Official Journal of the Asia Oceania Geosciences Society (AOGS)
From: Landslide susceptibility assessment using frequency ratio model in Bogor, West Java, Indonesia
Conditioning factors | Area total (pixel) | Landslide points (n) | Class density | Map density | FR |
---|---|---|---|---|---|
Lithology | Â | Â | Â | Â | 36.865360 |
 a: Andesite with oligoclase–andesine, augite, hypersthene, and hornblende | 942 | 1 | 0.00106 | 0.00022 | 4.8679 |
 ab: Andesite and Basalt | 68 | 0 | 0 | 0.00022 | 0 |
 ha: Hornblende andesite | 4920 | 0 | 0 | 0.00022 | 0 |
 l aut: mainly stream deposits | 482 | 0 | 0 | 0.00022 | 0 |
 qd: Quart diorite | 302 | 0 | 0 | 0.00022 | 0 |
 Tmcb: polymict breccia with fragments of basalt–andesite and coralline limestone | 3703 | 5 | 0.00135 | 0.00022 | 6.19169 |
 Qvb: Volcanic breccia (Breccia, andesitic–basaltic, locally agglomerate) | 7074 | 8 | 0.00113 | 0.00022 | 5.18582 |
 Qvk: Blocks of andesitic tuff and andesitic breccia with abundant pyroxene phenocrysts and basaltic lava | 26,094 | 21 | 0.0008 | 0.00022 | 3.69039 |
 Qvas: Sudamanik formation, andesite | 3913 | 3 | 0.00077 | 0.00022 | 3.51564 |
 Qvt: Pumiceous tuff | 1393 | 1 | 0.00072 | 0.00022 | 3.29186 |
 Qvpo: Older deposits, lahar and lava, andesitic basalt, with oligoclase-andesine, labradorite, olivine, pyroxene, and hornblende | 42,960 | 22 | 0.00051 | 0.00022 | 2.34829 |
 Msc: Mainly claystone containing beds and modules of hard marly limestone, marl, and dark gray limestone | 3248 | 1 | 0.00031 | 0.00022 | 1.41181 |
 Qpv: Endut volcanics (volcanic breccia, lava, and tuff) | 49,609 | 13 | 0.00026 | 0.00022 | 1.20164 |
 Tmtb: Tuff and Breccia: Pumiceous tuff, tuffaceous breccia (andesitic), tuff sandstone, tuffaceous clay with silicified wood and plant remains | 4810 | 1 | 0.00021 | 0.00022 | 0.95334 |
 Qv: Volcanic breccia, agglomerate and tuff | 24,120 | 5 | 0.00021 | 0.00022 | 0.95057 |
 Tmj: Jatiluhur formation (marl and clayey shale, and quartz sandstone intercalation) | 45,197 | 9 | 0.0002 | 0.00022 | 0.91312 |
 Qvsb: Lahar, tuffaceous breccia and lapilli, basaltic andesite in composition | 37,331 | 6 | 0.00016 | 0.00022 | 0.73701 |
 Tmb: Bojongmanik formation (sandstone, pumiceous tuff, marl with molluscs, limestone, claystone with bituminous clay and lignite intercalations and resin fragments | 53,343 | 7 | 0.00013 | 0.00022 | 0.60174 |
 Qav: Alluvium fans (mainly silt, sandstone, gravel and boulders from Quaternary volcanic rocks) | 94,297 | 11 | 0.00012 | 0.00022 | 0.53492 |
 Qvst: Sandy pumiceous tuff | 19,529 | 2 | 0.0001 | 0.00022 | 0.46962 |
 Tpg: Kaliglagah formation, consists of coarse sandstone, conglomerate, claystone and marl | 16,835 | 0 | 0 | 0.00022 | 0 |
 Qa: Alluvium (clay, silt, gravel and boulders) | 16,261 | 0 | 0 | 0.00022 | 0 |
 Qos: Tuffaceous sandstone and conglomerate | 13,328 | 0 | 0 | 0.00022 | 0 |
 Tmk: Klapanunggal formation, mainly reefal limestone with foraminifers, molluscs and echinoderms | 11,826 | 0 | 0 | 0.00022 | 0 |
 Qvsl: Lava flow, basaltic andesite with pyroxene | 9007 | 0 | 0 | 0.00022 | 0 |
 Qoa: Older alluvium (river conglomerates and sands of andesitic and basaltic composite) | 7101 | 0 | 0 | 0.00022 | 0 |
 Mdm: Jatiluhur formation, marl and quartz sandstone | 6947 | 0 | 0 | 0.00022 | 0 |
