cover
Contact Name
M. Iqbal Liayong Pratama
Contact Email
m.iqbal@ung.ac.id
Phone
+6285839510899
Journal Mail Official
jrpi@ung.ac.id
Editorial Address
Jl. Prof. Dr. Ing. B. J. Habibie, Moutong, Tilongkabila, Kabupaten Bone Bolango 96119, Gorontalo, Indonesia.
Location
Kota gorontalo,
Gorontalo
INDONESIA
Jurnal Riset dan Pengabdian Interdisipliner
ISSN : 30646111     EISSN : 30646111     DOI : https://doi.org/10.37905/jrpi.vxi
Jurnal Riset dan Pengabdian Interdisipliner (JRPI, E-ISSN: 3064-6111) is a peer-reviewed journal published by Department of Earth Science and Technology, Universitas Negeri Gorontalo. JRPI provides open access to the principle that research published in this journal is freely available to the public to support the exchange of knowledge globally. JRPI published four-issue articles per year namely October, January, April and July. JPRI provides a place for academics, researchers, and practitioners to publish scientific articles. Each text sent to JRPI editor is reviewed by peer review. Starting from Vol. 1 No. 1 (October 2024), all manuscripts sent to the JRPI editor are accepted in Bahasa Indonesia or English. The scope of the articles listed in this journal relates to various topics, including Geography and Geology, Social Science, education for Sustainable Development, Community Services, People, Local Food Security, Nutrition and Public Health, Training, Marketing, Appropriate Technology, Design, Community Empowerment, Social Access, Student Community Services, Border Region, Less Developed Region. This journal is available in print and online and highly respects the ethics of publication and avoids all types of plagiarism. JPRI has been identified in crossref with a DOI number: 10.37905.
Arjuna Subject : Umum - Umum
Articles 232 Documents
Kajian Geologi Dan Statigrafi Daerah Botu dan Sekitarnya, Provinsi Gorontalo Hambali, Fauzia; Maryati, Sri; Akase, Noviar
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Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jrpi.v3i2.39020

Abstract

The research is located in Gorontalo Province, precisely in Dumbo Raya District with coordinates 0°32’24” N and 123°4’32” E. Geologically, the research area is located on the North Arm of Sulawesi Island and belongs to the Southern Mountain Zone. The geological conditions of this region are influenced by complex tectonic activities and intensive geomorphological processes that form diverse landscapes. This research aims to determine the geological conditions including geomorphology, stratigraphy, and geological structures. The method used is field geological mapping supported by secondary data, through observations of rock outcrops, lithological descriptions, and measurements of geological structures. The results show that the geomorphology of the area is dominated by denudational hill units and alluvial plains. The hill units are composed of igneous rocks such as granodiorite and andesite that have experienced weathering and erosion, forming steep slopes. The alluvial plain units are composed of younger loose material. Stratigraphically, the research area consists of granodiorite, andesite, and limestone unit.
Geologi Daerah Talumolo dan sekitarnya, Kecamatan Dumbo Raya, Provinsi Gorontalo Ardiansyah, Alief; Maryati, Sri; Akase, Noviar
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Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jrpi.v3i2.39016

Abstract

This research is located in Talumolo Village and its surroundings in Dumbo Raya District, Gorontalo City, Gorontalo Province, which is located at coordinates 0°32'59" N to 0°34'15" N and 123°02'32" E to 123°04'01" E. This research aims to analyze the geological conditions of the Talumolo area and its surroundings. The methods used include surface geological mapping, lithological analysis, geological structures. The results of the study indicate that the research area is composed of volcanic and sedimentary rocks that have undergone weathering, and has geological structures such as joints and geomorphological conditions of the research area are dominated by denudational hill units and alluvial plain units, which are formed due to weathering and erosion processes over a long period of time.

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