Morphometric Analysis and Stress Orientation of Kaba, Daun, and HulupalikVolcanoes, Bengkulu Province, Indonesia

Authors

  • Abimayu Program Studi Geofisika, Univesitas Bengkulu Author
  • Arif Ismul Hadi Hadi Program Studi Geofisika, Universitas Bengkulu Author
  • Refrizon Program Studi Geofisika, Univesitas Bengkulu Author
  • Nanang Sugianto Program Studi Geofisika, Univesitas Bengkulu Author
  • Dwiyono PVMKG, Stasiun Gunung Kaba, Bengkulu Author
  • Andre Rahmat Al Ansory Program Studi Geofisika, Univesitas Bengkulu Author
  • Hana Raihana Raihana Program Studi Geofisika, Univesitas Bengkulu Author
  • Arieffin Yusuf Hakim Hakim Program Studi Geofisika, Univesitas Bengkulu Author
  • Asy Syifa Auliya Putri Ramadhani Program Studi Geofisika, Univesitas Bengkulu Author

Abstract

Bengkulu Province is an area in Sumatra that is surrounded by Bukit Barisan. This research aims to provide information about the horizontal stress orientation data σHmaxs on the volcanoes of Kaba, Bukit Daun, and Hulupalik, as well as added information about the slope data in the research location that underlies the volcanic arc on the Sumatra Fault. We conducted this research by mapping the morphology of the mountain and determining the straight line of stress orientation, this research uses DEMNAS data of Geospatial Information Agency (BIG). At Kaba Mountain, the maximum stress azimuth angle (σHmaxs) is orientated towards 62° to the East-Northeast/ENE. The direction of plate movement that gives horizontal stress on Kaba volcano is from the east-northeast / ENE and west-southwest / WSW. On Mount Hulupalik determining the azimuth angle of the orientation of the Horizontal stress σHmaxs, the azimuth is towards NNE29°. On Mount Daun where the azimuth angle itself is NNE26°. From the azimuth direction of the horizontal stress (σHmaxs) of Mount Daun and Hulupalik, the plate stress moves from South Southwest/SSW and North Northeast/NNE. Regardless of the direction of horizontal stress/σHmaxs of each mountain, it is influenced by several factors that can cause different stress directions.

Article ID

15222

Published

2024-12-18