Lecture 20 - Mass Wasting Part 2 Flashcards
fall
a material dropping through air, vertically or almost vertically
slide
a material movie as a mass along a sloping surface (there is no internal motion within the mass itself)
flow
downslope movement of a material that also has internal motion, like a fluid (eg. water, lava)
regardless of name, most mass wasting examples include two or more of the following: ____
fall, slide, or flow
falls are an extremely __ or very ___ form of mass wasting seen with ___ and ____
rapid
rapid
rocks (rockfall)
unconsolidated materials (soil fall)
rockfalls
- rapid downslope movement of dislodges rocks that originates above a steep enough slope
- rocks may experience falling, rolling, bouncing, and/or sliding
- falling rocks include broken chunks from bedrock outcrops or boulders coming down mountain slides/cliffs
bedrock
- hard, solid sock (ie. consolidated rock) under unconsolidated surface materials such as soil, sand or gravel
- can extend hundreds of meters below earths surface
- exposed (ie. above earths surface) bedrock seen on mountain tops, along coastlines, in quarries and on plateaus
plateau
region of relatively level/flat ground with a higher elevation than surrounding area
outcrops
visible exposures of bedrock occurring due to erosion or tectonic plate activity
hydrostatic pressure
pressure exerted by any fluid (eg. water) in a confined space
rockfalls and soil falls can also be driven by:
(other than factors discussed in previous lecture — shear force, shear strength, rock strength)
- hydrostatic pressure and the presence of water in bedrock cracks
- freeze (ie. expansion) and thaw (ie. contraction) cycles
- heavy snowfall and subsequent melt
- plant roots in bedrock cracks
- erosion by rivers/streams and/or wave action below (aka. undercutting)
- quarrying (ie. mining) activities
slides can range from extremely ___ to extremely __. this form of mass wasting is seen with __ and __
slow
rapid
rocks
unconsolidated materials such
types of slides
- rock slide
- rock avalanche
- slump
rock slide
- sliding motion of rocks along a sloped surface
- can range from very slow to moderately fast
rock avalanche
- sliding motion of rocks along a sloped surface
- larger rocks moving downhill quickly (at speeds on the order of meters/second) fragment (ie. breaks down) to form smaller rocks/pieces that keep moving downhill /slope
slump
- sliding encountered when have thick (>10 meters) layer/slice of unconsolidated material on a curved slope
- (may also observe same for rock layer on curved slope)
- can occur extremely slowly to moderately fast
- mass of unconsolidated material gradually moves downward and spread outward
- often caused by presence of excess water between unconsolidated layer and served slope
types of flows
- creep
- mudflows
- debris flows
what’s a creep
- very slow (mm/year to cm/year) movement of soil/unconsolidated materials down a slope
- prevalent on sloped surfaces
- an example of very slow flow but difficult to rule out some sliding in many cases
- results in cracked roads
- results in trees, fenceposts, grave markers, etc… that lean downhill
trees exposed to creep end up with ___
curved lower trunk
curved trunk is also known as ___
pistol butt
flows can range from extremely ___ to extremely ___. this form of mass wasting is generally associated with unconsolidated materials
slow
rapid
creep down a sloped surface can be enhanced by (3)
- frozen subsoil preventing water drainage and wet materials down above slowly moves downhill
-freeze/thaw - frequent wetting/drying of soil
what is solifluction
- creep triggered by freeze-thaw in colder climates
- gradual movement of wet soil/wet unconsolidated materials down a slope
what are mudflows and debris flows
- often rapid and extremely raid movement of soil/sediment/unconsolidated materials down a slope
sediment/unconsolidated materials saturated with water (eg. due to heavy rain, ice/snow thaw) lose strength and ability to stay/stick together
sediment/unconsolidated material grains are pushed apart to extent that saturated mixture can actually flow