Chapter 11: Mass Wasting Flashcards
Mass Wasting
Gravity movement, either downslope (landslide) or vertical (subsidence)
Shear Stress
Component of weight that is directed downslope; increases w/ slope angle
Friction
grain to grain contact
Angle of repose
the steepest slope angle that dry material will support w/out failing
-related to grain size, shape, and sorting
Cohesion(Capillary Force)
Mineral/mineral and mineral/water attraction (electric charge); increases as grain size decreases
Water content
- Dry: air in pores (angle of repose); weak
- Moist: air and water in pores; strongest
- Saturated: Only water in pores; weak
- Quick: Only upward-moving water in pores; no strength (liquefaction)
Heave
Expansion and contraction of soil’s slope)- slow and small amount
- Wetting/Drying
- Freezing/Thawing
- Heating/Cooling
- Soil Creep
- Talus Creep
Slide
Moves as a unit; no internal deformation
- Slip-translation
- Slump-rotation
- Landslide, rockslide
Flow
Internally deformed
- grain flow; dry sand
- mudflow; debris flow, lahar
- debris avalanche
- solifluction (common in saturated active layer above impermeable permafrost, can be quick)
Fall
Free fall from cliff; rock fall
Subsidence
Vertically downward movement, gradually (sinking) or suddenly (collapse)
Compaction
Gradual sinking
- compressible materials (Mississippi River Delta)
- Underground fluid w/drawl (San Joaquin Valley; ground water removal)
Collapse
Due to large, subsurface holes
- Limestone caves: sinkholes, karst topography
- Underground mines
Karst Topography
Lanscape consisting of numerous caves, sinkholes, and solution valleys formed by groundwater solution of rocks such as limestone and dolostone