The Effectiveness of Outdoor Learning in Improving Spatial Intelligence

Amaluddin, La Ode; Rahmat, Rahmat; Surdin, Surdin; Ramadhan, M I; Sejati, Andri Estining; Hidayat, Dayat; Saputra, I Gede Purwana Edi; Fayanto, Suritno

doi:10.17478/jegys.613987

Cited by 14 publications

(13 citation statements)

References 19 publications

(13 reference statements)

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“…Proses belajar yang baik adalah siswa lebih aktif daripada guru, karena proses pembelajaran seperti ini lebih menarik dan materi lebih mudah dipahami . Pendekatan yang cenderung menempatkan peserta didik sebagai penerima informasi (pasif) dan guru sebagai pemberi informasi dapat meminimalkan aktivitas peserta didik dalam pembelajaran, karena siswa yang berada dalam ranah berpikir aktif sudah berada di kemampuan berpikir analitis sesuai pemecahan masalah (Fayanto et al, 2019). Berdasarkan observasi awal di SMP Negeri 3 Leihitu, pendekatan metode pembelajaran yang digunakan masih cenderung pada metode ceramah dan pemberian tugas.…”

Section: Pendahuluanunclassified

Efektifitas Penggunaan Metode Problem Solving Dalam Mencapai Hasil Belajar Fisika SMP Negeri 3 Leihitu

Latukau¹,

Saputra²,

L³

et al. 2021

AL-KHAZINI

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Penelitian ini dilakukan dalam upaya meningkatkan kualitas hasil belajar peserta didik di SMP Negeri 3 Leihitu dengan menerapkan metode Problemm Solving. Problem Solving yang diterapkan dalam penelitian ini lebih menekankan kemampuan peserta didik dalam menghadapi masalah dan menentukan solusi penyelesaian masalah. Peserta didik dipacu untuk kreatif, aktif dan tanggap terhadap masalah-masalah yang berkaitan dengan mata pelajaran fisika khususnya materi Gaya. Jenis penelitian yang digunakan adalah penelitian deskriftif. Sampel penelitian ini adalah siswa kelas VIII1 yang berjumlah 30 orang siswa. Efektifitas dari pembelajaran pada penelitian ini dapat diketahui setelah di lakukan analisis terhadap hasil tes yakni pre test dan post test. Efektifitas pencapaian standar kompetensi siswa dianalisis dengan menggunakan uji-t. Setelah melakukan analisis data diperoleh hasil bahwa pembelajaran dengan metode problem solving sangat efektifitas karena melalui uji-t dimana nilai thit lebih besar 22,13 yang di peroleh melalui nilai ttab sebesar 2,042. Sedangkan pada aspek kognitif, aspek afektif, dan aspek psikomotor siswa dengan metode ini terlihat bahwa tingkat penguasaan meningkat secara signifikan dengan presentase ketuntasan sebesar 96,66%.

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Section: Pendahuluanunclassified

Efektifitas Penggunaan Metode Problem Solving Dalam Mencapai Hasil Belajar Fisika SMP Negeri 3 Leihitu

Latukau¹,

Saputra²,

L³

et al. 2021

AL-KHAZINI

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“…According to (Idrus et al, 2014) regional geological map performs as a complement in analyzing the metamorphic rock complex. According to (Amaluddin et al, 2019;Nursalam et al, 2019) geological and geography maps are functioning as additional and instant information for research. The research instruments is described in the table 1 below.…”

Section: Methodsmentioning

confidence: 99%

The Facies and Metamorphism Types Determination of Metamorphic Rock in The Part of Mekongga Complex

Musnajam¹,

Karim²,

Nurfadillah³

et al. 2020

Geos. Ind.

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Lambolemo Village is geomorphologically dominated by hilly slopes morphology. Lithology in the form of metamorphic rocks are mica schists and chlorite schists. The present research aimed to determine the facies and metamorphism types of metamorphic rocks in Lambolemo Village. The research methods engaged were field observation and laboratory observation utilizing petrographic analysis. Observations stage generated texture data and set of mineral both macroscopically and microscopically. The minerals were discovered within metamorphic rock of the research area, namely: muscovite, quartz, biotite, and chlorite. These findings then classified into two zones, there were chlorite zone and biotite zone. These zones were embodied into greenschist facies with chlorite mineral index. The greenschist facies was characterized with chlorite, albit, epidote, and actinolite minerals appearance. The metamorphic rock had a foliation structure. The structure was commonly generated by a regional metamorphic process, which was particularly a feature of the clear alignment, translucent minerals from flat minerals, such as : mica, chlorite and minerals that obtained fibers or scents. Keywords: Determination; Facies; Metamorfism Type Copyright (c) 2020 Geosfera Indonesia Journal and Department of Geography Education, University of Jember This work is licensed under a Creative Commons Attribution-Share A like 4.0 International License

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“…However, qualitative interpretation using geological and geography maps are used only as additional information. According to (Amaluddin et al, 2019) geological formation or structure for instance can use the maps which poured in the data field or 2D.…”

Section: Methodsmentioning

confidence: 99%

Mapping of Subsurface Geological Structure and Land Cover Using Microgravity Techniques for Geography and Geophysic Surveys: A Case Study of Maluri Park, Malaysia

Nursalam¹,

Arisona²,

Ramli³

et al. 2019

Geosfera Ind.

