{"blocks":[{"key":"4gmd8","text":"Below 2000 m (1000 m in the north end of the region), 10-30 mm of rain fell throughout the day on Wednesday, soaking the upper snowpack. In most places, a firm crust has formed on the surface. At treeline, this crust may be supportive to skis and snowshoes, but breakable under a snowmobile or a boot. Below treeline, the crust is thinner, weaker, and overlies moist snow.\n","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2ip5u","text":"Above 2000 m in the southern end of the region there are areas that received up to 30cm of snow, but observations so far suggest that this terrain was hammered by the wind, scouring some terrain and forming unreactive wind effected surfaces elsewhere.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"60np","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2re64","text":"See here for a summary of the conditions in the Microwave area from our field team.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":4,"length":4,"key":0}],"data":{}},{"key":"e03eg","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"5n4sl","text":"In the northern end of the region, where there was still dry snow available for transport, Thursday's wind formed reactive windslabs in the alpine. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"v0a9","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"396pm","text":"In some areas a combination of two thin crusts with faceting above and below exists 40 to 50 cm deep. Deeper in the snowpack, two weak layers may exist around 60 to 120 cm deep. The first is a surface hoar layer from mid-January and the second is a layer of faceted snow from early January. These layers haven't produced recent avalanches, but they are producing concerning results in snowpack tests, and the potential remains until these layers bond to the snowpack.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://avalanche.ca/mountain-information-network/submissions/0efb0265-8ad2-11ec-9319-52ee8ee72627"}}}}