Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 3
So far this week we haven't heard much from our problem child, the persistent weak layer, now buried in the mid portion of our snowpack. However, given its recent track record what we do know is this... each time the snowpack receives a big thump of water, snow, and wind, this dormant layer comes back to life and we see avalanches breaking deeper than we might expect, particularly in terrain where the snowpack is thin and weak. Now here's the problem- "persistent weak layers" in the snowpack are a headache because all we need to do is find one weakness, maybe around a bush or rock that we can't see buried underneath the snow, collapse the pack, and now we've triggered a slide that quickly gets out of hand.
With a big storm on tap we'll need to recalibrate our cerebral travel policy and implement an avoidance plan. So you're asking, "how do we manage an unmanageable avalanche dragon is the snowpack?" Well we simply avoid it... and the usual suspects come to mind- steep, rocky terrain and slopes that have already avalanched this year. In addition, periphery terrain where the pack has remained shallow all season should be considered guilty until proven otherwise.
These beautifully detailed JG pits clearly illustrate a tale of two snowpacks.
In the upper image a pack with a bit of body and short-term stability. Whilst the lower image shows a pack with structural weaknesses and questionable strength.
In either case, snowpit stability tests reveal failures on or near the early January snow which has faceted, confirming a suspicious layer to keep an eye on, especially as a series of storms sets its sights on the range this week.