{"blocks":[{"key":"9tnpg","text":"50-70 cm new snow through Thursday (and still counting) has been heavily impacted by strong southwesterly winds forming a reactive storm slab. This new snow overlies a variety of wind affected surfaces in exposed treeline and alpine areas. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"39ura","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"dpldi","text":"Snowfall from the second half of January over lies a thin layer of facets, down 70-140 cm, that formed during the mid-January outflow event. Recent avalanche activity in the Bear Pass area and snowpack tests results have indicated that this layer is still a concern (check out this MIN report). Below tree line, a recent warm-up moistened snow surfaces up to 900 m, forming a temperature crust. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":282,"length":10,"key":0}],"data":{}},{"key":"1oj9l","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"bj7sb","text":"A crust from mid November lurks at the base of the snowpack. The last reported avalanche on this layer was Jan 17th. While it is promising that last week's significant snowfall did not trigger avalanches on this deep persistent weak layer, there is lingering uncertainty as to whether this week's weather could meet the threshold. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":2,"length":5,"key":1}],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/map?panel=mountain-information-network-submissions/7ce732e1-d515-49e3-88ed-81e8a38fb13b"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"href":"https://www.avalanche.ca/glossary#crusts-are-hard-layers-of-snow-usually-created-by-liquid","target":"_self","url":"https://www.avalanche.ca/glossary#crusts-are-hard-layers-of-snow-usually-created-by-liquid"}}}}