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All Journal Tunas Geografi Paduraksa : Jurnal Teknik Sipil Universitas Warmadewa Jurnal Pengelolaan Sumberdaya Alam dan Lingkungan (Journal of Natural Resources and Environmental Management) AKSIOLOGIYA : Jurnal Pengabdian Kepada Masyarakat UNM Geographic Journal SELAPARANG: Jurnal Pengabdian Masyarakat Berkemajuan Jambura Geoscience Review Lamahu: Jurnal Pengabdian Masyarakat Terintegrasi Sustainability (STPP) Theory, Practice and Policy Geosfera: Jurnal Penelitian Geografi JAGE Panrita Inovasi: Jurnal Pengabdian Kepada Masyarakat Jurnal Riset dan Pengabdian Interdisipliner

Noviar Akase

Universitas Negeri Gorontalo

Author-ID : 1069676

Agriculture, Biological Sciences & Forestry Humanities Astronomy Civil Engineering, Building, Construction & Architecture Computer Science & IT Control & Systems Engineering Earth & Planetary Sciences Economics, Econometrics & Finance Education Energy Engineering Environmental Science Health Professions Languange, Linguistic, Communication & Media Law, Crime, Criminology & Criminal Justice Medicine & Pharmacology Nursing Physics Public Health Social Sciences Other

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GEOLOGI BAWAH PERMUKAAN DESA DAMBALO KECAMATAN TOMILITO KABUPATEN GORONTALO UTARA Cindi Claudia Male; Ahmad Zainuri; Noviar Akase
Sustainability (STPP) Theory, Practice and Policy Vol. 4 No. 1 (2024): Sustainability: Theory, Practice and Policy June Edition
Publisher : Pusat Kajian Berkelanjutan UIN Sulthan Thaha Saifuddin Jambi

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.30631/sdgs.v4i1.2424

Dambalo Village, Tomilito District, North Gorontalo Regency, Gorontalo Province, is the designated research area listed in the administrative records. The main objectives of this research are to determine the surface and subsurface geology, understand the geological conditions of the research area, and analyze the cross-section of subsurface geological layers. The study employs the Schlumberger configuration geoelectric method to examine the subsurface geological cross-section. The researchers used a combination of geological surveys and subsurface data surveys, collecting data on surface geological features, outcrop observations, and resistivity measurements. The research area features a single landform unit, the denudational plain, and its stratigraphy includes a lithostratigraphic unit, Volcanic Breccia. The study area comprises four rock layers: the first layer is topsoil (passive clay), the second layer is sand, the third layer is breccia, and the fourth layer is sand. These conclusions are supported by geological and geoelectric data, demonstrating the effectiveness of integrating surface and subsurface surveys to provide a comprehensive understanding of the geological structure.

Analysis of Microfaces and Depositional Environment of Limestone in North Isimu Area, Gorontaolo Regency Robot, Ladya Cheryl; Permana, Aang Panji; Akase, Noviar
Tunas Geografi Vol 13, No 1 (2024): JURNAL TUNAS GEOGRAFI
Publisher : Department of Geography Education, Faculty of Social Sciences, Universitas Negeri Medan

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24114/tgeo.v13i1.41981

The geological conditions in the northern part of Lake Limboto vary greatly from the constituent rocks to the working geological structures. Lithological variations consist of volcanic and plutonic rocks to limestone. The area where limestone is widely distributed is in the North Isimu Region, Gorontalo Regency. This research aims to analyze the geological conditions, microfacies and depositional environment of limestone in the North Isimu Region, Gorontalo Regency. The research methods used to achieve this goal consist of field surveys and petrographic laboratory analysis. Field surveys include taking rock samples, taking coordinate points, taking elevation, geomorphological observations, observing geological structures and taking field documentation. Meanwhile, petrographic analysis of rocks uses a polarizing microscope as a tool to follow up megascopic observations. Observation of rock incisions under a microscope using cross nicol and parallel nicol. Based on the results and discussion, it shows that the geomorphology of the research area includes structural hills with sub-parallel river flow patterns. The geological structure of the research area is a descending fault trending northwest-southeast. The research area is divided into four facies, namely foraminifera wackestone, crystalline limestone, foraminifera algae packstone and coralline floatstone. Standard microfacies (SMF) in the North Isimu Region consists of three SMF namely SMF-3, SMF-4 and SMF-5 with two limestone depositional environmental zones namely toe of slope (FZ-3) and slope (FZ-4). FZ-3 was deposited at the end of the foreslope zone and FZ-4 was deposited seaward of the foreslope from the edge of the carbonate debris platform.Keywords: Limestone; Microfacies; Depositional Environment; North Isimu

