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Identifikasi Kualitas Batugamping Berdasarkan Analisis Geokimia dan Petrografi Daerah Pilolodaa Provinsi Gorontalo Paputungan, Ulfanna; Permana, Aang Panji; Akase, Noviar
Journal of Applied Geoscience and Engineering Vol 4, No 1 : Juni 2025
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jage.v4i1.33607

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Gorontalo is one of the provinces with significant limestone potential, particularly in the industrial sector. This study aims to identify the quality of limestone found in the Pilolodaa area and its surroundings. The methods used in this research include petrography to determine the limestone facies and XRF analysis to identify the mineral composition of the rocks. The study area consists of lithologies such as floatstone limestone facies, carbonate sandstone, and alluvial units. The floatstone limestone has a CaO composition greater than 50% and MgO less than 2%, making it highly potential for industrial applications.
Peningkatan Kapasitas Masyarakat Dalam Mengurangi Risiko Bencana Di Desa Bandung Rejo Kabupaten Gorontalo Koem, Syahrizal; Akase, Noviar; Muis, Irwan
Aksiologiya: Jurnal Pengabdian Kepada Masyarakat Vol 3 No 2 (2019): Agustus
Publisher : Universitas Muhammadiyah Surabaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.30651/aks.v3i2.1815

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The community capacity building program in reducing disaster risk aims to realize the Bandung Rejo village as a disaster resilient village. Efforts made to achieve community capacity building include: (1) institutional aspects through the establishment of Disaster Risk Management forums (DRR) and Community Disaster Preparedness Teams (CDPT), (2) aspects of capacity building through dissemination and training in the preparation of disaster management plans and contingency plans , (3) aspects of the implementation of disaster management through a program to create a threat map and create disaster warning signs. The establishment of DRR and CDPT forums has a strategic role in minimizing disaster risk. The results achieved from the socialization and training were the availability of Bandung Rejo village disaster risk analysis document. The document can be a reference in making development policies in the village. Based on the results of the analysis conducted by the forum that Bandung Rejo village had a flood hazard level in the medium category. The results of identification and analysis obtained two flood-prone points that were able to reach agricultural land and facilities and infrastructure facilities. The implementation of community capacity building programs in Bandung Rejo village can provide stimulus to local governments and the public about the importance of disaster anticipation.
Pemetaan Geologi Dalam Mengungkap Potensi Sumber Daya Alam Desa Bonedaa, Suwawa Selatan, Gorontalo Pade, Dwi Ziana Jamila; Akase, Noviar; Hutagalung, Ronal; Dachi, Mirdayanti; Mokodompit, I Gede Wahyu; Tangkudung, Latifa; Ente, Amargio Saputro; Rahman, Adisty S.; Puhi, Rian; Yani, Lisra; Putra, Moh. Bahrul Zaman Momidu; Nurahman, Ikwan
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Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jrpi.v2i3.33435

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The community in Bonedaa Village and its surroundings possesses untapped natural resource potential. This community service aims to enhance public understanding of local geological conditions and natural resources through participatory geological mapping. The methods applied include field education, group discussions, and training on rock and geological structure identification. The results show an increased awareness among residents regarding local rock types, construction material potential, and geological hazards such as landslides and erosion. Participatory mapping produced a simplified geological map useful for village-level planning and decision-making. This activity demonstrates that geological approaches can contribute directly to sustainable resource management and disaster risk reduction. The outcomes are significant in promoting community resilience and independence based on local potential.
Stratigrafi Daerah Sumalata Timur, Kabupaten Gorontalo Utara Rivai, Alya Sri Andini; 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.v2i3.33928

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The research area was located at coordinates 122°28’0’’- 122ᵒ36’0’ N - 0ᵒ52’0’’ - 1ᵒ2’0’ E with an area of 157 km2. Administratively, it is located in Sumalata Timur Subdistrict, North Gorontalo Regency, Gorontalo Province. The methods used in this research were surface geological surveys and laboratory analysis. Surface geological surveys included direct lithological observations at outcrops. Laboratory analysis included petrographic analysis using thin sections. The geologycal mapping aims to knowing the geological condition in East Sumalata. The lithology of the research area consists of 5 units, namely andesite unit, diorite unit, breccia unit, sandstone unit, and coastal sediment unit. The geomorphology of the research area is divided into 3 morphological units, namely the Volcanic Hills Unit, the Denudational Hills Unit, and the Marine Plains Unit.
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

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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
Geomorfologi Daerah Mananggu dan Sekitarnya, Kecamatan Mananggu, Kabupaten Boalemo, Provinsi Gorontalo Kayambo, Muhammad Ridho; Arifin, Yayu; Akase, Noviar; Uno, Djamal Adi Nugroho
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Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jrpi.v3i1.36273

