Wednesday, April 12, 2006

Weather, Avalanche

National Park Service Olympic National Park Newsletter, Avalanche scar on north-facing slope just north of Hurricane Ridge parking areaNational Park Service Olympic National Park Newsletter, Avalanche scar on north-facing slope just north of Hurricane Ridge parking area
National Park Service Olympic National Park Newsletter, Olympic Mountain Rescue volunteer investigates avalanche face shortly after the slideNational Park Service Olympic National Park Newsletter, Olympic Mountain Rescue volunteer investigates avalanche face shortly after the slide.
Types of Avalanches:

Wet avalanche, Definition: A flow of snow, ice, rock, and other material that occurs as a result of thawing. Context: These occur mostly late in the snow season when the snowpack is deep and the thaw is just beginning.
Wet Slab Avalanche, National Park Service.Slab avalanche, Definition: A mass of snow, ice and possibly other material caused when a large slab of snow breaks free from the layers beneath. Context: A slab avalanche is the most deadly. The weight of a skier is enough to break a slab.
Battleship Avalanche, National Park Service.Powder or Loose Snow Avalanche, Definition: A mass of loosely packed snow that begins with a piece of falling rock or ice. Small loose snow avalanches are called "sluffs". Context: The largest and most destructive is a powder avalanche. A piece of falling ice or rock starts a mass of loose snow sliding down the mountain.
Cornice Fall Avalanche, Definition: Cornices are snow structures formed by wind drifing snow onto the lee (downwind) side of an obstacle, such as a ridgeline. The weight of a falling cornice breaks into hundreds of pieces and forms its own avalanche. Context: Cornice fall fatalities are a significant problem in big mountains, they often break off farther back than expected.

Ice Avalanche, Definition: Falling blocks of ice create an avalanche, which often entrains snow below it or triggers slabs. Context: Glaciers flowing over cliffs form icefalls and most common in big mountains.

Glide Avalanche, Definition: A type of wet avalanche, they occur when the entire snowpack slowly slides as a unit on the ground (similar to a glacier). Context: Glide avalanches are a slow process which usually occur over several days, weeks or even months. Caused by melt water libricating the ground and allowing the overlying snowpack to slowly "glide" downhill.

Slush Avalanche, Definition: A sluch avalanche occurs when a cold dry snowpack suddenly becomes saturated with water. It then catastrophically looses strength and the resulting slush often runs long distances on gentle terrain. Context: Common in northern latitudes such as Alaska and other high latitiude permafrost regions.

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Avalanches, Much of the terrain in the Olympics is prone to avalanches and should be avoided until avalanche danger lessens. Avalanche hazards may exist through out the winter, spring and early summer in some areas.

Don't let the next avalanche victim be you or someone you know!

Avalanche Tips, All winter travelers should be familiar with the terrain they will be traveling in and should be familiar with avalanche self-rescue techniques. Remember, the most important factor is prevention -- the probability of rescuing someone who has been buried in an avalanche is low.

Do not travel alone in Avalanche Country! Avalanche release zones may be well above you and not within your sight. Do not travel below steep open slopes, especially where avalanches have already occurred and during warming periods or times of heavy rain or snowfall.

The most dangerous time for avalanches is during heavy snowfall (rates of one inch or more per hour) and warming periods with heavy rains or sunshine. When planning or leading a trip into the mountains, examine your destination and EVERY STEP OF THE ROUTE to see whether or not the terrain and conditions pose a threat. Be especially vigilant if the temperature rises significantly or suddenly by 4-10 degrees, if steady rain falls on the snowpack, or if bright sunlight shines directly on exposed slopes.

Avoid climbing or traversing suspect slopes or traveling along valley bottoms beneath such slopes. Ridge-tops are much safer; but watch out for huge cornices overhanging leeward sides.

Special dangers: 1) steep north, east or lee faces; 2) south slopes at midday; 3) warmer than usual weather.

If there is any doubt, cancel the trip or reschedule your route or destination to a safer location with gentle, forested slopes and little snowpack. Use good avalanche practices of never raveling alone, and spacing party members some distance apart in questionable spots.

Carry and know how to use avalanche transceivers, but do not rely on them to keep you from danger. If you are a member of a party led by someone you don't know or if you have questions or doubts about their judgment, ask questions. Do not assume they are competent.

More Information, Avalanche conditions may exist throughout the spring and well into the summer months in some areas. Before your trip, find out snow conditions in the area you plan to travel.

For more information on snow conditions, route information and snowpack analysis contact: The Wilderness Information Center (360) 565-3100

Source: National Park Service Olympic National Park Avalanche Hazards

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