ANALISIS SPASIAL DAERAH POTENSI RAWAN LONGSOR DI KOTA AMBON DENGAN MENGGUNAKAN METODE SMORPH
The geographical condition of Ambon City, which is 75% a hilly area resulted in most communities building in marbled areas with slopes above 20%, which has the potential to threaten life and landslide disasters. This study simply looked at the influence of slopes and slope shapes in Ambon City that...
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Language: | English |
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Universitas Brawijaya
2022-06-01
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Series: | JTSL (Jurnal Tanah dan Sumberdaya Lahan) |
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Online Access: | https://jtsl.ub.ac.id/index.php/jtsl/article/view/773 |
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author | Heinrich Rakuasa S Supriatna Mangapul Parlindungan Tambunan Melianus Salakory Wiclif. S. Pinoa |
author_facet | Heinrich Rakuasa S Supriatna Mangapul Parlindungan Tambunan Melianus Salakory Wiclif. S. Pinoa |
author_sort | Heinrich Rakuasa |
collection | DOAJ |
description |
The geographical condition of Ambon City, which is 75% a hilly area resulted in most communities building in marbled areas with slopes above 20%, which has the potential to threaten life and landslide disasters. This study simply looked at the influence of slopes and slope shapes in Ambon City that can be analyzed using geographic information systems (GIS) to map areas that have the potential for landslides. Identification and mapping of potential landslide areas have an important role as an effort in overcoming and anticipating the occurrence of landslide disasters. This study aimed to analyze the spread of potential landslide areas in Ambon City based on the results of SMORPH modeling. The study used the slope morphology or SMORPH method, which has a better degree of accuracy than the Storie Index and SINMAP methods to identify and classify potential landslide areas based on the matrix between slope shape and slope angle. This study resulted in 4 levels of landslide potential areas, namely very low, low, medium and high potential. Areas with high landslide potential dominate the northern and southern parts of Ambon City. In the region, most landslides occur in the form of sunken and convex slopes. The region has a hilly and mountainous topography with a steep slope. The results of this research using the SMORPH method can illustrate that the slope of the increasingly higher slope accompanied by the shape of a convex or concave slope will cause the potential for landslides that are higher in the region.
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first_indexed | 2024-03-08T04:06:05Z |
format | Article |
id | doaj.art-e326b3d0b6574184bd9022734fe6fa06 |
institution | Directory Open Access Journal |
issn | 2549-9793 |
language | English |
last_indexed | 2024-03-08T04:06:05Z |
publishDate | 2022-06-01 |
publisher | Universitas Brawijaya |
record_format | Article |
series | JTSL (Jurnal Tanah dan Sumberdaya Lahan) |
spelling | doaj.art-e326b3d0b6574184bd9022734fe6fa062024-02-09T05:36:38ZengUniversitas BrawijayaJTSL (Jurnal Tanah dan Sumberdaya Lahan)2549-97932022-06-019210.21776/ub.jtsl.2022.009.2.2ANALISIS SPASIAL DAERAH POTENSI RAWAN LONGSOR DI KOTA AMBON DENGAN MENGGUNAKAN METODE SMORPHHeinrich Rakuasa0S Supriatna1Mangapul Parlindungan Tambunan2Melianus Salakory3Wiclif. S. Pinoa4Departemen Geografi FMIPA Universitas IndonesiaDepartemen Geografi, Fakultas Matematika dan Ilmu Pengetahuan Alam, Universitas IndonesiaDepartemen Geografi, Fakultas Matematika dan Ilmu Pengetahuan Alam, Universitas IndonesiaProgram Studi Pendidikan Geografi, FKIP, Universitas PattimuraProgram Studi Pendidikan Geografi, FKIP, Universitas Pattimura The geographical condition of Ambon City, which is 75% a hilly area resulted in most communities building in marbled areas with slopes above 20%, which has the potential to threaten life and landslide disasters. This study simply looked at the influence of slopes and slope shapes in Ambon City that can be analyzed using geographic information systems (GIS) to map areas that have the potential for landslides. Identification and mapping of potential landslide areas have an important role as an effort in overcoming and anticipating the occurrence of landslide disasters. This study aimed to analyze the spread of potential landslide areas in Ambon City based on the results of SMORPH modeling. The study used the slope morphology or SMORPH method, which has a better degree of accuracy than the Storie Index and SINMAP methods to identify and classify potential landslide areas based on the matrix between slope shape and slope angle. This study resulted in 4 levels of landslide potential areas, namely very low, low, medium and high potential. Areas with high landslide potential dominate the northern and southern parts of Ambon City. In the region, most landslides occur in the form of sunken and convex slopes. The region has a hilly and mountainous topography with a steep slope. The results of this research using the SMORPH method can illustrate that the slope of the increasingly higher slope accompanied by the shape of a convex or concave slope will cause the potential for landslides that are higher in the region. https://jtsl.ub.ac.id/index.php/jtsl/article/view/773Spatial AnalysisLandslide ProneAmbon CitySMORPH |
spellingShingle | Heinrich Rakuasa S Supriatna Mangapul Parlindungan Tambunan Melianus Salakory Wiclif. S. Pinoa ANALISIS SPASIAL DAERAH POTENSI RAWAN LONGSOR DI KOTA AMBON DENGAN MENGGUNAKAN METODE SMORPH JTSL (Jurnal Tanah dan Sumberdaya Lahan) Spatial Analysis Landslide Prone Ambon City SMORPH |
title | ANALISIS SPASIAL DAERAH POTENSI RAWAN LONGSOR DI KOTA AMBON DENGAN MENGGUNAKAN METODE SMORPH |
title_full | ANALISIS SPASIAL DAERAH POTENSI RAWAN LONGSOR DI KOTA AMBON DENGAN MENGGUNAKAN METODE SMORPH |
title_fullStr | ANALISIS SPASIAL DAERAH POTENSI RAWAN LONGSOR DI KOTA AMBON DENGAN MENGGUNAKAN METODE SMORPH |
title_full_unstemmed | ANALISIS SPASIAL DAERAH POTENSI RAWAN LONGSOR DI KOTA AMBON DENGAN MENGGUNAKAN METODE SMORPH |
title_short | ANALISIS SPASIAL DAERAH POTENSI RAWAN LONGSOR DI KOTA AMBON DENGAN MENGGUNAKAN METODE SMORPH |
title_sort | analisis spasial daerah potensi rawan longsor di kota ambon dengan menggunakan metode smorph |
topic | Spatial Analysis Landslide Prone Ambon City SMORPH |
url | https://jtsl.ub.ac.id/index.php/jtsl/article/view/773 |
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