陳有蘭溪四個小流域崩塌與土石流發生頻率之研究

dc.contributor國立臺灣師範大學地理學系zh_TW
dc.contributor.author張瑞津zh_TW
dc.contributor.author沈淑敏zh_TW
dc.contributor.author劉盈劭 zh_TW
dc.date.accessioned2015-11-17T08:52:27Z
dc.date.available2015-11-17T08:52:27Z
dc.date.issued2001-05-01
dc.description.abstractThe Chenyulan river basin, located in central Taiwan, is characterized by frequent landslides and debris flows. The catastrophic hazards, especially that induced by typhoon Herb in 1996, have drawn great concerns islandwide. It is believed that a better understanding on the spatial and temporal distribution of these rapid geomorphic changes (i.e., landslides and debris flows) over longer time span will be very helpful on risk assessment and hazard mitigation in this region. The method applied was to make a thorough examination of 17~29 versions of aerial photographs (ranging from 1951 to 2000) of four selected small catchments located in the northern part of the Chenyulan basin (i.e., Tzuzaichiao, Shanganchiao, Peiputzai, and Fengchiu catchment). According to the frequency of landslides and debris flows which identified from available photographs over last 50 years, the Shanganchiao catchment is the least responsive to external inducing events among four catchments, while the Fengchiu catchment is the most, which has experienced six debris flow events over the period.en_US
dc.identifierntnulib_tp_B0414_01_010
dc.identifier.issn1019-6684
dc.identifier.urihttp://rportal.lib.ntnu.edu.tw/handle/20.500.12235/75870
dc.languagezh_TW
dc.publisher國立臺灣師範大學地理學系zh_TW
dc.relation國立臺灣師範大學地理研究報告,34,63-83。zh_TW
dc.subject.other陳有蘭溪zh_TW
dc.subject.other崩塌zh_TW
dc.subject.other土石流zh_TW
dc.subject.otherLandslidesen_US
dc.subject.otherDebris flowsen_US
dc.subject.otherTyphoon eventsen_US
dc.subject.otherGeomorphic sensitivityen_US
dc.subject.otherThe Chenyulan Riveren_US
dc.title陳有蘭溪四個小流域崩塌與土石流發生頻率之研究zh_TW
dc.titleA Study on the Occurrence of Landslides and Debris Flows in Four Small Catchments of the Chenyulan Riveren_US

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