800 AM PDT MON DEC 10 2007 && ZONE AVALANCHE FORECASTS * OLYMPICS, WASHINGTON CASCADES, MT HOOD AREA- Moderate avalanche danger above 5000 feet and low below Monday through Tuesday night. SNOWPACK ANALYSIS In most areas relatively small amounts of recently received snow or surface hoar overly the refrozen old snowpack that was saturated during the heavy rain event a week ago. As of early Monday morning most areas received an additional trace to 2 inches of new snow that fell with light winds. Most areas now have between 2 to 6 inches of recent snow above the crust ranging up to about 6 to 10 inches in the MT Baker and Mt Hood areas where the greatest snow overlies the crust. Some localized pockets of small wind slabs may have developed over the crust during the past few days maintaining some areas of unstable snow and a moderate danger above 5000 feet. Although these areas would be considered localized, the main emphasis on the danger should be near ridges on mainly southeasterly to southwesterly facing slopes at higher elevations. Elsewhere the soft shallow amounts of recent snow overlying the hard crust are maintaining mostly stable snow and a low danger. The cold recent weather is beginning to facet and weaken the near surface crust as well as decomposing the old previously wet snowpack through destructive metamorphism. While this is currently not affecting the snowpack stability, it may become a factor when additional snow loading occurs. There have also been recent reports of small surface hoar development over the past few nights and this may also become a significant weak layer if buried by snowfall and subsequently loaded by the next significant storm snow now expected to develop late in the week. DETAILED FORECASTS MONDAY, MONDAY NIGHT, TUESDAY, TUESDAY NIGHT A few light snow showers ending Monday morning in the passes with most other areas becoming mostly sunny. Cool weather with light winds is expected later Monday through Monday night. Increasing high clouds are expected Tuesday and becoming gradually warmer. This should not appreciably change the overall danger as some pockets of unstable snow persist at higher elevations on some lee slopes near ridges with mostly stable shallow amounts of soft snow over a firm crust elsewhere. It should be noted that this weather should allow for further surface hoar formation as well as continued faceting and weakening of the crust region and the bond of recent snow to the old decomposing crust surface. These may be important factors when future heavier snow loading occurs. At lower elevations, the combination of light winds, a very shallow and in places patchy snow cover, and significant terrain and vegetative anchoring should all help to maintain a generally low danger and stable snowpack structure. &&