Week 9, Mass Movements and Avalanches Flashcards
Gravity is always toward the ____ of the earth, not ____ to surface.
Gravity is always toward the centre of the earth, not perpendicular to surface.
For an object to move parallel to a slope we need 2 criteria:
Must overcome
Friction (shake or kick boulder) AND inertia (rain)
How water increases instability
- adding weight to soil or porous rock
- expanding and weakening clay minerals
- decrease rock cohesion, also called cement dissolution
- subsurface erosion
- increasing pore pressure due to burial weight, destabilizes soil
- raising water table
How can we trigger a mass movement event?
- heavy rain
- earthquakes
- thawing of frozen ground
- surface disruption by humans
1 kg boulder experiences __N of force.
1 kg boulder experiences 9.8N of force.
Mass Movement Classification
Downward: Falls and subsidence
Down and outward: Slides and flows
Mass Movement Classification: Falls
Individual blocks detach along fractures
Mass Movement Classification: Subsidence
Collapse into void, dominantly vertical downward movement, moves as separate blocks.
Mass Movement Classification: Slides
Slide of blocks on surface
Mass Movement Classification: Flows
No sliding surface, more as fluids. (Includes creep)
2 types of slides
rotational and translational
Rotational Slide
Decrease in the driving mass, increase in the resisting mass. Does not typically slide for long distances.
Translational Slide
Mass slides on surfaces of weakness, can slide for long distances.
Block Slides: Material remains intact
Debris Slides: Material deforms as it slides
Lateral Slides: Underlying material breaks and flows
Creep
Slowest but most common failure.
Caused by successive expansion/contraction due to freezing/thawing, wetting/drying of clay minerals heating/cooling.
Expansion due to heating it is perpendicular to the surface while contraction is due to gravity.
Complex Events
Mass movements that combine falls, slides, and flows along their path.
Subsidence can happen fast or slow, what do these speeds look like?
Fast: Sudden collapse into subsurface void
Slow: Slow sag due to compact of water saturated sediments (Like Italy) or long term removal of ground’s water.
Inertia
The tendency of an object to stay in place
Mass Movement Mitigation
- Reinforce Hazard: unload head, reinforce body, support toe
- Contain Hazard: wire mesh, steer flows in direction of least harm
- Support Hazard: buttress overhanging blocks or weak layers
- Protect against hazard: tunnels snowsheds
- Sea to sky highway
Avalanche Path
Starting Zone: Steepest slope: 30-40 degrees
Track: Guided by topography: 20-30 degrees
Run-out zone: < 20 degrees
Avalanche size scale
Logarithmic:
Size 1: 10 tonnes, 10 metres, 1 kilopascal of force Size 2: Can kill people Size 3: Danger to highways Size 4: Rare Size 5: Massive, very rare
Avalanche Types
- loose snow/sluff
- slab avalanche
What is needed for a slab avalanche?
- cohesive slab on top
- weak layer to fail and slide on
- most common on slope > 30 degrees
- most commonly triggered by extra weight of skier
Snow becomes denser and more cohesive with
age.
Explain how hoar frost creates weakness in the snow pack?
Hoar develops on the surface, when buried it can be deadly because it is so weak. Wind can cause loading.
Indicators of wind loading:
- cornices (out of wind)
- rime growing on object (into wind)