Human Triggered Avalanche in Sluice – Tuckerman Ravine

By Jeff Fongemie | MWAC

Date of Observation: December 21, 2019  10:30 AM
Location of Observation: Sluice, skiers right, Tuckerman Ravine

Observed fresh avalanche crown with ski tracks entering in from lookers right. Slope SE, slightly convex, approx 40 degree slope angle. D1 hard slab, 30′ wide with a crown height 20″. Very little debris remained possibly due to fragmenting & spreading and the overall small volume of snow. My impression: this is a nasty place to take a fall due to the steepness and exposed rocks.


Snowpack observations are one part of the complex puzzle which is your decision to enter avalanche terrain. Some observations may include stability tests. It’s important to understand that the results of a stability tests are seldom conclusive anywhere, but particularly in snow climates and terrain like ours where the primary driver of instabilities is wind drifted snow. Many stability tests exist and each works best with specific avalanche problem types. Stability test results should never be used alone as an indication that a slope or conditions are safe particularly when more obvious red flags are present. Please use this page as part of your information gathering process, but don’t make decisions based on a single piece of information. A good article that summarizes some of the issues associated with snow and avalanche observations can be found here.

The Mount Washington Avalanche Center cannot verify the quality or accuracy of any observations that come from the general public.


See an avalanche or evidence of previous avalanche activity?  Near-miss? Snowpack observations?

Your observations are valuable to an accurate forecast! We welcome observations from everyone. You don’t need to be an avalanche professional to submit helpful observations, just be as detailed and accurate as you can.