dc.contributor.author | Sunarti, Syamsidar | |
dc.date.accessioned | 2023-05-29T01:27:32Z | |
dc.date.available | 2023-05-29T01:27:32Z | |
dc.date.issued | 2023-05-29 | |
dc.identifier.citation | RPIJM 2018 RPIJM Kabupaten Kutai Kartanegara. Kutai Kartanegara. Syamsidar, S M and Alam F 2019 Memahami Bencana Banjir dan Longsor (Samarinda: RV Pustaka Horizon). Moss S, Chambers J, Cloke I R, Nas D S 1997 New observations on the sedimentary and tectonic evolution of the Tertiary Kutai Basin, East Kalimantan. Satyana A H 1999 Kalimantan An Outline of The Geology of Indonesia (Indonesian Association of Geologist) p.69-89. Van Bemmelen R W 1949 The Geology of Indonesia Vol IA (The Hague: Netherlands, Govt. Printing Office) p.732. Nuay 1985 Kerangka Tektonik Pulau Kalimantan: Peta Geologi Lembar Kotabaru. Allen G P and Chambers J L 1998 Sedimentation In The Modern and Miocene Mahakam Delta (Indonesia: IPA). https://tanahair.indonesia.go.id/demnas/#/ accessed 19 April 2021. Supriatna, S. Sukardi, R, and R. Rustandi. (1995). Peta Geologi Bersistem, Lembar Samarinda, Kalimantan sekala 1:250.000, Pusat Penelitian dan Pengembangan Geologi Bandung. Badan Nasional Penanggulangan Bencana 2019 Petunjuk Teknis Kawasan Rawan Bencana Tanah Longsor Jakarta. Van Zuidam (1985). Aerial Photo – Interpretation in Terrain Analysis and Geomorphologic Mapping, The Hague: Netherlands, Smith Publisher. Karnawati, D. (2005). Bencana Alam Gerakan Massa Tanah di Indonesia dan Upaya Penanggulangannya, Jurusan Teknik Geologi Fakultas Teknik Universitas Gadjah Mada, Yogyakarta | id_ID |
dc.identifier.other | 1071012007 | |
dc.identifier.uri | https://dspace.umkt.ac.id//handle/463.2017/3228 | |
dc.description.abstract | Abstract. The Kalimantan Island is part of the Sundaland crust, namely the Eurasian Continental
Plate. The plate is moving to the southeast colliding with the Indo-Australian plate which is
moving north. Whereas for Kutai Kartanegara Regency in the Kalimantan Island position is far
from the collision zone, so it is relatively stable tectonically. This is important to research that
is, due to tectonic processes that occurred earlier, resulting in the formation of geological
structures, especially faults. The purpose of the study was to determine the morphotectonic and
landslide hazards in the Kutai Kartanegara Regency, where this research was carried out
quantitatively with data collection techniques, then analyse landslide hazards based on data;
DEM (Digital Elevation Model) including the slope, slope direction, and slope length for
vulnerability analysis, geological data from Regional Geological Maps, which include rock
formations, distances from faults data and administrative boundary spatial data in the form of
vector GIS for the preparation of landslide hazard maps. The result showing Kutai Kartanegara
predominantly categorized as moderate to high hazard zone. The low hazard zone covering
9.88% area, moderate hazard zone covering 35.81% area, and 54.31% area is high hazard zone
of landslide. The analysis showing that the hazard of the research area consist predominantly
sedimentary rocks and controlled by structural geology identified as thrust fault, strike slip fault,
and fold which include in Anticlinorium Samarinda. Those lithology and geological structure
features along with the slope are identified as controlling factor to the landslide hazard in the
research area. | id_ID |
dc.language.iso | en | id_ID |
dc.publisher | IOP Conference Series: Earth and Environmental Science | id_ID |
dc.relation.ispartofseries | IOP Publishing;10.1088/1755-1315/1071/1/012007 | |
dc.title | Preliminary Study of Landslide Hazard in Kutai Kartanegara Regency, East Kalimantan using Digital Elevation Model | id_ID |
dc.type | Article | id_ID |