{"blocks":[{"key":"aqo4","text":"Melt freeze and sun crusts may be found at the surface on steep solar aspects. Recent moderate to strong (and in some cases extreme) southwest to westerly winds have stripped low density snow off the windward sides of alpine and near treeline and redistributed snow into wind slabs and soft slabs in immediate lees of ridge crests.  Multiple layers of Wind slab are present in many locations.  Soft snow can still be found in sheltered areas. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":20,"length":6,"key":0},{"offset":271,"length":10,"key":1},{"offset":310,"length":4,"key":2}],"data":{}},{"key":"fkas7","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2vl48","text":"A thick rain crust sits 30-60 cm below the surface and can be found up to 2100 m. Recent avalanche activity has been observed at the faceting interface between this crust and overlying snow.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":8,"length":10,"key":3},{"offset":133,"length":8,"key":4}],"data":{}},{"key":"2o48c","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"8ffk9","text":"A well consolidated and  settled mid-pack overlies generally weak basal facets that may be possible to trigger in isolated shallow rocky start zones or with large loads, such as a Cornice fall.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":25,"length":7,"key":5},{"offset":66,"length":12,"key":6},{"offset":123,"length":25,"key":7},{"offset":180,"length":7,"key":8}],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#crusts-are-hard-layers-of-snow-usually-created-by-liquid"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#wind-slab"}},"2":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#leeward"}},"3":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#crusts-are-hard-layers-of-snow-usually-created-by-liquid"}},"4":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#facetcrust-layer"}},"5":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#settlement"}},"6":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary/#basal-facets"}},"7":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary/#a-shallow-rocky-start-zone-is-an-area-of-the-snowpack"}},"8":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#cornice"}}}}