result of this study was the geology of a research area consisting of 3 geomorphological units, namely the Structural Curve Slab Hills Unit (S3), Structural Waveed Hills Unit (S2), and Intrusion Unit to Basalt (S11). Stratigraphy of research areas is composed of sandstone (Tmph) and andesite lava (Tmpk) units. Special study methods use the AHP, assessment, and weighting against the landslide movement's causative factors, such calculations combined with primary and secondary data. The data and calculations were inserted into the parameter map then combined to obtain a map of the rock-mass movement susceptibility zone. Analyzing results show research areas divided into two levels of rock-mass movement vulnerability, medium, and high vulnerability levels. Medium levels of vulnerability cover 60% of Karangkemiri Village. Meanwhile, a high level of vulnerability encompasses 40% of Karangkemiri Village.},
   issn = {2088-5334},
   publisher = {INSIGHT - Indonesian Society for Knowledge and Human Development},
   url = {http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=12189},
   doi = {10.18517/ijaseit.12.2.12189}
}

EndNote

%A Laksono, FX Anjar Tri
%A Fauzan, Muhammad Rifki
%A Widagdo, Asmoro
%A Kovács, János
%D 2022
%T Karangkemiri Village Landslide Potential Risk Mapping Based on Integrating Litho-structure and Morphology
%B 2022
%9 Susceptibility; litho-structure; landslide, Karangkemiri; Cilacap.
%! Karangkemiri Village Landslide Potential Risk Mapping Based on Integrating Litho-structure and Morphology
%K Susceptibility; litho-structure; landslide, Karangkemiri; Cilacap.
%X The Karangkemiri Village, Jeruklegi District, Cilacap Regency, Central Java Province, has a high risk of rock-mass movement. This is proven by the occurrence of a landslide in March 2020. The susceptibility of landslides is influenced by eight factors: slope, lithology, land cover, elevation, loading, rainfall, distance from rivers, and roads. Therefore, a landslide potential risk map is needed as a disaster mitigation effort. The integration between litho-structure and morphology was applied to understand the distribution of landslides vulnerability in Karangkemiri Village. The Analytical Hierarchy Process (AHP) method was adopted to find the dominant factor that causes a landslide. The result of this study was the geology of a research area consisting of 3 geomorphological units, namely the Structural Curve Slab Hills Unit (S3), Structural Waveed Hills Unit (S2), and Intrusion Unit to Basalt (S11). Stratigraphy of research areas is composed of sandstone (Tmph) and andesite lava (Tmpk) units. Special study methods use the AHP, assessment, and weighting against the landslide movement's causative factors, such calculations combined with primary and secondary data. The data and calculations were inserted into the parameter map then combined to obtain a map of the rock-mass movement susceptibility zone. Analyzing results show research areas divided into two levels of rock-mass movement vulnerability, medium, and high vulnerability levels. Medium levels of vulnerability cover 60% of Karangkemiri Village. Meanwhile, a high level of vulnerability encompasses 40% of Karangkemiri Village.
%U http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=12189
%R doi:10.18517/ijaseit.12.2.12189
%J International Journal on Advanced Science, Engineering and Information Technology
%V 12
%N 2
%@ 2088-5334

IEEE

FX Anjar Tri Laksono,Muhammad Rifki Fauzan,Asmoro Widagdo and János Kovács,"Karangkemiri Village Landslide Potential Risk Mapping Based on Integrating Litho-structure and Morphology," International Journal on Advanced Science, Engineering and Information Technology, vol. 12, no. 2, pp. 681-689, 2022. [Online]. Available: http://dx.doi.org/10.18517/ijaseit.12.2.12189.

