Face-to-face learning implemented by the government raises parents concerns because theCovid-19 pandemic isn't over yet. The purpose of this community service activity is to increase awareness of health and improve health protocol discipline for Covid-19 prevention inLonuo Village, Tilongkabila Sub District, Bone Bolango Regency. The target of this program is elementary school and kindergarten students. The methods used in this community service program are socialization of the Covid-19 disease,health protocol discipline, distribution of masks, hand sanitizers, and leaflets, practicing good and correct hand washing, and coloring pictures by kindergarten and preschool students. The number of participants in this community service is 80 students in Lonuo Village, Tilongkabila Sub District, Bone Bolango Regency. The implementation of this program raised a positive response from teachers, students and the student’s parents. They need information about COVID-19 and life patterns during the pandemic. This program is expected to reduce parental concerns in re-implementing face-to-face learning. This program is expected to provide benefits for schools in increasing student obedience to comply health protocols.
Economic growth and improvement the quality of life of good rural communities require the availability of adequate infrastructure and social public facilities.Infrastructure development in the village requires good planning, according to the needs of the community and according to the characteristics of each village. The results of field observations in Raku Village showed several findings, namely infrastructure and social public facilities were inadequate, there was no infrastructure distribution map, and the existing maps were not up to date. Mapping of public and social facilities in Raku Village, North Tabukan District, Sangihe Archipelago Regency, North Sulawesi Province is part of the community service activities of the Universitas Negeri Gorontalo Collaborative Real Work Lecture. The mapping of public and social facilities aims to map social public facilities, determine the distribution of public and social facilities, and provide spatial data as a basis for policy making by the government. Mapping of village public and social facilities which are part of this community service activity uses the integration method of field surveys and spatial data analysis. Data collection on the location of public and social facilities was carried out using an Android-based GPS, while information on public and social facilities was collected through interviews with residents. Processing and analysis of field survey data, both spatial data and attribute data, was carried out using the Geographic Information System software application, namely ArcGIS 10.8. The results of the primary data survey on public and social facilities and analysis of spatial data show that the public and social facilities in Raku Village are divided into educational facilities, religious facilities, health facilities, government offices, and other social facilities.
Gorontalo merupakan wilayah yang berada di bagian tengah lengan utara sulawesi. Gorontalo memiliki keterdapatan batuan granit yang tersebar di beberapa tempat. Penelitian ini bertujuan untuk mengetahui kenampakan mikroskopi mineral penyusun batuan granit di daerah pohe. Penelitian ini dilakukan dengan metode pemetaan geologi yang digunakan pada saat observasi dan pengambilan data dilapangan serta metode analisis petrografi dengan menggunakan mikroskop polarisasi Olympus. Ada empat sampel batuan yang di ambil dari lokasi penelitian. Berdasarkan analisa petrografis pada stasiun EF 1, stasiun EF 2, stasiun EF 3, dan stasiun EF 4 menunjukan batuan granit dengan komposisi kuarsa diatas 30%, plagioklas diatas 20%, dan alkali feldspar diatas 15 %. Mineral sekunder yang hadir diseluruh batuan adalah biotit, klorit, dan serisit. Selain itu terdapat tekstur khas pada batuan beku yang ada pada seluruh sayatan berupa tekstur poikilitik sebagai penciri dari fraksionasi kristal. Tekstur mineral yang diamati yaitu tekstur myrmkite diinterpretasikan sebagai proses yang pembekuan magma yang pelan.
Daerah penelitian secara administratif berada di Kecamatan Boliyohuto, Kabupaten Gorontalo, secara fisiografi daerah penelitian berada di lembah paguyaman yang didominasi oleh batuan gunungapi dan endapan danau. Penelitian ini bertujuan untuk mengetahui geologi bawah permukaan daerah Bongonggoayu. Metode yang digunakan dalam penelitian ini menggunakan geolistrik konfigurasi Wenner-Sclumberger. Hasil penelitian geologi bawah permukaan daerah penelitian menggunakan geolistrik Wenner-Schlumberger terbagi atas 4 lintasan berdasarkan pengolahan Res2dinv dan rockword terdapat beberapa lapisan litologi berdasarkan penampang 2D bawah permukaan dimana didominasi oleh lapisan kelompok batupasir, lempung dan pasir kerikil. Kemudian terdapat anomali yang kemungkinan besar pada anomali ini terdapat pengaruh struktur dengan arah barat laut-Tenggara pada lintasan 1 dan lintasan 4.
Secara administratif lokasi penelitian berada di Provinsi Gorontalo terletak antara 0° 19’ – 0° 57’ Lintang Utara dan 121° 23’ – 125° 14’ Bujur Timur. Lokasi penelitian ini terdapat di Desa Oluhuta, Kecamatan Kabila Bone, Kabupaten Bone Bolango, Provinsi Gorontalo. Pada lokasi penelitan yang akan dipetakan hanya seluas 3,1 km2. Pemetaan geologi lanjut ini bertujuan memetakkan keadaan geologi daerah penelitian dengan pendekatan lapangan dan studio. Beberapa metode yang dilakukan meliputi aspek geomorfologi, stratigrafi dan struktur geologi. Hasil penelitian berupa peta kerangka geologi, peta geomorfologi dan peta geologi. Berdasarkan peta Geomorfologi didapatkan 3 satuan bentuk lahan berupa Satuan Dataran Alluvial, Satuan Perbukitan Piroklastik, Satuan Perbukitan Aliran Lava. Pada peta geologi Desa Oluhuta disusun oleh 4 litologi yaitu lava dasit, breksi piroklastik, batugamping wackstone, Aluvial & Endapan Pantai. Hasil dari analisis struktur geologi menghasilkan bahwa arah sesar Sinistral dengan bidang sesar berarah timur laut – barat daya dan diperoleh bidang sesar N2260/42E, slickensides 34°N314E dan pitch 35°, data-data ini kemudian dianalisis dan diperoleh nilai ϭ1 57°N59°E, ϭ2 22°, N287°E, ϭ3 21°, N187°E.
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