Recently formed windslabs may exist on lee slopes adding to a strengthening hard wind slab problem that developed last week.
Cornices
N
NE
E
SE
S
SW
W
NW
Alta quota
Limite del bosco
Sotto il limite del bosco
Probabilità
Possible
Dimensione
1–5
Large cornices exist in alpine terrain. A failure could be destructive by itself, and could also trigger an avalanche on the slope below.
Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alta quota
Limite del bosco
Sotto il limite del bosco
Probabilità
Possible
Dimensione
3–5
The persistent weak layer that formed in early February is most prominent on unsupported, sheltered slopes at treeline . Although avalanches on this layer have not been reported this week, triggering may still be possible in isolated terrain.
Avalanche observations have been limited. There was, however, point release sluffing to size 2 in steep terrain in the north of the region on Tuesday.
Snowpack Summary
Light amounts of low density snow sit over a variety of old surfaces that include widely distributed hard wind slabs, or melt freeze crusts that exist on most aspects below 1000m and on solar aspects as high as 1600m. In exposed areas the newer low density snow has been shifted into deeper pockets of soft wind slab. The mid February surface hoar, down around 60cm, is not widespread and is gaining strength, but should still be on your radar in steeper, unsupported terrain at treeline and below. Cornices in the area are also reported to be very large and primed for triggering.