IDENTIFIKASI PENINGGALAN ARKEOLOGI MENGGUNAKAN METODE GEOLISTRIK KONFIGURASI DIPOLE-DIPOLE DI SITUS LIYANGAN JAWA TENGAH

UTAMA, BONANG SURYA (2024) IDENTIFIKASI PENINGGALAN ARKEOLOGI MENGGUNAKAN METODE GEOLISTRIK KONFIGURASI DIPOLE-DIPOLE DI SITUS LIYANGAN JAWA TENGAH. Other thesis, UPN Veteran Yogyakarta.

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Abstract

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ABSTRAK
IDENTIFIKASI PENINGGALAN ARKEOLOGI MENGGUNAKAN METODE
GEOLISTRIK KONFIGURASI DIPOLE DIPOLE DI SITUS LIYANGAN
JAWA TENGAH
Bonang Surya Utama
115.190.075
Candi Liyangan ditemukan pada saat kegiatan penambangan pasir dan
dalam kondisi terkubur. Balai Arkeologi Provinsi Daerah Istimewa Yogyakarta
telah meneliti dan mengungkapkan bahwa Situs Liyangan merupakan sebuah
pemukiman kuno yang dihuni oleh masyarakat dari abad ke-Masehi. Permukiman
Liyangan terkubur akibat letusan Gunung Sindoro, dan ditemukan peninggalan
berupa candi, talus, petirtaan, batur, dan arca yang terbuat dari batu andesit.
Material vulkanik yang mengubur Candi Liyangan adalah batuan piroklastik,
sehingga mudah untuk memahami perbedaan antara peninggalan arkeologi yang
terbuat dari batu andesit dan batuan piroklastik karena perbedaan material
penyusun litologi batuannya. Perbedaan material penyusun litologi batuan dapat
diketahui menggunakan metode geolistrik. Metode geolistrik resistivitas
merupakan salah satu metode geofisika yang dapat menggambarkan keadaan
bawah permukaan bumi dengan cara mempelajari sifat aliran listrik batuan di
bawah permukaan bumi berdasarkan perbedaan nilai resistivitas batuan. Penelitian
ini dilakukan dengan menggunakan metode geolistrik resistivitas untuk dapat
mengetahui sebaran peninggalan Candi Liyangan sehingga dapat menjadi acuan
dalam pengembangan Candi Liyangan berdasarkan aspek kepariwisataan,
geoarkeologi, dan pendidikan. Pengukuran data menggunakan 9 lintasan yang
tersebar di area Situs Liyangan. Hasil pengolahan data dan interpretasi data
menunjukkan bahwa 6 lintasan memiliki anomali nilai resistivitas yang tinggi
(>2000 Ω.m) dan terletak di permukaan bumihingga kedalaman 4 meter sehingga
diduga merupakan peninggalan Candi Liyangan.
Kata kunci: Candi Liyangan, Resistivitas, Geolistrik, Dipole-Dipole
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ABSTRACT
IDENTIFICATION OF ARCHEOLOGICAL USING DIPOLE-DIPOLE
CONFIGURATION GEOELECTRI METHODS AT LIYANGAN SITE, CENTRAL
JAVA
Bonang Surya Utama
115.190.075
Liyangan Temple was discovered during sand mining activities and in a
buried condition. The Archaeology Agency of Yogyakarta Special Region
Province has researched and revealed that Liyangan Site is an ancient settlement
inhabited by people from the 2nd century AD. The Liyangan settlement was
buried due to the eruption of Mount Sindoro, and relics were found in the form of
temples, talus, petition, batur, and statues made from andesite stone. The volcanic
material that buried Liyangan Temple is pyroclastic rock, so it is easy to
understand the difference between archaeological relics made from andesite stone
and pyroclastic rock because of the difference in the material that makes up the
rock lithology. Differences in the materials that make up rock lithology can be
determined using geoelectric methods. Resistivity geoelectric method is one of the
geophysical methods that can describe the state of the earth's subsurface by
studying the electrical flow properties of rocks below the earth's surface based on
differences in rock resistivity values. This research was conducted using the
resistivity geoelectric method to determine the distribution of Liyangan Temple
relics so that it can be a reference in the development of Liyangan Temple based
on tourism, geoarchaeological, and educational aspects. Data measurements
using 9 lines scattered in the Liyangan Site area. The results of data processing
and data interpretation show that 6 passes hgave very high resistivity value
anomalies (> 2000 Ω.m) and are located on the earth's surface to a depth of 4
meters so they are suspected of being relics of Liyangan Temple.
Keywords: Liyangan Temple, Resistivity, Geoelectric, Dipole-Dipole

Item Type:	Thesis (Other)
Uncontrolled Keywords:	Liyangan Temple, Resistivity, Geoelectric, Dipole-Dipole
Subjects:	Q Science > QE Geology
Divisions:	Faculty of Engineering, Science and Mathematics > School of Engineering Sciences
Depositing User:	Eko Yuli
Date Deposited:	19 Jul 2024 02:09
Last Modified:	19 Jul 2024 02:09
URI:	http://eprints.upnyk.ac.id/id/eprint/40304

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