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Ayub Pratama Aris
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Geology Engineering Study Program, Universitas Negeri Gorontalo Prof. Dr. Ing. B. J. Habibie Street, Moutong, Tilongkabila, Bone Bolango 96119, Gorontalo, Indonesia
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JAGE
Published by Universitas Negeri Gorontalo
ISSN : 2964478X     EISSN : 29644534     DOI : https://doi.org/10.34312
Core Subject : Science, Social, Engineering,
Civil Engineering, Building, Construction & Architecture Earth & Planetary Sciences Energy Engineering Environmental Science
Journal of Applied Geoscience and Engineering (JAGE, P-ISSN: 2964-478X, E-ISSN: 2964-4534) is a peer-reviewed journal published by Geology Engineering Study Program, Universitas Negeri Gorontalo. JAGE 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. JAGE published two-issue articles per year namely June and December. JAGE provides a place for academics, researchers, and practitioners to publish scientific articles. Each text sent to JAGE editor is reviewed by peer review. Starting from Vol. 1 No. 1 (June 2022), all manuscripts sent to the JAGE editor are accepted in Bahasa Indonesia or English. The scope of the articles listed in this journal relates to various topics, including education for Geological, Geoscience and Engineering. This journal is available in print and online and highly respects the ethics of publication and avoids all types of plagiarism. JAGE has been identified in crossref with a DOI number: 10.34312.
Arjuna Subject : Ilmu Bumi dan Planet (semua kategori) - Teknik Geologi dan Geologi Teknik
Articles 5 Documents
 1 
Search results for , issue "Vol 1, No 1 : Juni 2022" : 5 Documents clear
Penentuan Tipe Akuifer Daerah Bulontala Kabupaten Bone Bolango Menggunakan Metode Geolistrik Dai, Elan; Zainuri, Ahmad; Akase, Noviar
Journal of Applied Geoscience and Engineering Vol 1, No 1 : Juni 2022
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1231.753 KB) | DOI: 10.34312/jage.v1i1.15533

Abstract

Research area Geographically, the location is at 0áµ’31'0''N - 0áµ’31'30'' North Latitude 123áµ’8'0'' - 123áµ’8'30'' East Longitude with an area of ± 22.02 km. The research location is an andesite lava hill unit. because the type of rock found at that location is andesite igneous rock. The purpose of this study is to determine the type or type of aquifer. The method used is in the form of collecting surface and subsurface geological data. The method used is the geoelectric method with the Schlumberger configuration. The results of the research for geological mapping of the research location have morphology in the form of volcanic plains and hills with an altitude of 200 meters above sea level. The statigraphic sequence at the research site is sorted from easy to leader, old unit in the form of Andesite and easy unit in the form of alluvial. As for the geological structure that plays a role in the study, the dominant direction is from the north to the south.Groundwater at the research site follows the topography of the research location which flows from south to north where the water flows from upstream to downstream, from high to low elevation points. based on the results of geoelectric research and well water data collection that the aquifer at that location is shallow with alluvial material types, sand and andesite igneous rocks.The type of aquifer at the research site obtained from geoelectric research is a free aquifer type (not compressed) and only has 1 boundary layer, namely andesite igneous rock.
Analisis Lokasi Sekolah SMA yang Ideal di Kabupaten Bone Bolango dengan Sistem Informasi Geografis Antu, Arjun B
Journal of Applied Geoscience and Engineering Vol 1, No 1 : Juni 2022
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (461.907 KB) | DOI: 10.34312/jage.v1i1.16740

Abstract

In Indonesia, the problem of educational equity is still a serious problem, there are still few schools and the distance between most students' homes and schools is quite far from the school location. This study aims to determine the location of the ideal high school in Bone Bolango Regency by using a Geographic Information System. The location of this research was carried out in Bone Bolango Regency, the schools studied were SMA Negeri 1 Tapa, SMA Negeri 1 Kabila, SMA Negeri 1 Suwawa, SMA Negeri 1 Suwawa Timur, SMA Negeri 1 Bone, SMA Negeri 1 Bone Pantai, SMA Negeri 1 Bulango Ulu. , SMA Negeri 1 Pinogu, SMAS Terpadu Wirabakti. The method used in the research is a survey, interviews and then given a score with predetermined criteria. Primary data is obtained directly through observations, field measurements and interpretation of satellite imagery. In this study, the primary data were land area for education units, slope, accessibility, free of disasters and landslides, educational reach, and number of students. Secondary data is obtained from information, statistical data and data derived from existing field data. In this study the secondary data is the distribution of high school schools. The time of the study was conducted for 6 months from February to July. The research results are based on parameters with certain criteria, namely land area for education units, slope, accessibility, free of disasters and landslides, and educational reach. Then the five parameters are scored and the results are overlaid into an ideal school map.
Geologi Wilayah Tapaluluo dan Sekitarnya, Kabupaten Gorontalo Rasyid, Fajri Fitrah Fidianto A.; Zainuri, Ahmad; Kasim, Muhammad
Journal of Applied Geoscience and Engineering Vol 1, No 1 : Juni 2022
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1234.609 KB) | DOI: 10.34312/jage.v1i1.15502

