Abstract
Megalithic age artifacts are spreaded in the Jember region, one of them in the Kendal hamlet adjacent to the Duplang site. There are still many artifacts buried in this location that need to be explored using the geoelectric resistivity method of the Wenner configuration. Data acquisition was carried out on 3 lines with length of 40 m. Base on 2D resistivity distribution image for all three lines, it was known that the subsurface structures were dominated by clay with resistivity value of (1.54 – 89.4) Ωm. Resistivity anomaly with value (197-581) Ωm, which are suspected of being andesite stones forming the artifacts are at a depth (0.25 -3.19) m on the three lines. The presumption existence of the artifacts is reinforced by the presence of kenong rock and menhirs outcrops on line 2.
Highlights
PENDAHULUAN Sejarah peradaban manusia di Indonesia dibedakan atas beberapa zaman, salah satunya yaitu zaman pra-sejarah
Megalithic age artifacts are spreaded in the Jember region, one of them in the Kendal hamlet adjacent to the Duplang site
There are still many artifacts buried in this location that need to be explored using the geoelectric resistivity method of the Wenner configuration
Summary
PENDAHULUAN Sejarah peradaban manusia di Indonesia dibedakan atas beberapa zaman, salah satunya yaitu zaman pra-sejarah. Hal ini diperkuat dengan hasil penelitian (Maskur, 2016) yang menyatakan bahwa batu andesit banyak digunakan dalam bangunan dan peralatan zaman prasejarah. Berdasarkan hasil yang diperoleh, citra sebaran resistivitas pada lintasan 1 mempunyai nilai (1.54-581) Ωm.
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: Jurnal Fisika Flux: Jurnal Ilmiah Fisika FMIPA Universitas Lambung Mangkurat
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
