Interpretasi Potensi Massa Longsoran Dengan Metoda Geolistrik(Studi Kasus Daerah Gayo Lues)
One indication of a potential landslide area is a formation along the slip field slope. The slope is formed due to the difference between the cover layers (top soil) with a layer beneath it. The top layer is usually a layer of soil that passes the water so that it could be easily infiltrated into th...
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| Format: | Article |
| Language: | English |
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Universitas Syiah Kuala
2015-09-01
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| Series: | Jurnal Natural |
| Online Access: | http://www.jurnal.unsyiah.ac.id/natural/article/view/4345 |