{"blocks":[{"key":"6dfvj","text":"Up to 25 cm of low density snow over the past several days has combined with intermittent northwest winds to create wind slabs which may be possible to human trigger in specific lee features. In sheltered areas, cohesion-less powder may be prone to dry loose avalanches that can run far and fast in these cold, dry conditions. With clear skies, there is uncertainty as to how much direct sun on Tuesday might warm steep slopes midday given the frigid temperatures. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2o743","text":"40-70 cm of snow from the past week is settling over a reactive weak layer of surface hoar. Reactivity on this layer has primarily been observed at treeline and in \"treeline-like\" features that are below treeline. Snowpack tests results continue to show the potential for propagation on this layer, like this MIN report from near Barkerville on Sunday. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":78,"length":12,"key":0},{"offset":309,"length":10,"key":1}],"data":{}},{"key":"610ds","text":"A second weak of layer of surface hoar from mid January is down around 70-110 cm and is most prevalent in sheltered, open slopes at treeline and below. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"eslc8","text":"Deep persistent weak layers can still be found in the lower snowpack. These weak layers are most likely to be triggered from rocky areas with a shallow or thin to thick snowpack.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"href":"https://www.avalanche.ca/glossary#surface-hoar","target":"_blank","url":"https://www.avalanche.ca/glossary#surface-hoar"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/7d535bff-3285-4d4f-8d0c-b878e2fffa41"}}}}