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This research was conducted in the Mananggu area and its surroundings, Mananggu District, Boalemo Regency, Gorontalo Province. The study aims to map the geological conditions and identify the characteristics of geomorphology and geological structures developed in the area. The methods employed included surface geological mapping for field data collection, followed by laboratory analyses. Geomorphologically, the research area is divided into two units: the Volcanic Hills Unit and the Structural Hills Unit. The stratigraphy consists of the Eocene-Oligocene Porphyritic Andesite Unit (Tinombo Formation) and the Pliocene Granite Unit (Bumbulan Granodiorite Formation) acting as an intrusive body. The geological structures are controlled by a transtensional regime resulting from compression, manifested as NW-SE shear joints, right normal slip faults, and normal right slip faults. The landscape evolution is strongly influenced by the interplay between the resistance of the igneous lithologies and the active tectonic deformation that shapes the drainage patterns and slope configurations.
Pemanfaatan Penginderaan Jauh Dalam Bidang Geologi Mamonto, Ahmad Firly; Lahay, Muamart; Hermawan, Riki; Panai, Irdiansyah; Puhi, Riyan; Maryati, Sri; Akase, Noviar; Sune, Nawir
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Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jrpi.v3i1.36195

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This study summarizes various studies on the use of remote sensing technology, both multispectral and radar, in the fields of geology, hydrology, and the environment. The main journals reviewed show that satellite imagery such as Landsat TM, Landsat 8 OLI/TIRS, Sentinel-2, ASTER, and LiDAR radar data play a significant role in identifying the physical characteristics of the earth, such as soil moisture, mineralization, lithology, suspended sediments, and surface deformation due to tectonic activity. The use of multispectral imagery is effective in mapping lithology and minerals, while radar and LiDAR remote sensing excel in morphological analysis, geological structure, and hydrodynamic modelling of flood inundation. Overall, remote sensing has proven to be an efficient, time-saving, and accurate tool in supporting geological resource exploration, topographic mapping, and natural disaster mitigation. The integration of various image data sources increases the validity of interpretation results and can be an important basis for decision-making related to spatial planning, mineral exploration, and environmental management in Indonesia.
Geokimia (XRF) Batuan Andesit Desa Biluhu Barat, Kecamatan Biluhu, Kabupaten Gorontalo Hamid, Rinto Saputra; Arifin, Yayu Indriati; Akase, Noviar
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Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jrpi.v3i1.35897

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This study aims to analyze the geochemical characteristics of andesite rocks within the Tinombo Formation located in Biluhu Barat Village, Biluhu District, Gorontalo Regency. Data collection was conducted through geological mapping and geochemical analysis using X-Ray Fluorescence (XRF) to determine the magma series, magma type, and tectonic setting of the rock origin. The results show that the study area consists of porphyritic andesite and granodiorite units. Geochemical data indicate that the andesite rocks belong to the calc-alkaline magma series, with rock types identified as andesite and basaltic andesite. Geochemical diagrams reveal that the rocks originated from an Island Arc Calc-Alkaline Basalt tectonic setting. The calculated magma source depth ranges from 156 to 164 km, indicating magmatic processes occurring within a subduction zone. This study contributes to a better understanding of the tectonic framework and magmatic evolution in the Gorontalo region. 
Karakteristik Batuan Piroklastik Berdasarkan Analisis Petrografi Daerah Molingkapoto dan Sekitarnya Kabupaten Gorontalo Utara Provinsi Gorontalo Putri Aprilia Matoka; Muhammad Kasim; Noviar Akase
Geosfera: Jurnal Penelitian Geografi Vol 4, No 2 (2025): Geosfera : Jurnal Penelitian Geografi
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/geojpg.v4i2.32267

