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ANALISIS BIDANG GELINCIR DENGAN METODE GEOLISTRIK KONFIGURASI DIPOLE-DIPOLE DI DUSUN BENGLE, KECAMATAN TIRTOMOYO, KABUPATEN WONOGIRI
The landslide disaster that occurred in Bengle Hamlet, Dlepih Village, Tirtomoyo District, Wonogiri Regency has resulted in two fatalities and damage to several houses. The factor that influences the occurrence of landslides is the presence of slip areas. The slip area can be identified by identifying subsurface layers using geophysical methods. The method used in this research is the geoelectric resistivity method with a resistivity meter, namely the Naniura NRD-300 HF and produces current and potential difference values. The resulting data is then processed using Res2dinv software. From the processing results, it was obtained that the resistivity value range for the area was 2.32 to 3803 Ωm. classified into two categories, namely, values ≤107 Ωm are sediment deposits that act as landslide material. Values >107 Ωm are included in the bedrock category which acts as a slip surface. The slip area is thought to be andesite which stretches from west to east with a thickness of ± 17 meters.
FAKULTAS SAINS DAN TEKNOLOGI, UIN SUNAN KALIJAGA YOGYAKARTA
NIM.: 21106020026 Indar Mery Sulya Aryani
ANALISIS BIDANG GELINCIR DENGAN METODE GEOLISTRIK KONFIGURASI DIPOLE-DIPOLE DI DUSUN BENGLE, KECAMATAN TIRTOMOYO, KABUPATEN WONOGIRI (Text)
ANALISIS BIDANG GELINCIR DENGAN METODE GEOLISTRIK KONFIGURASI DIPOLE-DIPOLE DI DUSUN BENGLE, KECAMATAN TIRTOMOYO, KABUPATEN WONOGIRI (Other)
HTML Summary of #69978 ANALISIS BIDANG GELINCIR DENGAN METODE GEOLISTRIK KONFIGURASI DIPOLE-DIPOLE DI DUSUN BENGLE, KECAMATAN TIRTOMOYO, KABUPATEN WONOGIRI