Movement of soil, rock and other earth
materials (together called regolith) downslope by gravity
without the direct aid of a transporting medium such as ice,
water, or wind. It is estimated that more than 2 million mass
movements occur each year in the United States alone. Mass
movements occur at various rates, from a few inches per year
to sudden catastrophic rock falls and avalanches that can
bury entire towns under tons of rock and debris. In general,
the faster the mass movement the more hazardous it is to
humans, although even slow movements of soil down hill
slopes can be extremely destructive to buildings, pipelines,
and other societal constructions. In the United States alone,
mass movements kill tens of people and cost more than $1.5
billion a year. Other mass movement events overseas have
killed tens to hundreds of thousands of people in a matter of
seconds. Mass wasting occurs under a wide variety of environmental
conditions and forms a continuum with weathering,
as periods of intense rain reduce friction between regolith
and bedrock, making movement easier. Mass movements also
occur underwater, such as the giant submarine landslides
associated with the 1964 Alaskan earthquake.
Mass movements are a serious concern and problem in
hilly or mountainous terrain, especially for buildings, roadways
and other features engineered into hillsides. Mass movements
are also a problem along riverbanks and in places with
large submarine escarpments, such as along deltas (like the
Mississippi Delta in Louisiana). The problems are further compounded
in areas prone to seismic shaking or severe stormrelated
flooding. Imagine building a million-dollar mansion on
a scenic hillside, only to find it tilting and sliding down the hill
at a few inches per year. Less spectacular but common effects
of slow downhill mass movements are the slow tilting of telephone
poles along hillsides, and the slumping of soil from
oversteepened embankments onto roadways during storms.
Mass wasting is becoming more of a problem as the
population moves from the overpopulated flat land to new
developments in hilly terrain. In the past, small landslides in
the mountains, hills, and canyons were not a serious threat
to people, but now, with large numbers of people living in
landslide-prone areas, landslide hazards and damage are
rapidly increasing.














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