 Qaf: Clayey sand and peaty clay (floodplain deposits) | 4739 | 0 | 0 | 0.00022 | 0 |
 Tmbc: Bentang formation (tuffaceous sandstone with pumice and lignite, tuffaceous marl, tuffaceous shale, and calcareous conglomeratic breccia) | 4680 | 0 | 0 | 0.00022 | 0 |
 Qvep: Gunung Endut-Prabakti Lava, containing oligoclase-andesine, hypersthene and hornblende | 4438 | 0 | 0 | 0.00022 | 0 |
 Qvl: Volcanic lava (lava flow) basaltic with labradorite, pyroxene, and hornblende | 3062 | 0 | 0 | 0.00022 | 0 |
 Tmkt: Tuff (tuffaceous breccia, tuffaceous sandstone, tuffaceous claystone) | 1756 | 0 | 0 | 0.00022 | 0 |
 Qvba: Basalt lava flow of Gegerbentang mountain | 1690 | 0 | 0 | 0.00022 | 0 |
 Tpss: Alternating conglomerate, sandstone, siltstone, and claystone with plant material–pumice conglomerate, pumice tuff | 1154 | 0 | 0 | 0.00022 | 0 |
 Tms: Saraweh formation, claystone, sandstone, marl, and tuff | 1052 | 0 | 0 | 0.00022 | 0 |
 Tmrs: Rengganis formation, fine–coarse-grained sandstone, conglomerate and claystone | 954 | 0 | 0 | 0.00022 | 0 |
 Tmbl: Limestone member of the Bojongmanik formation, containing molluscs | 860 | 0 | 0 | 0.00022 | 0 |
 Tmqd: Quartz diorite, quartz monzonite, micro quartz diorite, diorite and gabbro | 824 | 0 | 0 | 0.00022 | 0 |
 Tmpb: Bentang formation (tuffaceous sandstone, sandstone, calcareous sandstone, conglomerate, volcanic breccia, tuff, tuffaceous claystone, tuff breccia, calcareous breccia, limestone, claystone, lignite intercalations) | 640 | 0 | 0 | 0.00022 | 0 |
 Tmc: Cimandiri formation, interbedded light to medium gray claystone and siltstone, and yellowish sandstone in places calcareous | 480 | 0 | 0 | 0.00022 | 0 |
 Tmda: Dacite | 421 | 0 | 0 | 0.00022 | 0 |
 Tmp: Pemali formation (globigerina marls, bluish gray and grayish green) | 276 | 0 | 0 | 0.00022 | 0 |
 Tma: Andesite, hornblende andesite, hypersten andesite, basalt, diabase and propylitized andesite | 124 | 0 | 0 | 0.00022 | 0 |
 Tba: Andesite | 92 | 0 | 0 | 0.00022 | 0 |
 Qbr: Coarse sand with mollusc shell | 2 | 0 | 0 | 0.00022 | 0 |
 Mttc: Cantayan formation, claystone, tuffaceous shale | 31 | 0 | 0 | 0.00022 | 0 |
 Mttb: Cantayan formation, polymict breccia with basaltic, andesitic, and coralline limestone components | 11 | 0 | 0 | 0.00022 | 0 |
Slope gradient | Â | Â | Â | Â | 8.06515 |
 Flat (percentage 0–3 %, slope degree < 2) | 63,618 | 6 | 0.00009 | 0.00022 | 0.43248 |
 Undulating (percentage 3–8 %, slope degree 2–5) | 97,995 | 10 | 0.0001 | 0.00022 | 0.46794 |
 Moderately sloping (percentage 8–15 %, slope degree 5–8) | 93,283 | 13 | 0.00014 | 0.00022 | 0.63905 |
 Hilly (percentage 15–30 %, slope degree 8–17) | 161,969 | 45 | 0.00028 | 0.00022 | 1.27401 |
 Moderately steep (percentage 30–45 %, slope degree 17–24) | 60,095 | 16 | 0.00026 | 0.00022 | 1.22088 |
 Steep (percentage 45–65 %, slope degree 24–33) | 41,608 | 21 | 0.0005 | 0.00022 | 2.31438 |
 Very steep (percentage > 65 %, slope degree > 33) | 13,358 | 5 | 0.00037 | 0.00022 | 1.71641 |
Slope aspect | Â | Â | Â | Â | 9.99447 |
 South | 46,242 | 18 | 0.00039 | 0.00022 | 1.78496 |
 Southwest | 51,905 | 14 | 0.00027 | 0.00022 | 1.23683 |
 East | 56,071 | 15 | 0.00027 | 0.00022 | 1.22672 |
 Northeast | 72,939 | 17 | 0.00023 | 0.00022 | 1.06876 |
 North | 32,020 | 7 | 0.00022 | 0.00022 | 1.00247 |
