Glide Cracks
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Although much of the wet avalanche activity remains behind us, it takes time for water to fully drain an 80+" snowpack. Deep rain rills serve as a reminder that the lower and mid-elevation snowpacks formed a drainage network to let massive amounts of water drain. Glide avalanches tend to linger the longest after a massive rain event (ending early Saturday) as water continues to lubricate bedrock faces. A glide avalanche frequently takes the entire season's snowpack along with it, making them nearly unsurvivable if you are in the wrong spot and a surficial crust doesn't prevent the problem. The glide threat is becoming low probability, but remains high consequence. We don't know when a particularly slope will avalanche, but our terrain selection can help us avoid the problem. Don't linger under smooth bed surfaces (which can be identified by satellite imagery) and/or "brown frowns of glide cracks."
Glide cracks were spotted on a number of slopes on 1/14 in the nearby West Central Zone. Give these areas a wide berth by not traveling on or beneath them.
Photo: Irene Henninger