Analisis Petrografi Dan Sebaran Litologi Daerah Saripi Dan Sekitarnya, Kecamatan Paguyaman, Kabupaten Boalemo, Provinsi Gorontalo Rusdi, Infithar Hi; Arifin, Yayu Indriati; Akase, Noviar
Geosfera: Jurnal Penelitian Geografi Vol 1, No 1 (2022): Geosfera: Jurnal Penelitian Geografi
Publisher : Universitas Negeri Gorontalo

Lokasi penelitian terletak di Kecamatan Paguyaman, Kabupaten Boalemo, Provinsi Gorontalo. Ditinjau dari fisiografi regional lokasi penelitian termasuk dalam wilayah Pegunungan Selatan Bone-Tilamuta-Modello, sedangkan dari geologi regional terdapat empat formasi batuan di lokasi penelitian yaitu Formasi Diorit Boliohuto, Formasi Tinombo, Formasi Dolokapa, dan Formasi Endapan Danau. Tujuan penelitian ini adalah memetakan jenis dan sebaran litologi yang terdapat di lokasi penelitian berdasarkan analisis petrologi dan petrografi. Metode penelitian dilakukan dengan survei lintasan geologi permukaan berupa pendeskripsian petrologi singkapan batuan serta pengambilan sampel untuk analisis petrografi. Hasil yang diperoleh menunjukkan bahwa di lokasi penelitian terdapat dua jenis litologi yakni batuan beku dan batuan sedimen. Analisis petrografi membagi jenis litologi di lokasi penelitian menjadi lima satuan batuan : 1. Satuan Andesit tersebar seluas 16% luas lokasi penelitian, 2. Satuan Granodiorit yang menguasai 70% luas lokasi penelitian, 3. Satuan Batupasir sebarannya seluas 4% luas lokasi penelitian, 4. Satuan Tuff tersebar seluas 4% luas lokasi penelitian dan 5. Satuan Aluvial yang tersebar seluas 6% dari luas lokasi penelitian.

Potensi Airtanah Menggunakan Metode Geolistrik Resistivitas Di Desa Molingkapoto, Kecamatan Kwandang, Kabupaten Gorontalo Utara, Provinsi Gorontalo Fatimah, Siti; Kasim, Muhammad; Akase, Noviar
Geosfera: Jurnal Penelitian Geografi Vol 1, No 1 (2022): Geosfera: Jurnal Penelitian Geografi
Publisher : Universitas Negeri Gorontalo

Kecamatan Kwandang memiliki kepadatan penduduk tertinggi di Kabupaten Gorontalo Utara, dengan kepadatan penduduk 29.124 jiwa/km2. Kepadatan penduduk yang tinggi ini disbanding kecamatan lainya membuat kebutuhan kebutuhan air akan lebih banyak untuk melengkapi kebutuhan sehari-hari yang salah satunya warga memanfaatkan pemenuhannya dari air tanah. Hal ini penting untuk mengetahui arah aliran, karakteristik akuifer dan potensi air tanah. Tujuan dari penelitian ini adalah untuk mengetahui potensi airtanah di daerah penelitian. Metode yang digunakan dalam penelitian ini adalah pemetaan geologi pengumpulan data permukaan dan bawah permukaan dengan metode geolistrik konfigurasi Schlumberger. Hasil Penelitian yaitu Arah aliran muka air tanah mengikuti topografi daerah penelitian yang mengalir dari selatan, barat, timur ke utara. Karakteristik akuifer di daerah penelitian dibagi menjadi dua berdasarkan interpretasi data geolistrik, yaitu akuifer dangkal dengan material pasir halus dan akuifer dalam dengan material pasir dan kerikil. Potensi cadangan airtanah diperoleh dari interpretasi data geolistrik dan data perhitungan muka airtanah dangkal di lokasi penelitian. Dengan demikian, potensi airtanah dangkal di daerah penelitian adalah 1.264,54 m3/hari atau 0,014 m3/detik, prediksi potensi airtanah dalam adalah 3.536,39 m3/hari atau 0,040 m3/hari.

