Title of article :
Frequency and spatial distribution of landslides in a mountainous drainage basin: Western Foothills, Taiwan
Author/Authors :
Chang، نويسنده , , Jui-chin and Slaymaker، نويسنده , , Olav، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2002
Pages :
23
From page :
285
To page :
307
Abstract :
Maps from 1904 and 1915 and air photographs from 1963, 1980, 1985, 1993 and 1996 provide a record of landslide incidence in a 92.1-km2 drainage basin, a headwater tributary of the Cho-Shui River in Taiwan. Interpretation of landslide patterns from the early maps indicate that in four sub-basins (36 km2) structural geological factors control chronic landsliding regularly reactivated by intense rains. Within these four sub-basins, all later air photographs reveal a continuing high incidence of landslides (with landslide densities of 3–11 ha/km2). Air photographs taken in 1963, following extensive logging, in 1985, following highway construction, and in 1996, following the very large typhoon Herb event demonstrate the short-term effects of disturbance in these structurally weak sub-basins. Air photographs from 1980 and 1993 demonstrate recovery of the land surface from logging and highway construction impacts, respectively. For the adjacent sub-basins (56 km2), two modes of response to perturbations were identified: six sub-basins (48 km2) showed direct response to logging, road construction and typhoon Herb and five sub-basins (8 km2) were more buffered and showed some lagged responses. Even this last category of sub-basins is more active than the average for Taiwan, where the mean landslide density is 0.84 ha/km2. It is proposed that, for the 92.1-km2 Hoshe basin, the ‘formative event’ sensu Brunsden [Z. Geomorphol. Suppl. 79 (1990) 1] is one that produces approximately 200 ha of landslides, a value that has been equaled or exceeded in each of the periods of study (1963–1980, 1980–1985, 1985–1993 and 1993–1996). Logging activity, major road construction, and extreme typhoon and earthquake events produce short-term acceleration of landslide incidence. In principle, recovery rates of the land from pulsed perturbations of about 20 years for logging activity and about 8 years for major road construction may also be suggested.
Keywords :
Land use , Landslides , Formative events , Recovery time , Taiwan
Journal title :
CATENA
Serial Year :
2002
Journal title :
CATENA
Record number :
2251908
Link To Document :
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