Valanga

Andesite Peak

Andy AndersonCentral Sierra Nevada
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Foto dell’osservazione 1Foto dell’osservazione 2Foto dell’osservazione 3Foto dell’osservazione 4

Quick report

Cracking
widespread

We started to see signs of unstable snow almost as soon as we started our tour. By noon, rapid snow accumulation and blowing snow had already formed unstable wind slabs on wind-loaded slopes, and the first wind-loaded test slope we kicked failed easily. A few minutes later, we triggered shooting cracks that failed on surface hoar layer buried about 14 inches deep. We kept triggering shooting cracks and test slope failures to the top of Andesite Peak. These included wind slabs, cracks on buried surface hoar, and cracks on other buried weak layers like weak snow near crusts. The signs of unstable snow grew larger and more widespread during the afternoon. We used conservative terrain choices during our tour. 

We triggered several test slope failures in wind-loaded areas. We also experienced widespread cracking that failed on weak layers in the old snow like buried surface hoar or weak sugary snow (facets) near crusts.

Weather

Air Temp
19
Cloud Cover
overcast
Wind Loading
intense
Recent Snowfall
20
Snow Avail For Transport
large amounts

During our tour, snowfall rates reached at least 2 inches per hour. We experienced strong winds and intense blowing snow in exposed areas, and temperatures stayed in the teens.

Avalanche

Size
D1 R1
Type
SS
Aspect
E
Trigger
AS
Elevation
7890 ft

We intentionally triggered a small wind slab avalanche with ski kicks at the top of this path on Andesite Peak. We also triggered test slope failures on other small test slopes. In the most wind-loaded areas on the ridge, the wind slabs were ~ 30 - 35 cm thick. In the less wind-loaded places like this, they were only 10-15 cm thick. Sometimes, the cracks that formed as the wind slab failed went deeper into the snowpack, down to either a buried surface hoar layer or a layer of facets near a crust. See the attached ob for more details.