Bentuk Lahan Geomorfologi Di Daerah Gunungapi Ambang, Bolaang Mongondow Timur Sumarjis, Suly Ayu; Arifin, Yayu Indriati; Hutagalung, Ronal; Akase, Noviar; Manyoe, Intan Noviantari
Journal of Applied Geoscience and Engineering Vol 2, No 1 : Juni 2023
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.34312/jage.v2i1.19405

Sulawesi or Celebes is located in the central part of the Indonesian archipelago which has interesting geological potential to be developed. One of this interesting area is known as Ambang volcano area. Ambang volcano is one of the active volcanoes in North Sulawesi. Administratively, the research area is located in Bongkudai Baru Village, Modayag sub-district, East Bolaang Mongondow district, mapped at coordinates N 0°45'58.89'' and E 124°24'13.04''. This study is aimed to analyze volcanic geomorphological units using satellite imagery and surface geological mapping. The results showed that the geological conditions of the study area consist of 4 lithologies i.e volcanic breccia, andesite, agglomerate and sandstone rocks. Based on the morphographic and morphogenetic analysis of the study area which refers to the Van Zuidam and Verstapen 1985 classification, the study area is divided into five landforms i.e fumarole and solfatara ambang volcanic, ambang volcanic cone, plains and fluvial slope feet of ambang volcano, denudational hill ambang volcanoes and lake units.

Interpretasi Lapisan Bawah Permukaan Sebagai Perencanaan Tempat Penyimpanan Sampah Di Desa Talumelito, Kabupaten Gorontalo K Badaun, Nur Azizah; Zainuri, Ahmad; Akase, Noviar; Aris, Ayub Pratama
Journal of Applied Geoscience and Engineering Vol 1, No 2 : December 2022
Publisher : Universitas Negeri Gorontalo

The Talumelito waste storage area is located in Talumelito Village, Telaga Biru District, Gorontalo Regency which accommodates waste from various human activities. Organic and inorganic waste will become a breeding ground for diseases that are very dangerous for society and the environment. The purpose of this study was to determine the subsurface layer as an interpretation of the planning for the construction of a waste storage area and determine whether it is feasible or not. The resistivity geoelectric method of the Schlumberger configuration is one of the geophysical methods that is easy, inexpensive and efficient and does not damage the environment. The geoelectric method is a geophysical method used to identify the properties and physical conditions of the subsurface based on the resistivity values of the rock. This method utilizes variations in the resistivity values of the subsurface rocks to detect geological structures or subsurface rock formations. Based on an analysis of resistivity and geological electrical properties, the location of the planning for the construction of a waste storage area is at VES 2, VES 3, and VES 5 points. Where from the interpretation results the three VES points have bedrock rock layers with granite rock types. Meanwhile, at VES 1 and VES 4, there is a layer of sandstone under the top soil layer. VES 2, VES 3 and VES 5 points are suitable for waste storage because there are layers of waterproof rock. Whereas at VES 1 and VES 4 points it is not suitable for waste storage because the sandstone layer is a layer that has good permeability, so if there is liquid waste from garbage, the waste will contaminate groundwater.

