lecture 21: avalanches Flashcards
how does snowpack on slopes fail due to gravity
creep
fall
slide
flow
avalanche paths
a: starting zone, steepest slope 30-45 degrees
b: track: guided by topography 20-30
c: run out zone <20 degrees
snow pack
snowpack deposited by multiple storms leading to snow layers with different properties
- becomes denser and more cohesive with age
frost crystals can grow between layers
boundaries are weaknesses
loose powder avalanche
acts like a flow, high speed (65-100km/hr), light snow often buries victims largely unharmed
slab avalanche
slab of heavy cohesive snow detaches at weak layer boundary
- act like a translational slide evolving into flow
- speeds of 30-65 km/h but heavy snow can cause casualties and destory buildings and railways
- most dangerous avalanche
rogers pass
150 tonne locomotive overturned in 1910 rogers pass slab avalanche
- 58 men losxt their lives
- canadas deadliest avalanche
- workers clearing snow when another slide came roaring down
avalanche safety
difficult to outrun avalanche - escape to side
- get rid of backpack skis and poles
- use swimming motion to stay near surface
- maintain air pocket in front of face
- fast location and rescue
before
consult and obey avalanche bulletins
- avalanche kit: transceivers, collapsible shovel and probe pole
how many people have been killed by avalanches in the past 26 years
more than 200 people
impacts of rogers pass
400m of track buried
locomotiev and plow hurled 15m and landed upside down, cars crushed
- abandon route through rogers pass instead go underground
present day rogers pass
abandoned line still visible
now used by cross country skiers
studies of avalanches led to detailed maps of where avalanches were occuring and how strong