|Region:||Chugach State Park|
Route & General Observations
Standard route up Arctic Valley toward Rendezvous Saddle.
Avalanche Level 1 field days. Dug hasty snow pits on SW slope @ 2900′ across from ski area on Dec 16 , and N slope @ 3500′ between Avalanche Gully and Rendezvous Saddle on Dec 17.
Obvious signs of instability
|Recent Avalanches?||No||Collapsing (Whumphing)?||Yes||Cracking (Shooting cracks)?||No|
Whumphing in larger consistent patches of snow at lower elevations in the valley and easy CT results in this same area; snowpit at 2900'.
Generally mild; 20-30F, light winds, broken cloud cover, 1-2cm new snow over both days.
Variable. 1-2 cm new snow, some wind effect.
Highly variable. Shallow overall, but patchy with areas scoured to ice crust on the ground to deeper areas of wind packed deposition. Depths from ~5cm to ~100 cm in areas we observed in the mid-elevations of the valley.
In general the snowpack is a mix of faceted weak layers, crusts, and wind slabs in several layers. See pit profiles photos.
Both snow pits had ~10cm of basal facets overloaded by a thick melt freeze crust, facets, and then a combination of facet/crust layers and wind slabs in the mid to upper pack. The snow pit @ 2900' had 2 thin (easily breakable) ice layers that indicate it may have rained for short periods during the recent warming trend. These were not observed in the pit at 3500'.
Pit 1: SW, 2900': Easy CT results (CTV, CT3, CT4 (SC)) of the entire snowpack on the basal facet layer on the ground, and moderate (CT13, CT15 (RP)) results on a faceted/(weak) ice layer sandwich 11-20cm down under a thin 1F wind slab near the snowpack surface
Pit 2: N, 3500': Moderate to Hard CT results (CT15-CT26 (SCx2, SPx1) 66cm down on a weak facet layer below a 44cm thick dense wind slab. Hard CT results (CT23, CT28, CTN) on the basal facet layer. This area is near the saddle and has pockets of deeper snow and a lot more wind effect than lower down in the valley but is still highly variable in snowpack depth. Test results suggest that the dense thick wind slab in the mid-upper snowpack (found in snow deposition areas at this elevation) is more supportive and more stubborn to collapse than found at lower elevations. However, the weak facet layers still exist in the lower snowpack below this dense slab and suspect could still be triggered in areas where the slab is thinner.
If this is any representation of the conditions of the Front Range and Eagle River, there are definitely some persistent weak layers still present in the lower snowpack underneath wind slabs that are present in varying depths and in most areas (including SW to NW slopes) that indicate touchy to stubborn sensitivity to collapse dependent on their thickness. Something to be cautious of if we ever get a big snow dump that we are all waiting for.