%0 Thesis
%9 Skripsi
%A Amalia Nur Azizah, NIM.: 22106020021
%B FAKULTAS SAINS DAN TEKNOLOGI
%D 2026
%F digilib:75894
%I UIN SUNAN KALIJAGA YOGYAKARTA
%K Tanah Bergerak, Bidang Gelincir, Konfigurasi Wenner-Schlumberger
%P 133
%T ANALISIS BIDANG GELINCIR DENGAN METODE GEOLISTRIK KONFIGURASI WENNERSCHLUMBERGER DI DESA RATAMBA, KECAMATAN PEJAWARAN, KABUPATEN BANJARNEGARA
%U https://digilib.uin-suka.ac.id/id/eprint/75894/
%X The landslide event that resulted in damage to several houses and road occurred in  Kaliireng Hamlet, Ratamba Village, Pejawaran District, Banjarnegara Regency.  One of the factors influencing the event is the presence of a slip surface, which can  be identified through subsurface lithological layers based on resistivity values.  Research was conducted in the moving land zone aimed to identify the slip surface  using the Wenner–Schlumberger configuration geoelectrical resistivity method. The  result of data collection on 4 tracks were processed using Res2DInv software. The  obtained 2D model was interpreted basod on the results of field werification ang  geological data from the Kalibiuk formation ang Jembangan volcano formation.  The interpretation results showed a low-resistivity layer (≤20 Ωm) in the form of  marl acting as a slip surface found at a depth of 3 meters to 5 meters and distributed  downwards, a medium-resistivity layer (20 to 125 Ωm) in the form of clayey soil  acting as the moving material found on the surface to a depth of 3 meters to 5 meters  and a high-resistivity layer (>125 Ωm) in the form of andesite rocks found in the  northern part and several boulders found on the surface. The slip surface is  suspected to blocated beneath clayey soil at a depth of 3 to 5 meters. The results of  the study are expected to be used as a reference and basis for consideration in the  preparation and development of village spatial palnning, especially in areas  affected by moving ground events.
%Z Dr. Thaqibul Fikri Niyartama, S.Si., M.Si. dan Nugroho Budi  Wibowo, S.Si., M.Sc.