A Study Of Mass Wasting Potential In South-Western Taiwan

碩士 === 國立成功大學 === 地球科學系專班 === 96 === Nine locations in ChiaYee County, Tainan County and Kaoshiung County were selected for mass wasting study. The study includes the field geological surveys such as rock type, attitude of slope and discontinuity (including strata), density of discontinuity; and int...

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Main Authors: HU-TI WEN, 溫湖滴
Other Authors: Ching-Lang Tsai
Format: Others
Language:zh-TW
Published: 2008
Online Access:http://ndltd.ncl.edu.tw/handle/48928165241471314548
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spelling ndltd-TW-096NCKU51350252017-07-09T04:29:44Z http://ndltd.ncl.edu.tw/handle/48928165241471314548 A Study Of Mass Wasting Potential In South-Western Taiwan 坡地崩塌潛感性調查研究-個案分析 HU-TI WEN 溫湖滴 碩士 國立成功大學 地球科學系專班 96 Nine locations in ChiaYee County, Tainan County and Kaoshiung County were selected for mass wasting study. The study includes the field geological surveys such as rock type, attitude of slope and discontinuity (including strata), density of discontinuity; and interpretation of air photography, geology map, morphology map and satellite image. Four indices: ISS ( index of slanting of the slope), IDS( index of down sloping) IV (index of volume of mass wasting by down sloping) and IVDS (index of dangerous mass wasting by down sloping) are calculated to evaluate the mass wasting potential for rocK slope. 5 outcrops are syn-slant slopes, 6 outcrops are anti slant slopes; 3 outcrops are slumped debris. The rocK sliding is the major pattern of mass wasting in syn-slant slopes, while debris fall or rock fall is the major pattern of mass wasting in anti-slant slope. Undercutting by meander is the initiating cause of mass wasting in 4 localities. The mass wasting potential is high in nine localities. Ching-Lang Tsai 蔡金郎 2008 學位論文 ; thesis 134 zh-TW
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description 碩士 === 國立成功大學 === 地球科學系專班 === 96 === Nine locations in ChiaYee County, Tainan County and Kaoshiung County were selected for mass wasting study. The study includes the field geological surveys such as rock type, attitude of slope and discontinuity (including strata), density of discontinuity; and interpretation of air photography, geology map, morphology map and satellite image. Four indices: ISS ( index of slanting of the slope), IDS( index of down sloping) IV (index of volume of mass wasting by down sloping) and IVDS (index of dangerous mass wasting by down sloping) are calculated to evaluate the mass wasting potential for rocK slope. 5 outcrops are syn-slant slopes, 6 outcrops are anti slant slopes; 3 outcrops are slumped debris. The rocK sliding is the major pattern of mass wasting in syn-slant slopes, while debris fall or rock fall is the major pattern of mass wasting in anti-slant slope. Undercutting by meander is the initiating cause of mass wasting in 4 localities. The mass wasting potential is high in nine localities.
author2 Ching-Lang Tsai
author_facet Ching-Lang Tsai
HU-TI WEN
溫湖滴
author HU-TI WEN
溫湖滴
spellingShingle HU-TI WEN
溫湖滴
A Study Of Mass Wasting Potential In South-Western Taiwan
author_sort HU-TI WEN
title A Study Of Mass Wasting Potential In South-Western Taiwan
title_short A Study Of Mass Wasting Potential In South-Western Taiwan
title_full A Study Of Mass Wasting Potential In South-Western Taiwan
title_fullStr A Study Of Mass Wasting Potential In South-Western Taiwan
title_full_unstemmed A Study Of Mass Wasting Potential In South-Western Taiwan
title_sort study of mass wasting potential in south-western taiwan
publishDate 2008
url http://ndltd.ncl.edu.tw/handle/48928165241471314548
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