 West | 57,480 | 12 | 0.00021 | 0.00022 | 0.95732 |
 North | 50,650 | 10 | 0.00019 | 0.00022 | 0.90534 |
 Northwest | 69,926 | 13 | 0.00019 | 0.00022 | 0.85251 |
 Southeast | 53,517 | 6 | 0.00011 | 0.00022 | 0.51410 |
 Flat | 41,176 | 4 | 0.0001 | 0.00022 | 0.44546 |
Land cover | Â | Â | Â | Â | 14.32469 |
 Shrubs | 4469 | 8 | 0.00179 | 0.00022 | 8.20867 |
 Settlement | 76,140 | 25 | 0.00033 | 0.00022 | 1.50563 |
 Plantations | 24,843 | 6 | 0.00024 | 0.00022 | 1.10749 |
 Dryland agriculture | 186,799 | 45 | 0.00024 | 0.00022 | 1.10467 |
 Mixed dryland agriculture with shrubs | 76,950 | 18 | 0.00023 | 0.00022 | 1.07265 |
 Industrial plantation forest | 44,441 | 7 | 0.00016 | 0.00022 | 0.72228 |
 Secondary dryland forest | 52,114 | 6 | 0.00011 | 0.00022 | 0.52795 |
 Rice fields | 60,854 | 1 | 0.00002 | 0.00022 | 0.07535 |
 Primary dryland forest | 1618 | 0 | 0 | 0.00022 | 0 |
 Mining | 1535 | 0 | 0 | 0.00022 | 0 |
 Open land | 1391 | 0 | 0 | 0.00022 | 0 |
 Water bodies | 772 | 0 | 0 | 0.00022 | 0 |
Soil | Â | Â | Â | Â | 17.01816 |
 Latosols | 18,951 | 18 | 0.00095 | 0.00022 | 4.35546 |
 Association of reddish brown latosols and brown latosols | 37,640 | 25 | 0.00066 | 0.00022 | 3.04567 |
 Yellow podzolic soils | 18,469 | 9 | 0.00049 | 0.00022 | 2.23456 |
 Complex of yellowish red latosols, reddish brown latosols and litosols | 80,415 | 32 | 0.0004 | 0.00022 | 1.82476 |
 Association of brown latosols and yellowsih brown latosols | 16,244 | 6 | 0.00037 | 0.00022 | 1.69376 |
 Complex of yellowish red latosols and yellowish red podzolic soils | 16,269 | 4 | 0.00025 | 0.00022 | 1.12744 |
 Association of brown latosols and regosols | 39,668 | 9 | 0.00023 | 0.00022 | 1.04039 |
 Andosols | 5911 | 1 | 0.00017 | 0.00022 | 0.77577 |
 Yellowish red podzolic soils | 54,838 | 9 | 0.00016 | 0.00022 | 0.75258 |
 Alluvial soils | 48,106 | 1 | 0.00002 | 0.00022 | 0.09532 |
 Association of red latosols, reddish brown latosols | 126,593 | 2 | 0.00002 | 0.00022 | 0.07245 |
 Grumusols | 27,071 | 0 | 0 | 0.00022 | 0 |
 Red podzolic soils | 17,625 | 0 | 0 | 0.00022 | 0 |
 Regosols | 14,477 | 0 | 0 | 0.00022 | 0 |
 Association of andosol and regosols | 3789 | 0 | 0 | 0.00022 | 0 |
 SNG | 3330 | 0 | 0 | 0.00022 | 0 |
 Association of yellow podzolic and gray hydromorphic soils | 2530 | 0 | 0 | 0.00022 | 0 |
Distance to lineament | Â | Â | Â | Â | 7.59769 |
 0–250 | 119,883 | 17 | 0.00007 | 0.00022 | 0.31240 |
 250–500 | 73,939 | 36 | 0.0003 | 0.00022 | 1.37701 |
 500–750 | 40,116 | 36 | 0.00049 | 0.00022 | 2.23266 |
 750–1000 | 24,395 | 19 | 0.00047 | 0.00022 | 2.17185 |
 1000–1250 | 249,533 | 8 | 0.00031 | 0.00022 | 1.50377 |
 1250–1500 | 15,281 | 0 | 0 | 0.00022 | 0 |
 1500–1750 | 6219 | 0 | 0 | 0.00022 | 0 |
 1750–2000 | 1820 | 0 | 0 | 0.00022 | 0 |
 2000–2250 | 495 | 0 | 0 | 0.00022 | 0 |
 2250–2500 | 204 | 0 | 0 | 0.00022 | 0 |
 2500–2750 | 41 | 0 | 0 | 0.00022 |  |
Rainfall intensity | Â | Â | Â | Â | 5.12200 |
 > 5000 mm/year | 56,380 | 17 | 0.0003 | 0.00022 | 1.38266 |
 4000–5000 mm/year | 87,057 | 30 | 0.00034 | 0.00022 | 1.58019 |
 3500–4000 mm/year | 163,804 | 49 | 0.0003 | 0.00022 | 1.37172 |
 3000–3500 mm/year | 129,119 | 18 | 0.00014 | 0.00022 | 0.63926 |
 2500–3000 mm/year | 61,896 | 2 | 0.00003 | 0.00022 | 0.14817 |
 < 2500 mm/year | 33,670 | 0 | 0 | 0.00022 | 0 |