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Mass Movements
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Introduction Explain why slopes fail under force of gravity
Explain factors influencing slope failure Describe types of mass movements and why they usually occur Discuss importance of mass movement processes in shaping landscapes and associated hazards
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Introduction Rock, soils, and other materials move downhill
Sometimes rapidly, sometimes slowly Pose threats to people Modify the landscape
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Slope Stability and Mass Movement
Gravity is main force driving materials downslope Slopes have threshold of steepness Angle of repose is steepest angle at which a given material will remain stable `sand degrees, boulders as steep as 45 Frictional strength of material resist movement Rough surfaces greater frictional strength Increased weight of material increases resistance
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Force of Gravity Two components
Shear stress –pushes block parallel to slope Other component pushes block into slope Stress is perpendicular to slope surface The greater the weight of block the more resistance to movement
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Cohesion Besides shear stress, cohesion also resists motion
Is tendency of materials to stick together to resist movement Cements and roots can increase cohesion
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Water Pressure Increases chance of failure
Pressure of pores filled with water reduces frictional resistance
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Forms of Mass Movement Mass movement – movement of earth materials by gravity Mass wasting is term also used
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Creep and Solifuction Slow almost imperceptible mass movement
Revealed by tilted trees, fence posts Soil particles rise with freeze or wetting, settle lower on slope when warmed or dry Flow of soil occurring mostly cold high latitudes
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Slides Blocks of rocks moving on distinct plane
Landslide is general term Slump is movement on a curved plane Rockslides – large blocks break loose, move rapidly downslope Important factors in slides Groundwater pressure Oversteepening slopes
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Flows Fluid movement of loose earth materials
Earth flows are slow moving flows of mostly fine grained or clay-rich soil/sediment Debris flows – fast-moving mixture of sediment and water Mudflows are debris flows of mostly muddy sediment Debris flows involve water
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Flows
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Rockslides Mass of bedrock moving rapidly downslope
One of most dangerous mass movement types
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Fall Rocks break off and fall to base of slope/cliff
Talus accumulates at base
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U.S. Map of Landslide Risk
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