When a chunk of the side of Wai`ale`ale/Kawaikini sloughed
off this week, it sent a catastrophic debris flow down a tributary of the
Wailua River.
A flash flood of water, rocks, dirt and logs scoured the river
bed and its banks, destroying all vegetation and any wildlife in the area.
(Image: A screenshot of the Wailua streambed after the
debris flow. The image is taken from a Kaua`i Fire Department video taken from
a helicopter.)
The event turned the Wailua River a yellowish milk chocolate
color, as the mud mixed with the flow from myriad streams feeding Wailua.
This isn’t new. It happens fairly frequently, though mostly
in smaller events. You frequently see vertical brown streaks against the green steep
cliffs of the older islands, indicating similar events.
The Wailua event appears considerably smaller than a massive
slide at the back of Olokele Canyon around 1980, when an immense chunk of material
plunged down a towering basalt wall, hit the bottom, and surged downstream. An
image of that event is visible on the first page of this site from the Association of American State Geologists.
In that case, the Makaweli River flowed milk chocolate
in color for months. A most interesting view was where Makaweli and Waimea
joined, and you could see swirling and mixing of the the tea-tinted Waimea
water mix with the café-au-lait of the Makaweli River.
This landslide process is sometimes called mass wasting, the
downward movement of soil and rock under the influence of gravity, often
lubricated by water. It is an entirely natural process that has been going on
for millennia.
Indeed, just as periodic volcanic eruptions are responsible for
building the Islands, periodic landslide events are significant features in
unbuilding them.
“Volcanoes are particularly prone to massive rock slope
failure and can experience very large scale sector collapse or much smaller
partial collapse,” says a 2006 paper, “Landslides from massive rock sloped
failure and associated phenomena.”
What is often far more dangerous—sometimes catastrophic—is the
water, mud, rock and debris flow and lunges downstream as part of the collapse.
It can rip out everything in its path, scouring the valley floor to bare mud
and rock.
Such events also have significant impacts on nearshore waters, dumping tons of sediment into the coastal ocean, often temporarily blanketing reefs.
Such events also have significant impacts on nearshore waters, dumping tons of sediment into the coastal ocean, often temporarily blanketing reefs.
© Jan TenBruggencate 2014
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