ISSN:
1573-0840
Schlagwort(e):
Slump
;
debris flow
;
slope movement
;
mountain area
Quelle:
Springer Online Journal Archives 1860-2000
Thema:
Energietechnik
,
Geographie
,
Geologie und Paläontologie
Notizen:
Abstract In September 1979, rain-induced complex landslides occurred in two separate localities along the slopes of the Akovolwo Mountains near Jato-Aka in the Kwande Local Government area of Benue State, Nigeria. The two movements developed on bedrock slopes covered by a veneer of colluvium and (or) residuum no more than 1.5 to 2m deep. Each started as a slump and graduated into a debris flow. The slump, extending downhill a short distance away from the head scarp, had been reconstituted into a debris flow as the initial movement (sliding movement) of the soil mass caused remoulding of the saturated moving mass into viscous debris-laden mud. The resulting mass moved partly along a pre-existing mountain stream channel and partly along a fresh channel it cleared in the savanna forest. At the break of slope, the mass of boulders was dumped and a trail of smaller fragments littered the channels towards the Katsina-Ala River.
Materialart:
Digitale Medien
URL:
http://dx.doi.org/10.1007/BF00126611
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