{"blocks":[{"key":"5qumb","text":"Extensive wind affect at all elevations. Southerly winds are forming fresh windslabs from new snow in places that were previously scoured by northeasterly arctic outflows. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"605i","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"70tk1","text":"Around treeline, the old windslabs may overly a layer of surface hoar, up to 1 m deep. This means they may remain sensitive to human triggering and resulting avalanches could be surprisingly large. Deeper in the snowpack, another couple of surface hoar layers are currently buried about 80-120 cm below the surface in sheltered areas around treeline. There have been no reports of avalanche activity associated with them for a few weeks, during which several storm slab avalanche cycles have tested their potential for step-downs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":57,"length":12,"key":0},{"offset":240,"length":12,"key":1},{"offset":519,"length":10,"key":2}],"data":{}},{"key":"76fod","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"ac6vm","text":"A deep crust from mid November lurks at the base of the snowpack. A couple of recent large avalanches are suspected to have run on this layer in isolated incidents on lee and cross-loaded features high in the alpine.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"href":"https://www.avalanche.ca/glossary#surface-hoar","target":"_self","url":"https://www.avalanche.ca/glossary#surface-hoar"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"href":"https://www.avalanche.ca/glossary#surface-hoar","target":"_self","url":"https://www.avalanche.ca/glossary#surface-hoar"}},"2":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#step-down-avalanche"}}}}