Tuckerman Ravine

Found no signs of instabilities in the surface snow or deeper in the snowpack and observed a consolidated snowpack. Warm temperatures and rain seemed to promote stability within thin weak layers between various wind slabs. The surface was firming as temperatures began to drop and with sub freezing temperatures tonight this surface will become a new melt freeze crust and likely a bed surface for future avalanches. 

Observed no wet loose surface snow or evidence of debris in the Ravine.