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Mind map avalanches, hazard paper 2
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AVALANCHES
What?
Falling masses of snow that contain rocks, soil or ice that move downhill at speeds up to 300 kph.
When hazardous?
When interact with people & surrounding i.e. cause damaged to
properties, death, injuries,It also cause damaged to transport
networks & livelihood-tourism
TYPES
WET SNOW AVALANCHES
SLAB AVALANCHES
LOOSE SNOW AVALANCHES
-Later season-8 to 25 km/hr-causing snow weight 1 million tonne
-more deadly-start due to human error-a large slab ice & snow shear away from hillside & more rapidly downhill-it has immense power
-start at a single point-involve loose powdery snow-occur little warning-any season-speed; 300km/hrforce 50 tonnes/m2
CAUSES
HEAVY SNOWFALL TREE REMOVEDHIGH RAINFALLHUMAN
RISE IN TEMPERATURE
Add weight easily snowfalls
Rapid melting of snow, in
spring
Off piste skiing
Lubricate snow & trigger avalanches
Snow move downhill
unimpeded
Ways to reduce
Closing Avalanches prone slope & issue
warning
Trigger small avalanches
Controlled Avalanches activities
Planning
-Restrict activities; snowboarding, skiing in recreation with high risk areas.
-close prone slope & issue warning depend:snow condition,
Under controlled condition before the snow pack build to a dangerous situation. (use of explosive to produce small avalanches)
Stabilizing snow pack in starting zone-prevent snow pack from achieving momentum to begin to move2.planting of trees
Where and when to build infrastructure in mt areas to minimized damage to building & infrastructure. It is based on record of previous avalanches
Case study: Galtur Austria.Where? Tyrolean village of GalturWhen? Tues, 23 Fe, 1999, 4 pmCauses:-Jan 20 Jan onwards, a sequence of 3 storms recorded-Warmer weather at end of Jan causes melting & re-freezing until there was a much greater accumulation of snow-Temperatures had fluctuated so that heavy wet snow fell on top of dry snow, forming unstable boundaries in the snow packNature of avalanches:100 m height, 800 m wide, 2 sources; 200 kmph -300 kmph, 400 000 tonnes & lasted 16 seconds
Effect:
People crushed to death, 30 died in event, by 27th
Feb -38 final death toll,40 000 were stranded in ski resort, cars were crushed & hurled across roads, housesWere completely buried, snow & ice clearly sliced off top of one building.
CASE STUDY: GALTUR AUSTRIA
Where? Tyrolean village of Galtur
When? Tues, 23 Fe, 1999, 4 pm
Causes:1. Jan 20 Jan onwards, a sequence of 3 storms recorded2. Warmer weather at end of Jan causes melting & re-freezing until there was a much greater accumulation of snow3. Temperatures had fluctuated so that heavy wet snow fell on top of dry snow, forming unstable boundaries in the
snow pack
-Restrict activities; snowboarding, skiing in recreation with high risk areas.
-close prone slope & issue warning depend:snow condition,
Under controlled condition before the snow pack build to a dangerous situation. (use of explosive to produce small avalanches)
Stabilizing snow pack in starting zone-prevent snow pack from achieving momentum to begin to move2.planting of trees
Where and when to build infrastructure in mt areas to minimized damage to building & infrastructure. It is based on record of previous avalanches
Nature of avalanches:100 m height, 800 m wide, 2 sources; 200 kmph -300 kmph, 400 000 tonnes & lasted 16 seconds
Effect:People crushed to death, 30 died in event, by 27th Feb -38 final death toll,40 000 were stranded in ski resort, cars were crushed & hurled across roads, housesWere completely buried, snow & ice clearly sliced off top of one building.