{"blocks":[{"key":"9tnpg","text":"60-80 cm of recent storm snow has been heavily impacted by strong winds from varying directions, forming reactive wind slabs on all aspects in wind-exposed areas. This snow overlies old 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":"90-150 cm of snow from the second half of January over lies a thin layer of facets that formed during the mid-January cold snap. Recent avalanche activity in the Bear Pass area and snowpack tests results have indicated that this layer remains a concern (check out this MIN report).","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":269,"length":10,"key":0}],"data":{}},{"key":"1oj9l","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"bj7sb","text":"A crust from mid November exists at the base of the snowpack. So far, we have only one observation from Saturday in the far north of the region showing this layer waking up during the storm. Previously, the last avalanche reported on this layer was on January 17. Limited potential still exists for large avalanches in surface layers to step down to this layer.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":2,"length":5,"key":1},{"offset":337,"length":9,"key":2}],"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"}},"2":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#step-down-avalanche"}}}}