ZONASI DAERAH BAHAYA LONGSOR DI KAWASAN GUNUNG TAMPOMAS KABUPATEN SUMEDANG, JAWA BARAT

Main Author: -, Lucky Lukmantara
Other Authors: Fakultas Teknik Geologi
Format: Article info application/pdf Journal
Bahasa: ind
Terbitan: Fakultas Teknik Geologi Universitas Padjadjaran , 2007
Subjects:
Online Access: http://jurnal.unpad.ac.id/bsc/article/view/8141
http://jurnal.unpad.ac.id/bsc/article/view/8141/3714
Daftar Isi:
  • Research area generally have a big slope. Based on Van Zuidam classification (1983), the research area can be divided into 3 angle class or slope: 1) area which have surging hilly morphology with of slope range from 25 - 35 %, 2) area which have precipitous hilly morphology with slope range from 35 - 90 %, and 3) area which have hilly morphology cut sharply or hilly very precipitous with slope 90 – 150 %Area which including into landslide-zone in generally reside at area which have precipitous hilly and surging hilly morphology, there are at group 2 and 3. Both of the area of compiler rock generally not yet lihtificated powerfully, water content is high enough especially in rain season and rock generally relative soften