Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2.5
Our long cold sunny dry spell that was the theme for the latter part of January created what we are calling the January Drought Layer or JDL. Weak facets and surface hoar was buried and now sits under a 3-4 foot of slab of snow that could step down another foot to a weak layer of facets underneath a rain crust from 1/3.
***This problem not going away soon and is going to be your problem if you venture into steep terrain, especially shaded, or Northerly aspects where the weak layers are weakest. Our test pit results point to human triggering being likely to possible (ECTPV to ECTP15, PSTEND 19/100) with the most potential to trigger being on slopes tipped away from the Sun. This layer is getting deep and may be harder to trigger in some spots than others. Thin spots in the slab or weaker areas near tees and rock are likely trigger points and this may not happen until the second or third person gets on the slope.
When this layer fails, it collapses suddenly and propagates a fracture fast and clean...you likely cannot outrun this or out smart this if you are in terrain steeper than 35 degrees.
Choose simple terrain with a slope angle less than 35 degrees!
State of the Snowpack at Palooza Basecamp & Eatery in Cascade Palooza Basecamp 112 N Main, Cascade, ID, United States
State of the Snowpack at Palooza Basecamp & Eatery in Cascade February 6 - 6pm - 8pm Come find out what is going on in the snowpack with the PAC forecasters. Just how bad/good is it our there? Support the avalanche center and enjoy some great food!
Free
Today's Forecast is sponsored by Brundage Mountain Resort. Thanks for supporting the PAC and your awesome bar graph on your snow report!