Karakteristik Geomorfologi Daerah Ayuhulalo Dan Sekitarnya Kecamatan Tilamuta, Kabupaten Boalemo Mamonto, Fajri Kurniawan; Arifin, Yayu Indriati; Akase, Noviar; Manyoe, Intan Noviantari
Journal of Applied Geoscience and Engineering Vol 3, No 1 : Juni 2024
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jage.v3i1.26918

The research was conducted in Ayuhulalo area, which is located in the western part of Gorontalo Province, precisely in Tilamuta Sub-district, Boalemo Regency. The geomorphology of the research area is dominated by hilly to mountainous areas. The purpose of this study is to determine the characteristics of the landscape in the study area, determine Geomorphological units, and identify the type of constituent lithology in each Geomorphological unit with a remote sensing analysis approach based on DEM (Digital Elevation Model) SRTM (Shuttle Radar Topography Mission) data and field observations to identify the lithological conditions of the study area. The method includes aspects of geomorphology such as morphography, morphometry, and morphogenetics. The geomorphology of the study area consists of lava flow hills unit with porphyry andesite and porphyry dacite as the constituent lithology and pyroclastic flow hills unit where volcanic breccia is the constituent lithology.

Potensi Geodiversity Daerah Oluhuta Kecamatan Kabila Bone Kabupaten Bone Bolango Menggunakan Asesmen Ponto, Nadia Fransisca; Arifin, Yayu Indriati; Hutagalung, Ronal; Akase, Noviar; Manyoe, Intan Noviantari
Journal of Applied Geoscience and Engineering Vol 2, No 2 : Desember 2023
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jage.v2i2.22992

Geotourism emphasizes the beauty, uniqueness, rarity and wonder of natural phenomena as an impetus for the development of geology-based tourism. The many variations in geological aspects fulfill the potential geodiversity value in the area. The aim of this research is to identify and assess the potential for geodiversity in Oluhuta Village. The research location has coordinates 0° 25' 0" - 0° 27' 0" N and 123° 8' 30" - 125° 10' 30" E. There are several research methods used in the form of field observations, laboratory research, and processing studios. The geological data obtained includes lithology, geomorphology and assessment of geodiversity aspects. The results of the research show that the location of the research area has lithology namely reef limestone and geomorphology namely reef terrace plains. The research area has a site called the Lautan Terangkat Site. This site has geological components including rocks and natural landscapes. Lautan Terangkat site have several assessment criteria with a total number and scientific assessment classification. Scientific value assessment is classified as medium, the educational value assessment is classified as high, tourism value assessment is classified as medium, and the assessment of degradation risk value is classified as low.

Geologi Daerah Buyat Dan Sekitarnya, Kecamatan Kotabunan, Kabupaten Bolaang Mongondow Timur, Provinsi Sulawesi Utara Deden, Mokoagow Deden; Kasim, Muhammad; Hutagalung, Ronal; Akase, Noviar
Journal of Applied Geoscience and Engineering Vol 2, No 2 : Desember 2023
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jage.v2i2.24181

This research focuses on the eastern part of the northern arm of Sulawesi to understand the geological conditions, including geomorphology, lithology, stratigraphy, and geological structure. The goal is to determine the geological history and map the geological conditions to identify potential mineral resources. The research methods include a qualitative approach through field observations such as morphology, outcrop descriptions, lithology, geological structure measurements, stratigraphic relationships, as well as an inventory of natural resources and geological disaster risks. The quantitative approach involves calculations and analyses, including geomorphological analysis, petrography, paleontology, geological structure, stratigraphy, and the reconstruction of geological history. The research results identify four geomorphological units (karst, denudational, volcanic, alluvial) and six geological units at the research site. Andesite and volcanic breccia are the oldest units dating back to the Miocene. At the end of the Miocene, uplift and subsidence formed intrusive hills of diorite and limestone. Volcanic activity ceased in the Miocene. In the Pliocene, sandstone formed due to river transport. The rock formation process continues to the present, with alluvial deposit units resulting from the breakdown of rocks around the lake. Geological structure analysis reveals fault lines with the main stress direction from northwest to southeast. Relative fault data indicates fault inclination values suggesting the main stress direction is northwest-southeast. The geological history in the research area began in the Miocene with magmatism and tectonic activities, forming andesite and volcanic breccia units. This history extends to the formation of alluvial deposit units in the present. The research provides in-depth insights into the geological history and potential mineral resources in the region, serving as a foundation for further research.

