Chapter 15 Flashcards
(26 cards)
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
flow
occurs when material moves downslope as a viscous fluid
rock avalanche
most rapid type of mass wasting
rocks float on air as they move downslope
creep
moves particles a few milimeters per year
slump
movement of mass of rock or unconsolidated material as a unit along a curved surface
occurs along oversteepened slopes
rockslide
occurs when blocks of bedrock slide down a slope
- fast and destructive
- triggered by earthquakes, rain or melting snow, common during spring
debris slide
occurs when unconsolidated material slides down a slope
debris flow
rapid form of mass wasting that involves the flow of soil and regolith with water
often confined to channels and canyons
Lahar
debris flows composed mostly of volcanic materials
Earthflows
form on hillsides in humid regions during heavy precipitation or snowmelt
commonly involve materials rich in clay and silt