Storm Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
A change in density weak layer exists about one foot deep in the newest strom snow. We got this layer to pop out with light force in our snowpit stress tests. We were not able to get this layer to react on rollovers or steep slopes. Our friends who were snowmobiling near Flattop in the Selkirks told us they were hearing whumphing and that was enough for them to play it safe and stick to the trees. I believe that change in density weak layer was the culprit for the whumphing.