Abstract

The research area is geographically located at coordinates 0041'30” – 0045'00” North Latitude and 12300'30” – 12303' 35” East Longitude with an area of ± 41 Km2. The method used in this research is scientific exploration by conducting a survey of surface geological mapping. It is carried out in the preparation of literature, tools and materials, the data collection stage is in the form of geomorphological data, stratigraphy, geological structure measurements and documentation. The data processing stage is in the form of laboratory analysis, namely conducting petrographic analysis and processing geological structure data in the form of joints and faults using the stereographic method. The geomorphology of the research area is divided into three geomorphological units, namely; lava flow ridge units, intrusion hills, and fault zone hill units. The study area is divided into three rock units informally in order from oldest to youngest, namely: andesite porphyry unit (early-middle Miocene), granodiorite unit (middle-late Miocene), and modified andesite porphyry unit (middle-late Miocene). The geological structure of the study area consists of joints, Tapaluluo Fault, and Botupololondalange Shear Fault. The geological potential of the research area is in the form of mineralization and rock mining.
Estimasi Potensi Cadangan Air Tanah Dengan Metode Persamaan Darcy di Desa Pilomonu, Gorontalo Sugianti, Komang; Zainuri, Ahmad; Hutagalung, Ronal
Journal of Applied Geoscience and Engineering Vol 1, No 1 : Juni 2022
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (715.376 KB) | DOI: 10.34312/jage.v1i1.15505

Abstract

This research aims  to know  the  prediction   of potential   for  groundwater reserves.   The  research method  applies  surface  geological mapping  and subsurface  data  collection  with  the 200-span   Schlumberger configuration   geoelectric  method.  The  stratigraphy of the research   area  is  sorted  from  old  to  young,  the  first  is  the  granodiorite   unit,  the sandstone   unit,  and  alluvial   units   are  deposited   inconsistently.   The  geological structure working in the research area has a dominant northwest-southeast direction. The  direction  of. groundwater flow  follows the topography of the  research area, whicb is flowing from the north to the south, where the elevation  of the norlh js higher than the eJevation of the south. The aquifer characteristics in the research area can be divided  into two based  on the mterpretation  of geoelectric  inversion,  such as shallow  aquifer with material  in the  form of sand  and  deep  aquifer with  sand  and gravel material. Prediction  of the  potential  for  groundwater   reserves   is  obtained  from  the interpretation   of geoelectric  data  and data  from  the  calculation  of the  groundwater level in the research area by observing the. conditions  around the research area So, it is obtained a prediction  of potential  for shallow groundwater reserves is 360.444 m3/day or equivalent to  360,444   liters/day,  and  the  prediction   of poteptial   deep groundwater reserves is 66,520.476  m3/day or equivalent to 66:,520,476 liters/day.
Analisis Tipe Longsoran Daerah Pohe Kota Gorontalo Berdasarkan Orientasi Struktur Geologi Usman, Fatma T.; Arifin, Yayu Indriati; Hutagalung, Ronal; Permana, Aang Panji
Journal of Applied Geoscience and Engineering Vol 1, No 1 : Juni 2022
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1025.447 KB) | DOI: 10.34312/jage.v1i1.15517

Abstract

Administratively, the research area is located in Pohe Village, Hulonthalangi sub-district, Gorontalo City, Gorontalo Province. Astronomically, the research area is at coordinates 00030'16.10"- 00030'41.58" north latitude and 12302'36.10"- 12303'19.55" east longitude. The purpose of this study was to analyze the type of landslide based on the orientation of the geological structure of the Pohe area and the type of landslide based on the orientation of the geological structure of the Pohe area. The method used in this research is retrieval of field data, namely lithological data, geological structure data and slope data of the research area, then structural data processing using dips 6.0 software application and analyzed using stereographic projections. Based on the results of identification and stereographic analysis, it shows that in the research area there are 2 types of landslides, namely plane failure and toppling failure. The type of plane failure is found at stations 1.1, 1.2, 1.3, 1.4, and 1.6. While the type of landslide toppling failure is found at stations 1.5, 1.7, and 1.8.

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