RefMan/ProCite (RIS)

TY  - JOUR
AU  - Laksono, FX Anjar Tri
AU  - Fauzan, Muhammad Rifki
AU  - Widagdo, Asmoro
AU  - Kovács, János
PY  - 2022
TI  - Karangkemiri Village Landslide Potential Risk Mapping Based on Integrating Litho-structure and Morphology
JF  - International Journal on Advanced Science, Engineering and Information Technology; Vol. 12 (2022) No. 2
Y2  - 2022
SP  - 681
EP  - 689
SN  - 2088-5334
PB  - INSIGHT - Indonesian Society for Knowledge and Human Development
KW  - Susceptibility; litho-structure; landslide, Karangkemiri; Cilacap.
N2  - The Karangkemiri Village, Jeruklegi District, Cilacap Regency, Central Java Province, has a high risk of rock-mass movement. This is proven by the occurrence of a landslide in March 2020. The susceptibility of landslides is influenced by eight factors: slope, lithology, land cover, elevation, loading, rainfall, distance from rivers, and roads. Therefore, a landslide potential risk map is needed as a disaster mitigation effort. The integration between litho-structure and morphology was applied to understand the distribution of landslides vulnerability in Karangkemiri Village. The Analytical Hierarchy Process (AHP) method was adopted to find the dominant factor that causes a landslide. The result of this study was the geology of a research area consisting of 3 geomorphological units, namely the Structural Curve Slab Hills Unit (S3), Structural Waveed Hills Unit (S2), and Intrusion Unit to Basalt (S11). Stratigraphy of research areas is composed of sandstone (Tmph) and andesite lava (Tmpk) units. Special study methods use the AHP, assessment, and weighting against the landslide movement's causative factors, such calculations combined with primary and secondary data. The data and calculations were inserted into the parameter map then combined to obtain a map of the rock-mass movement susceptibility zone. Analyzing results show research areas divided into two levels of rock-mass movement vulnerability, medium, and high vulnerability levels. Medium levels of vulnerability cover 60% of Karangkemiri Village. Meanwhile, a high level of vulnerability encompasses 40% of Karangkemiri Village.
UR  - http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=12189
DO  - 10.18517/ijaseit.12.2.12189

RefWorks

RT Journal Article
ID 12189
A1 Laksono, FX Anjar Tri
A1 Fauzan, Muhammad Rifki
A1 Widagdo, Asmoro
A1 Kovács, János
T1 Karangkemiri Village Landslide Potential Risk Mapping Based on Integrating Litho-structure and Morphology
JF International Journal on Advanced Science, Engineering and Information Technology
VO 12
IS 2
YR 2022
SP 681
OP 689
SN 2088-5334
PB INSIGHT - Indonesian Society for Knowledge and Human Development
K1 Susceptibility; litho-structure; landslide, Karangkemiri; Cilacap.
AB The Karangkemiri Village, Jeruklegi District, Cilacap Regency, Central Java Province, has a high risk of rock-mass movement. This is proven by the occurrence of a landslide in March 2020. The susceptibility of landslides is influenced by eight factors: slope, lithology, land cover, elevation, loading, rainfall, distance from rivers, and roads. Therefore, a landslide potential risk map is needed as a disaster mitigation effort. The integration between litho-structure and morphology was applied to understand the distribution of landslides vulnerability in Karangkemiri Village. The Analytical Hierarchy Process (AHP) method was adopted to find the dominant factor that causes a landslide. The result of this study was the geology of a research area consisting of 3 geomorphological units, namely the Structural Curve Slab Hills Unit (S3), Structural Waveed Hills Unit (S2), and Intrusion Unit to Basalt (S11). Stratigraphy of research areas is composed of sandstone (Tmph) and andesite lava (Tmpk) units. Special study methods use the AHP, assessment, and weighting against the landslide movement's causative factors, such calculations combined with primary and secondary data. The data and calculations were inserted into the parameter map then combined to obtain a map of the rock-mass movement susceptibility zone. Analyzing results show research areas divided into two levels of rock-mass movement vulnerability, medium, and high vulnerability levels. Medium levels of vulnerability cover 60% of Karangkemiri Village. Meanwhile, a high level of vulnerability encompasses 40% of Karangkemiri Village.
LK http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=12189
DO  - 10.18517/ijaseit.12.2.12189