Geology and Landslide Vulnerability Zoning Using Analytical Hierarchy Process in The Kebanaran Area and Surrounding Areas, Mandiraja District, Banjarnegara Regency, Central Java
DOI:
https://doi.org/10.20884/1.dinarek.2025.21.1.48Keywords:
DAFTAR PUSTAKA [1] Varnes, D. J., 1978. Slope Movement Types and Process. Special Report 176; Landslides; Analysis Control. Eds R. L. Schuster and R. J. Krizek. Transport Research Board, National Research Council, Washington D. C. [2] Condon, W., Pardyanto, I., Ketner, K., Amin, T., Gafoer, S., & Samodra, H. (1996). Peta Geologi Lembar Banjarnegara dan Pekalongan Skala 1:100.000. Bandung: Pusat Penelitian dan Pengembangan Geologi. [3] Djuri, M., Samodra, H., Amin, T., & Gafoer, S. (1996). Peta Geologi Regional Lembar Purwokerto dan Tegal Skala 1:100.000. Bandung: Pusat Penelitian dan Pengembangan Geologi. [4] Sinarta, I. N., Rifai, A., & Wilopo, W. (2006). Indeks Ancaman Gerakan Tanah Dengan Metode Analytical Hierarchy Process (AHP) Untuk Penataan Infrastruktur Kepariwisataan di Kawasan Geopark Gunung Batur, Kabupaten Bangli. [5] Kalijati, M., Sutriyono, & Jati, S. (2019). Analisis Bahaya Longsor dengan Menggunakan Metode Analytical Hierarchy Process (AHP) di Desa Lubuk Atung, Kabupaten Lahat. [6] Brahmantyo, B., & Bandono. (2006). Klasifikasi Bentuk Muka Bumi (Landform) untuk Pemetaan Geomorfologi pada Skala 1:25.000. Jurnal Geoaplika volume 1, no. 2, 71-78. [7] Darmawan, M, & Theml, S. (2008). Katalog MethodologiPenyusunan Peta Geo Hazard Dengan GIS. Banda Aceh: Badan Rehabilitasi dan Rekonstruksi (BRR) NAD-Nias.Banda Aceh. [8] Anbalagan, R. Landslide Hazard Evaluation and Zonation Mapping in Mountainous Terrain. Engineering Geology, 32. (1992): 269-277 [9] van Zuidam, R. (1985). Aerial Photointerpretation in Terrain Analysis and Geomorphologic Mapping. The Hague: Smits. [10] Dewi, T. S., Kusumayudha, S. B., Purwanto, H. S. Zonasi Rawan Bencana Tanah Longsor Dengan Metode Analisis GIS: Studi Kasus Daerah Semono dan Sekitarnya, Kecamatan Bagelen, Kabupaten Purworejo, Jawa Tengah. Jurnal Mineral, Energi dan Lingkungan vol. 1, no. 1, (2017), p. 50-59. [11] Zaenurrohman, Januar Aziz dan Indra Permanajati. 2019. Zona Kerentanan Gerakan Tanah (LONGSOR) di Daerah Kedungbanteng Menggunakan Analytical Hierarchy Process (AHP). Prosiding Seminar Nasional dan Call for Papers “Pengembangan Sumber Daya Pedesaan dan Kearifan Lokal Berkelanjutan IX”. Purwokerto. [12] Karnawati, D. 2005. Bencana Alam Gerak Massa Tanah di Indonesia dan Upaya Penanggulangannya, JurusAbstract
The Kabanaran area and its surroundings, Mandiraja District, Banjarnegara Regency, Central Java is an area located on the banks of the Serayu River and borders the southern mountain range. The research area is also an area that allows landslides to occur, this is due to several natural factors and human activity factors that cause landslides. This research was conducted to explain the relationship between geological conditions and landslide vulnerability factors in the research area. The method used is the Analytical Hierarchy Process (AHP) method. This method matches several parameters that are considered as factors in the occurrence of landslides and is given a value based on the weighting criteria. Based on the results of the study, there are several parameters, such as natural factors, geology, and other activities that affect landslides in the research area, including rainfall intensity, lithology, assessment frequency and weighting as to obtain the final value in determining the landslide vulnerability zone. The results of these calculations produce 4 levels of landslides, namely low landslide vulnerability zones, moderate landslide vulnerability zones, high landslide vulnerability zones, and very high landslide vulnerability zones.
