Chapter 07: Mass Wasting Flashcards
Mass wasting
General process of Earth materials moving downslope due only to gravity
Trigger mechanisms (5)
Processes or events that reduce friction and/or increase effect of gravity
- Nature of material (some are more cohesive/stables, others not)
- Oversteepened slopes
- Water content (unsatured v. saturated)
- Loss of vegetation (e.g. wildfires)
- Earthquakes/volcanic activity (vibrations)
Angle of repose
Steepest stable slope allowed by a loose material
35° is generally the steepest stable slope for loose material
Planar surfaces and stability
Planar surfaces: bedding planes, faults, fractures, foliation
Such surfaces represent weaknesses within rocks that can greatly reduce slope stability (dangerous when inclined in same direction as slope)
Fragment shapes and stability
Angular fragments have more frictional resistance than round fragments
Oversteepened slopes
Naturally:
Formed by meandering/migrating streams that form the cutback/overhang combination; overhang eventually mass wastes
Manmade:
Leveling terrain for human activity (e.g. roads)
Poor pressure
Pressure of groundwater held within a soil or rock; pressure increases as pores retain more water (from increased rainfall or snow melt)
Adhesive force
Force keeping material together; in underground material, small amounts of water (water film) keep material together, but being saturated with water causes a loss of friction
Frost wedging
Liquid water freezes, expands gaps in rock’s planar weakness (e.g. fractures, foliation, bedding), causing material to fall
Risk management of mass wasting (6)
- Build retaining walls
- Drain excess moisture
- Terracing (building terrace steps/benches for gradual fall of material
- Covering steep slopes
- Re-grade slopes
- Plant anchor vegetation
Land subsidence
Process of land either gradually lowering in elevation or suddenly falling after gradual removal of subsurface material
Subsurface ground failure
Natural: e.g. dissolution
Man-made:
- Withdrawal of fluids (water, petroleum)
- Withdrawal (mining) of solids (salts, minerals, rocks)
Karst topography
Land with pock marks (sink holes, sinking streams) with caves underneath and collapsed sinks
Sinkholes
Collapse of land due to subsurface failure with unusually large void spaces
Subsurface cavitites (caves) formed by groundwater dissolving rock; caves were filled with water, helped support weight of surface land. Once cavities are empty, sudden collapse occurs, forming sinkholes.