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A microgravity investigation on bedrock topography was conducted at Maluri park reference level in Kuala Lumpur, Malaysia. The study aim to mapping the near-surface structure and soil and land cover distribution for geography and geophysics surveys. Two types of cross-section modeling of the residual anomaly generated the MaluriBouguer Anomaly model for site-1 and site-2 at Maluri Park. The 2D microgravity models produced the contour map, displaying the characterization due to density contrast in rock types while mapping the subsurface geological structure at different depths. Moreover, a synthetic model was initiated with the assumption of lateral distance on the left and right sides taken at 50 m and a depth of 60 m. The results of modeling confirmed that the soil and rock type composition on both models site tests are topsoil (1.1 to 1.92 g/cm3), soil (1.8 g/cm3), clay (1.63 g/cm3), gravel (1.7 g/cm3), sand (2.0 g/cm3), shale (2.4 g/cm3), sandstone (2.76 g/cm3), and limestone (2.9 g/cm3). The 2D gravity modeling using two model site tests obtained a correspondence with the observed microgravity data. Keywords: Bouguer anomaly, limestone, microgravity, soil structure, topography. References Amaluddin, L. O., Rahmat, R., Surdin, S., Ramadhan, M. I., Hidayat, D. N., Purwana, I. G., & Fayanto, S. (2019). The Effectiveness of Outdoor Learning in Improving Spatial Intelligence. Journal for the Education of Gifted Young Scientists, 7(3), 667–680. https://doi.org/10.17478/jegys.613987 Arisona,A., Mohd N., Amin E.K., &Abdullahi, A.(2018).Assessment of microgravity anomalies of soil structure for geotechnical 2d models.Journal of Geoscience, Engineering, Environment, and Technology (JGEET)3(3), 151-154. Georgsson, L.S. (2009). Geophysical Methotds Used in Geothermal Exploration. Presented at Exploration for Geothermal Resources, 1-22 November 2009, 1-16. Grandjean, G. (2009). From Geophysical Parameters to Soil Characteristics.Florida: Report N°BRGM/FP7-DIGISOIL Project Deliverable 2.1, Final ReportDepartment of Civil and Coastal EngineeringUniversity of Florida. Hiltunen, D.R., Hudyma,N.,Tran,K.T.,&Sarno,A.I. (2012).Geophysical Testing of Rock and Its Relationthipsto Physical Properties.Florida:Final ReportDepartment ofCivil and Coastal EngineeringUniversity ofFlorida. Kirsch,R. (2006).GroundwaterGeophysics, ATool for Hydrogeology.New York: Springer. Kamal,H.,Taha,M.,&Al-Sanad,S. (2010). Geoenvironmental Engineering and Geotechnics, GeoShanghai 2010 International Conference. (accessed 02.03.17) Lilie, R.J. (1999).Whole Earth Geophysics: An Introductory Textbook for Geologists and Geophysicists. New Jersey:Prentice-HallInc. Pringle, J.K., Styles, P., Howell, C.P.,Branston, M.W., Furner, R., &Toon,S.M. (2012). Long-term time-lapse microgravity and geotechnical monitoring of relict salt mines, marston, cheshire, uk. Geophysic77(6), 165-171. Samsudin, H.T.(2003).A microgravity survey over deep limestone bedrock.Bulletin of Geological Society of Malaysia4(6), 201-208. Tan, S.M. (2005). Karsticfeatures of kualalumpur limestone. Bulletin of the Institution of EnginnerMalaysia 4(7), 6-11. Tajuddin, A.&Lat, C.N. (2004).Detecting subsurfacevoids using the microgravity method, a case study from kualalipis, pahang.Bulletin of Geological Society of Malaysia 3(48), 31-35. Tuckwell, G., Grossey, T., Owen, S., & Stearns, P. (2008). The use of microgravity to detect small distributed voids and low-density ground. Quarterly Journal of Engineering Geology and Hydrogeology, 41(3), 371–380. https://doi.org/10.1144/1470-9236/07-224 Wanjohi, A.W. (2014). Geophysical Field Mapping. Presented at Exploration for Geothermal Resources, 2-23 November 2014, 1-9. Yusoff , Z.M., Raju,G. &Nahazanan, H.(2016).Static and dynamic behaviour of kualalumpur limestone. Malaysian Journal of Civil Engineering Special Issue Vol.28 (1), p.:18-25. Zabidi, H. & De Freitas, M.H. (2011).Re-evaluation of rock core logging for the prediction of preferred orientations of karst in the kualalumpur limestone formation. Engineering Geology, 117(3-4), p.: 159–169. Copyright (c) 2019 Geosfera Indonesia Journal and Department of Geography Education, University of Jember This work is licensed under a Creative Commons Attribution-Share A like 4.0 International License

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The Effectiveness of Outdoor Learning in Improving Spatial Intelligence

Cited by 14 publications

References 19 publications

Efektifitas Penggunaan Metode Problem Solving Dalam Mencapai Hasil Belajar Fisika SMP Negeri 3 Leihitu

Efektifitas Penggunaan Metode Problem Solving Dalam Mencapai Hasil Belajar Fisika SMP Negeri 3 Leihitu

The Facies and Metamorphism Types Determination of Metamorphic Rock in The Part of Mekongga Complex

Mapping of Subsurface Geological Structure and Land Cover Using Microgravity Techniques for Geography and Geophysic Surveys: A Case Study of Maluri Park, Malaysia

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