KA]IAN SPASIAL GERAKAN TANAH DI KP. BARU, DESA CILOTO, KAB. CIANJUR
Slope movement is a natural phenomenon that occurs on uncompact soil on water saturated slope. In Indonesia, this phenomenon mostly found as creep and landslide. The research uses spatial study to observe slope movement phenomenon that foccused on vertical movement quantity and movement course. The...
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id-itb.:20252004-10-25T18:15:00ZKA]IAN SPASIAL GERAKAN TANAH DI KP. BARU, DESA CILOTO, KAB. CIANJUR SUPRIATNA, ATIP Indonesia Theses INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/2025 Slope movement is a natural phenomenon that occurs on uncompact soil on water saturated slope. In Indonesia, this phenomenon mostly found as creep and landslide. The research uses spatial study to observe slope movement phenomenon that foccused on vertical movement quantity and movement course. The research conducted at Kampung Baru, Desa Ciloto, Kabupaten Cianjur, Propinsi Jawa Barat. Two degrees polynomial regression analysist is used to analyze the corelation between a movement period to another period. The result of the research shows that the average vertical velocity movement of the active zone is 0,1269 m/year and tehe stable zone is 0,0281 m/year. Generally, the course of the movement is south east towards Cijember River. Trigerring factor of the movement that have significant impact is the increasing of the water intensity that caused by rainfall and water infilltration. text |
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Indonesia Indonesia |
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Indonesia |
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Slope movement is a natural phenomenon that occurs on uncompact soil on water saturated slope. In Indonesia, this phenomenon mostly found as creep and landslide. The research uses spatial study to observe slope movement phenomenon that foccused on vertical movement quantity and movement course. The research conducted at Kampung Baru, Desa Ciloto, Kabupaten Cianjur, Propinsi Jawa Barat. Two degrees polynomial regression analysist is used to analyze the corelation between a movement period to another period. The result of the research shows that the average vertical velocity movement of the active zone is 0,1269 m/year and tehe stable zone is 0,0281 m/year. Generally, the course of the movement is south east towards Cijember River. Trigerring factor of the movement that have significant impact is the increasing of the water intensity that caused by rainfall and water infilltration. |
| format |
Theses |
| author |
SUPRIATNA, ATIP |
| spellingShingle |
SUPRIATNA, ATIP KA]IAN SPASIAL GERAKAN TANAH DI KP. BARU, DESA CILOTO, KAB. CIANJUR |
| author_facet |
SUPRIATNA, ATIP |
| author_sort |
SUPRIATNA, ATIP |
| title |
KA]IAN SPASIAL GERAKAN TANAH DI KP. BARU, DESA CILOTO, KAB. CIANJUR |
| title_short |
KA]IAN SPASIAL GERAKAN TANAH DI KP. BARU, DESA CILOTO, KAB. CIANJUR |
| title_full |
KA]IAN SPASIAL GERAKAN TANAH DI KP. BARU, DESA CILOTO, KAB. CIANJUR |
| title_fullStr |
KA]IAN SPASIAL GERAKAN TANAH DI KP. BARU, DESA CILOTO, KAB. CIANJUR |
| title_full_unstemmed |
KA]IAN SPASIAL GERAKAN TANAH DI KP. BARU, DESA CILOTO, KAB. CIANJUR |
| title_sort |
ka]ian spasial gerakan tanah di kp. baru, desa ciloto, kab. cianjur |
| url |
https://digilib.itb.ac.id/gdl/view/2025 |
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1820663134009950208 |