坡地災害之發生機制：以溪頭集水區為例─總計畫暨子計畫：坡地土石流發生機制研究
Date Issued
2002
Date
2002
Author(s)
DOI
902625Z002017
Abstract
After the occurrence of Chichi earthquake in 1999, not only the 12,479.72 hectares of new
landslide happened, but also the fragile geological hillside is easier to collapse or separate than
before. These huge sediment deposits located on the upstream creek valley or transporting to
downstream area would largely threaten people who live in downstream area. In order to
mitigate the scale and threatening of debris-flow disaster, this project collected related
literature about debris flow and analyzed the disaster sources of Typhoon Toraji at Hsitou.
Moreover, the experimental content and its procedure are also planned here.
Subjects
Debris flow
Hsitou
Mechanism of occurrence
Publisher
臺北市：國立臺灣大學水工試驗所
Type
report
File(s)![Thumbnail Image]()
Loading...
Name
902625Z002017.pdf
Size
241.72 KB
Format
Adobe PDF
Checksum
(MD5):daa44621af8b2d992f705c974563dacd