Mass Wasting Flashcards
what is mass wasting
the downslope movement of rock, regolith and soil under the influence of gravity
what are two roles of mass wasting
- geologic processes that often follows weathering
- combined effects of mass wasting and running water produce stream valleys
how do weathering and mass wasting compliment each other
weathering weakens the material and allows gravity to easier act of the material
what process does mass wasting often follow
weathering
describe the evolution of mass wasting on slopes over time
in areas of rugged, geologically YOUNG mountains there are the MOST RAPID events
over time mountain sides lower through mass wasting and erosion
the older landscapes are LESS dramatic downslopes than young ones so they have LESS dramatic movements downslope
what is the controlling force of mass wasting
gravity
what are triggers of mass wasting
- water
- over steepened slopes
- loss of vegetation
- earthquakes
how does water act as a trigger for mass movements
saturation of the material with water molecules reduces the particle cohesion which decreases the materials resistance to gravity
AND
saturated soils have more weight which makes the soils also more susceptible to gravity because it changes the balance on the slope
how do steepening slopes act as a trigger for mass movements
slopes have a set slope angle that maintains the balance of the slope (not too steep but not too shallow), over steepened slopes lose that balance,
(they have a steeper slope angle which makes it unstable and more susceptible to failure)
what is a natural process for steeper slopes
- undercutting by streams or wave action (erodes the slope and increases steepness)
-
how does removal of vegetation act as a trigger for mass movements
removing vegetation from a slope removes the root systems that bind soil and regolith which were acting as protection for the slope from rainfall (increases saturation)
how does undercutting by streams/rivers cause steeper slopes
the process removes the slope’s base which both causes an increase in slope angle AND increases the gravitational force acting parallel to the slope
what are some human processes that cause steeper slopes
- cutting into its side too deeply
- excavation for road cuts and hillside building sites
- dumping or filling areas to build houses on top of hills
how do earthquakes trigger mass movements
the shaking can dislodge large volumes of rock and unconsolidated material = the sediments lose their strong cohesion and induce failure
how to classify mass movements
- type of material involved (debris, mud, earth or rock)
- type of motion
(fall, slide, flow) - rate of movement (fast or slow)
what type of movement is this
materials fall through the air from talus slopes
fall
what type of movement is this
material moves along a surface as a coherent mass
slide
what type of movement is this
materials viscously deforms - becomes a jumble of material
flow
what is a talus
a slope that is built of angular rock fragments that fall to the base of the cliff
are talus rock falls fast or slow
SLOW
what is a slump
the downward sliding mass of rock OR unconsolidated material as a unit along a CURVED surface
what are distinguishing features of slumps
- crescent shaped scarp at the head
- raised toe at the end
- curved slump plane/surface with step-like blocks for each section of the slump detaches
where are slumps common
along river valleys and eroding shorelines
what kinds of slopes do slumps occur
those that are oversteepened and overloaded
slump
what is indicative of a slump
the step-like pattern of the different slump slides
what is a rockslide
blocks of bedrock that slide down a slope very quickly
are slumps rotational or translational
rotational
where are rockslides common
where rocks and joints parallel the slope which gets undercut
what is a common example of rock slide
frank slide
what is a major cause of slides
frost wedging
rock slide
Soil slide
rock slide
rock fall