GEOLOGY OF PONELO REGION AND SURROUNDINGS, NORTH GORONTALO REGENCY Akase, Noviar; Supriadi, Supriadi
UNM Geographic Journal Volume 5 Nomor 2 September 2022
Publisher : Universitas Negeri Makassar

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.26858/ugj.v1i1.38243

The research area is one of the islands in the District of Ponelo Islands, North Gorontalo Regency, Gorontalo Province. This study aims to determine the geological conditions of the area using the geological mapping method. The results showed that the geomorphology of the study area was divided into 3 units, namely Lava Flow Hills, Denudasional Hills, and Marin Plains. The stratigraphy of the research area is divided into 5 unofficial units sorted from oldest to youngest, namely Sandstone Unit, Conglomerate Unit, Porphyry Andesite Unit, Basalt Lava Flow Unit (Late Pliocene-Early Pleistocene), and Coastal Sediment Unit (Recent age). The geological structures observed were Shear Fracture, Tension, Sheeting Joint, and Columnar Joint. The geological history of the research area starts from the Late Pliocene to Early Pleistocene where the Lokodidi Formation and Pinogu Volcano Formation were formed, resulting in sandstone and conglomerate units (Lokodidi Formation), porphyry andesite units and basalt lava flow units (Pinogu Volcano Formation). Then the alluvial deposition process which is still ongoing today is the result of weathering of rocks in the research area.

Co-Authors Abd Kadir Mubarak A Amin Abduh, Alan Gani Ahmad Iryanto Rompo Ahmad Zainuri Ahmad Zainuri Ana Saputri R Yahya Antoni, Isan Arifin, Yayu Aris, Ayub Pratama Cindi Claudia Male Dachi, Mirdayanti Dai, Elan Daud Yusuf Deden, Mokoagow Deden Dhea Amelia A. Banteng Djamal Adi Nugroho Uno Ente, Amargio Saputro Fandji Marfian Fauzia Hambali Fitryane Lihawa Hamid, Rinto Saputra Hermawan, Riki Hidayansya, Taufik Hutagalung, Ronal Indriati Arifin, Yayu Intan Noviantari Manyoe Irene Ester Wowiling Irmawati Irmawati Irwan Muis K Badaun, Nur Azizah Kayambo, Muhammad Ridho Lahay, Muamart Lasahido, Moh. Syach L. M. Iqbal Liayong Pratama Male, Cindi Claudia Mamonto, Ahmad Firly Mamonto, Fajri Kurniawan Moehammad Jasim Agi Saputra Moh. Nazer Ismail Mohamad Nazer Ismail Mokodompit, I Gede Wahyu Muh Kasim Muhammad Iqbal Asiki Muhammad Kasim Muis, Irwan Mutiara Nonsi Nonsi, Mutiara Nurahman, Ikwan Nurmuhniyanti M. Hubaib Pade, Dwi Ziana Jamila Pakaya, Siti Aqdawiya Panai, Irdiansyah Paputungan, Ulfanna Permana, Aang Panji Ponto, Nadia Fransisca Puhi, Rian Puhi, Riyan Putra, Moh. Bahrul Zaman Momidu Rachman, Arianzah Rizki Rahman, Adisty S. Rauf, Jayanti Rivai, Alya Sri Andini Rizky Hizrah Wumu Robot, Ladya Cheryl Ronal Hutagalung Rusdi, Infithar Hi Sahidah, Aril A.H Sino, Widya Indriani H. Siti Fatimah Sri Maryati Sri Maryati Sri Maryati Sri Maryati Suma, Muhamad Danial Sumarjis, Suly Ayu Sune, Nawir Supriadi Supriadi Syahrizal Koem Tangkudung, Latifa Umar Zulkarnain Bakkar Yani, Lisra Yayu Indriati Arifin

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