Based on Presidential Regulation Number 43 of 2019, the Ministry of PublicWorks and Public Housing through the Aceh Regional Settlement Infrastructure Center continues to accelerate the rehabilitation of schools/madrasahs' infrastructure. Aceh Besar Regency has an educational infrastructure totaling 376 public schools/madrasahs, including in the outermost (border) area. This research aims to identify and analyze the assessment of the condition of schools/madrasahs' infrastructure, as well as analyze the priorities for handling the rehabilitation and renovation of schools/madrasahs in Aceh Besar Regency. This study used a mixed-methods method where questionnaires were used as population and instrument determinations through observation and surveys. Samples were obtained from 79 public schools/madrasahs in Aceh Besar Regency. The processing techniques were carried out on 31 public schools/madrasahs identified as severely/moderately damaged, an analysis of the level of damage to schools/madrasahs based on the Circular Letter of the Directorate General of Cipta Karya Number 47 of 2020. The sampling technique used is Purposive Sampling with considerations based on stakeholders. Respondents were determined as many as 6 stakeholders in the field of infrastructure. The criteria reviewed are state schools/madrasahs, have at least 1 classroom heavily/moderately damaged, are in a 3T area or developing village (lagging, frontier, and outermost), are in state-owned locations/lands (recorded in state assets), are not currently receiving funding assistance, non-permanent buildings, and the number of students/i. The data analysis technique is used Multi-Criteria Analysis. The results showed that the dominant criterion that needs to be considered in handling the rehabilitation and renovation of schools/madrasahs infrastructure in Aceh Besar Regency is the criteria for state schools/madrasahs. The priority for handling is SMPN 2 Lembah Seulawah as priority 1, SDN Bak Sukon as priority 2, SMPN 1 lembah Seulawah as priority 3, SMPN 3 Kuta Cot Glie as priority 4, SDN Lamcot as priority 5.

The study aims to determine differences in the achievement of students who pass the National Selection of State Universities (SNMPTN), the Selection of Joint Entrance State University (SBMPTN), and the Joint Entrance examination (UMB) at the Faculty of Teachers Training and Education (FKIP) at the University of Syiah Kuala. The study used descriptive method with a quantitative approach. The population in this study were all FKIP Unsyiah students entering university in 2013 that passed the SNMPTN, SBMPTN, and UMB. The population pool was as many as 1,038 students, with 289 students selected for the sample using the Proportionate Stratified Random Sampling technique. The One Way Anova Test was used for data analysis followed by a Least Significance Difference (LSD) test. Hypothesis in this research is there are differences in the achievement of FKIP Unsyiah students passed through SNMPTN, SBMPTN, and UMB. The results showed that the achievement of FKIP Unsyiah students who passed through the SBMPTN had average GPAs of 3.46, 3.32 for the SNMPTN and 3.36 for the UMB. Based on the results, it can be concluded that students who pass the SBMPTN had greater achievement than student who pass the SNMPTN and UMB.

Geureudong Volcano area, Bener Meriah, has the potential to be developed as a renewable energy source. Analysis of the distribution of geothermal manifestations can be done with remote sensing techniques and direct measurement. Furthermore, information on geomorphological conditions, surface temperature, and geothermal potential distribution can be known based on the density value on the FFD (Fault Fracture Density) map and satellite image processing results. Data processing uses ArcGIS and ENVI software concerning geothermal manifestations. The analysis was performed by converting DEMNAS data to a hillshade for drawing straightness structures related to the fault. Image data processing to obtain vegetation density (NDVI), hydrological state (NDWI), and surface temperature distribution (LST). NDWI values are inversely proportional to NDVI. The LST value depends on the density of the vegetation; the higher the vegetation density, the lower the surface temperature. The FFD map is divided into three levels i.e. low (0-0.17 km/km2), moderate (0.17-0.47 km/km2) and high (0.47-1.2 km/km2). The distribution of geothermal potential is at medium and high-density levels, including the Silih Nara, Wih Pesam, and Pintu Rime Gayo areas. The straightness direction is in the north-south and southeast-northwest positions. Based on the NDVI, NDWI, and LST map analysis results, geothermal energy distribution has a rare to moderate vegetation density with surface temperatures ranging from 25.8oC-39.6oC. The result clearly shows that the Geureudong geothermal distribution is initial information before in situ exploration is carried out.Abstrak: Gunung berapi Geureudong, Bener Meriah, sangat prospektif untuk dikembangkan terutama sebagai sumber energi terbarukan. Analisis sebaran manifestasi panas bumi dapat dilakukan dengan teknik penginderaan jauh dan pengukuran langsung. Informasi geomorfologi, temperatur permukaan dan sebaran potensi panas bumi dapat diketahui berdasarkan nilai densitas pada peta FFD (Fault and Fracture Density) dan hasil pengolahan citra satelit Landsat 8. Pemrosesan data menggunakan perangkat lunak ArcGIS dan ENVI yang terkait dengan manifestasi panas bumi. Analisis dilakukan dengan mengubah data DEMNAS menjadi hillshade untuk menggambar struktur kelurusan yang berhubungan dengan sesar. Pengolahan data citra untuk mendapatkan kerapatan vegetasi (NDVI), keadaan hidrologi (NDWI) dan distribusi suhu permukaan (LST). Nilai NDWI berbanding terbalik dengan NDVI. Nilai LST tergantung pada kerapatan vegetasi, semakin tinggi kerapatan vegetasi maka semakin rendah suhu permukaan. Peta FFD dibagi menjadi tiga tingkatan; rendah (0-0,17 km/km2), sedang (0,17-0,47 km/km2) dan tinggi (0,47-1,2 km/km2). Sebaran potensi panas bumi berada pada tingkat kepadatan sedang dan tinggi, meliputi kawasan Silih Nara, Wih Pesam dan Pintu Rime Gayo. Arah kelurusan berada pada posisi utara-selatan dan tenggara-barat laut. Berdasarkan hasil analisis peta NDVI, NDWI dan LST didapatkan bahwa sebaran energi panas bumi memiliki kerapatan vegetasi jarang hingga sedang dengan temperatur permukaan berkisar antara 25.8oC-39.6oC.Hasil yang diperolehkan menunjukkan bahwa sebaran panas bumi Geureudong dengan sangat jelas tergambar sebagai informasi awal sebelum dilakukan eksplorasi lapangan (in situ).