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References
Varnes, D. J., 1978. Slope Movement Types and Process. Special Report 176; Landslides; Analysis Control. Eds R. L. Schuster and R. J. Krizek. Transport Research Board, National Research Council, Washington D. C.
Condon, W., Pardyanto, I., Ketner, K., Amin, T., Gafoer, S., & Samodra, H. (1996). Peta Geologi Lembar Banjarnegara dan Pekalongan Skala 1:100.000. Bandung: Pusat Penelitian dan Pengembangan Geologi.
Djuri, M., Samodra, H., Amin, T., & Gafoer, S. (1996). Peta Geologi Regional Lembar Purwokerto dan Tegal Skala 1:100.000. Bandung: Pusat Penelitian dan Pengembangan Geologi.
Sinarta, I. N., Rifai, A., & Wilopo, W. (2006). Indeks Ancaman Gerakan Tanah Dengan Metode Analytical Hierarchy Process (AHP) Untuk Penataan Infrastruktur Kepariwisataan di Kawasan Geopark Gunung Batur, Kabupaten Bangli.
Kalijati, M., Sutriyono, & Jati, S. (2019). Analisis Bahaya Longsor dengan Menggunakan Metode Analytical Hierarchy Process (AHP) di Desa Lubuk Atung, Kabupaten Lahat.
Brahmantyo, B., & Bandono. (2006). Klasifikasi Bentuk Muka Bumi (Landform) untuk Pemetaan Geomorfologi pada Skala 1:25.000. Jurnal Geoaplika volume 1, no. 2, 71-78.
Darmawan, M, & Theml, S. (2008). Katalog MethodologiPenyusunan Peta Geo Hazard Dengan GIS. Banda Aceh: Badan Rehabilitasi dan Rekonstruksi (BRR) NAD-Nias.Banda Aceh.
Anbalagan, R. Landslide Hazard Evaluation and Zonation Mapping in Mountainous Terrain. Engineering Geology, 32. (1992): 269-277
van Zuidam, R. (1985). Aerial Photointerpretation in Terrain Analysis and Geomorphologic Mapping. The Hague: Smits.
Dewi, T. S., Kusumayudha, S. B., Purwanto, H. S. Zonasi Rawan Bencana Tanah Longsor Dengan Metode Analisis GIS: Studi Kasus Daerah Semono dan Sekitarnya, Kecamatan Bagelen, Kabupaten Purworejo, Jawa Tengah. Jurnal Mineral, Energi dan Lingkungan vol. 1, no. 1, (2017), p. 50-59.
Zaenurrohman, Januar Aziz dan Indra Permanajati. 2019. Zona Kerentanan Gerakan Tanah (LONGSOR) di Daerah Kedungbanteng Menggunakan Analytical Hierarchy Process (AHP). Prosiding Seminar Nasional dan Call for Papers “Pengembangan Sumber Daya Pedesaan dan Kearifan Lokal Berkelanjutan IX”. Purwokerto.
Karnawati, D. 2005. Bencana Alam Gerak Massa Tanah di Indonesia dan Upaya Penanggulangannya, Jurusan Teknik Geologi, Fakultas Teknik Universitas Gadjah Mada, Yogyakarta.
Standar Nasional Indonesia. 2005. Penyusunan Peta Zonasi Gerakan Tanah SNI 13-7124- 2005. ICS 07.060, Badan Standardisasi