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Daerah penelitian berlokasi di Molingkapoto dan sekitarnya, Kabupaten Gorontalo Utara, Provinsi Gorontalo. Secara fisiografi, daerah penelitian berada pada zona pegunugan utara di formasi Batuan Gunung Api Bilungala dan Breksi Wobudu. Secara stratigrafi, daerah penelitian terdiri dari batuan berumur tersier hingga kuarter. Tujuan dari penelitian ini adalah untuk mengetahui karakteristik batuan piroklastik daerah penelitian berdasarkan analisis petrografi, dengan menggunakan metode pemetaan lapangan yang merupakan bagian dari pengumpulan data untuk pengolahan data studio, dan metode analisis petrografi yang digunakan untuk pengolahan data laboratorium. Hasil penelitian menunjukkan bahwa daerah penelitian terdiri dari perbukitan aliran piroklastik dan dataran aluvial dengan litologi breksi piroklastik dan tuff yang dimana merupakan produk hasil vulkanisme. Analisis petrografi menunjukkan bahwa matriks dari batuan breksi piroklastik daerah penelitian berjenis tufa kristal  (PA 04) yaitu batuan yang didominasi pecahan -pecahan kristal dan tufa litik (PA 24) yang didominasi pecahan -pecahan atau fragmen batuan sementara batuan tufa berjenis litik tufa (PA 18) yaitu batuan yang didominasi pecahan -pecahan atau fragmen batuan.
Analisis tipe gerakan tanah pada lereng Bendungan Bulango Ulu Kabupaten Bone Bolango menggunakan metode kinematika Moehammad Jasim Agi Saputra; Aang Panji Permana; Noviar Akase
PADURAKSA: Jurnal Teknik Sipil Universitas Warmadewa Vol. 12 No. 2 (2023)
Publisher : Program Studi Teknik Sipil, Fakultas Teknik dan Perencanaan, Universitas Warmadewa

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.22225/pd.12.2.7343.244-249

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The Bulango Ulu Dam is one of the strategic projects built in Tuloa Village, North Bulango District, Bone Bolango Regency, Gorontalo Province. In building a dam, geological analysis and slope stability are very important to avoid the risk of collapse or structural failure. This research aims to conduct geological analysis and slope stability at the Bulango Ulu Dam using kinematics methods. The kinematics method is used to determine the type of ground movement on the dam slope and identify the probability value of failure. Geological data related to lithology, petrography, geological structure and geomorphology are collected through direct observations and in the laboratory. Then, this data is used to determine geological conditions, geological structure and geomorphology which are then interpreted in relation to slope stability. The research results show that the geomorphological units are alluvial plains and low structural hills. The lithology that makes up the slopes of the Bulango Ulu Dam is composed of alluvial units and granodiorite units. The geological structure that develops is in the form of tensile joints in a general direction east-west (E-W) and cut by tension joints in a general direction north-south (N-S). The type and probability of ground movement that occurs based on segment, namely on segment A-B slopes in the form of Wedges (21.65%), segment B-C slopes in the form of Wedges (12.27%), segment E-F slopes in the form of Wedges (15.12%), and segment slopes G-H is a Wedge (21.8%). Based on the results of kinematic and boundary equilibrium analysis, the slopes on the Bulango Ulu dam are in the stable category. This research recommends that there is no need to make changes to the geometry of the dam slope because the slope is in a stable condition.
Co-Authors Abd Kadir Mubarak A Amin Abduh, Alan Gani Agustinus Sosang Ahmad Firli Aprilio Mamonto Ahmad Iryanto Rompo Ahmad Zainuri Ahmad Zainuri Alief Ardiansyah Ana Saputri R Yahya Antoni, Isan Arifin, Yayu Aril A.H Sahidah Aris, Ayub Pratama Cindi Claudia Male Dachi, Mirdayanti Dai, Elan Dana Christina Naomi Mambrasar Daud Yusuf Deden, Mokoagow Deden Dhea Amelia A. Banteng Diwa Ahmad Luly Djamal Adi Nugroho Uno Ente, Amargio Saputro Fandji Marfian Fauzia Hambali Fitryane Lihawa Hamid, Rinto Saputra Hermawan, Riki Hidayansya, Taufik Hutagalung, Ronal Intan Noviantari Manyoe Irene Ester Wowiling Irmawati Irmawati Irwan Muis K Badaun, Nur Azizah Kasim, Muhammad Kayambo, Muhammad Ridho Lahay, Muamart M. Iqbal Liayong Pratama Mamonto, Ahmad Firly Mamonto, Fajri Kurniawan Maryati, Sri Mirdayanti Dachi Mirdayanti Dachi Moehammad Jasim Agi Saputra Moh. Nazer Ismail Moh. Syach L. Lasahido 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 Putri Aprilia Matoka Putri Wulan Rahmawati Rachman, Arianzah Rizki Rahman, Adisty S. Rauf, Jayanti Rivai, Alya Sri Andini Rizky Hizrah Wumu Robot, Ladya Cheryl Ronal Hutagalung Rusdi, Infithar Hi Sino, Widya Indriani H. Siti Fatimah Sri Maryati Suma, Muhamad Danial Sumarjis, Suly Ayu Sune, Nawir Supriadi Supriadi Syahrizal Koem Tangkudung, Latifa Umar Zulkarnain Bakkar Yani, Lisra Yasin Septian Yayu Indriati Arifin