{"blocks":[{"key":"rd6g","text":"20-50cm of low density snow sits over a supportive crust up to 2400m on all aspects. In the high alpine, storm snow sits on a variety of wind affected surfaces.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"dnoae","text":"Westerly winds have redistributed new snow into deeper deposits in wind loaded features at higher elevations.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"ce4ph","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"6hl5a","text":"A surface hoar layer extends throughout the Toby Creek drainage and surrounding areas - down 30 to 70 cm in sheltered features at treeline and below. Recent snowpack tests have shown this layer to produce sudden propagating fractures. We have limited knowledge of the distribution of this layer, but suspect is its most prevalent between 1900-2400m.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":212,"length":11,"key":0}],"data":{}},{"key":"c209q","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"fplak","text":"A late October facet/crust layer of concern sits at the bottom of the snowpack above 1900m. This layer has been reactive to human and explosive triggers, producing large avalanches. This layer is widespread throughout the region and will likely continue to be a layer of concern.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"836k","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"312tv","text":"Average snowpack depth at treeline is 100-180cm, with the deepest snowpack found near the Bugaboos. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#propagation"}}}}