{"blocks":[{"key":"ek7bs","text":"Melt freeze and sun crusts may be found at the surface on steep solar aspects.  Recent moderate to strong southwest to westerly winds have stripped low density snow off the windward sides of alpine and exposed treeline and redistributed snow into hard and soft wind slabs in immediate lees of ridge crests.  Surface wind slabs may overly buried wind slabs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":20,"length":6,"key":0},{"offset":261,"length":10,"key":1},{"offset":285,"length":4,"key":2}],"data":{}},{"key":"1lnid","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"c4oug","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.  The mid-pack is well settled and strong.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":8,"length":10,"key":3},{"offset":133,"length":8,"key":4},{"offset":213,"length":7,"key":5}],"data":{}},{"key":"5ardh","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"alrhf","text":"The bottom 20 cm of the snowpack consists of basal facets and decomposing crusts that have not been an active avalanche problem since December, but could reemerge as a problem with a large trigger such as a Cornice fall, particularly in shallow rocky start zones.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":45,"length":12,"key":6},{"offset":237,"length":25,"key":7}],"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"}}}}