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| The physiognomy
feature of the valley where the waterfall passes through by landscape-oriented
faultage, is that large scales of fan-shaped age-old debris flow pile
and block the channel on the two hillsides. According to this physiognomy
characteristic, we can assume that the formation of this waterfall
is directly related to the large landslide caused by the earthquakes.
Now although the surface of the waterfall experienced anaphase calc-sinter,
cementation and sediment, the basic physiognomy feature that piled
up channel blocks are consisted of huge blocks of rocks formed by
landslide is very clear. |
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