Slopes and Mass Movements Flashcards
What is Denudation?
wearing away of the landscape (exogenous)
What is a Slope?
Inclined surface that forms a boundary between 2 landscape features
How are slope angles formed?
Slope angles are formed as weathered material is pulled downward by gravity
-Primary reason for differences is that the stronger material is able to maintain a steeper angle
What 3 forces must be overcome in order to move material?
Friction: resistence of movement by 2 passing objects
Inertia: something in motion wants to stay in motion, not moving wants to stay in place
Particle Cohesion: how well the pieces stick together
How to friction, inertia and particle cohesion relate to slope?
Higher friction, inertia and particle cohesion = stronger = steeper slope (They are the 3 factors of Shear Strength)
-Sheer Stress: gravity interacting with the slope angle
What is the Angle of Repose?
the angle that balances shear stress and shear strength
Slope stability
Determined by shear stress & strength
Stable: shear strength able to maintain angle
Unstable: shear strength unable to maintain angle (movement)
What could modify slope stability?
-changes in balance due to modification of slopes (rivers, road cuts, waves crashing on cliffs) or modification of shear strength (weathering, water, vegetation, shocks)
Mass Movement Types
SLIDES: fine material sliding (cohesive)
FLOWS: coarse material (non-cohesive, more turbulent)
HEAVES: general, overall movement
Rockfall
Source of rock up top (strong material = steep slope)
- weathering occurs
- Vertical drop (fast moving = wrong place, wrong time)
Landslide
Transitional slide (dirt, etc = land) Wetter would be a "Flow"
Slump
- top drops downward
- relatively cohesive, dry
Earthflow
- likely happening during rainy season
- rounded scar at top (origin)
- narrow connection
- rounded lobe at bottom
- fine material
Debris Flow
- river of cement like mixture of mud, debris
- can be very devastating
- mud piles up on sides, pushes stuff down the middle
- coarse material
- flow
Creep
very slow, gradual