Chapter 15 Flashcards
Landslide
sudden event where large quantities of rock move downhill
mass wasting
downslope movement of rock, regolith, and soil under the direct influence of gravity
most rapid and spectacular mass-wasting events occur in
areas of rugged, geologically young mountains
are changed to more subdued terrain
role of water
when sediment pores fill with water, cohesion among particles are destroyed
Water can lubricate materials
water adds weight to a mass of material
dry sand grains
bound mainly by friction to one another
damp sand grains
small amounts of water increase the cohesion
wet sand grains
saturation reduces friction and causes the sand to flow
Heavy rains trigger
debris flow
angle of repose
unconsolidated granular particles assume a stable slope
mass wasting can be triggered by
oversteepened slopes that are unstable; ex: stream cuts, oversteepen slope
landslides without triggers
slope material weakens over time
some landslides are random, unpredictable events
fall
the free fall of detached pieces
Talus slopes are built by rock falls
slide
occurs when there is a distinct zone of weakness separating the slide material from the underlying material
rotational slide
surface of rupture is concave up
translational slide
material moves long a flat surface