{"blocks":[{"key":"910nu","text":"New surface hoar is growing on top of 2- 5 cm of fresh snow that fell overnight between Monday and Tuesday. This covers another layer of surface hoar up to 12 mm in sheltered terrain, and a crust on solar aspects. This crust is reported to be thicker (up to 2 cm) and more likely to be present on steep slopes. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":199,"length":13,"key":0}],"data":{}},{"key":"hnr8","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"4c5f6","text":"In the northern end of the region, the upper snowpack seems to be mostly wind effected, especially in the alpine. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"24uh7","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"4sn8e","text":"This Mountain Information Network post seems to indicate that the surface crust could be thicker and more solid in the south end of the region. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":4,"key":1}],"data":{}},{"key":"9e9ac","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"fdd74","text":"A couple of thin surface hoar and crust layers exist in the upper 40 cm of the snowpack. These layers have not been producing concerning results in recent snowpack tests.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"3bi6k","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"7djp7","text":"The most notable layer of concern in the snowpack is a crust that was formed in early December and is now down 90-160 cm. This layer was reactive early last week producing large size 3 avalanches.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"1qb3o","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"7ft77","text":"Activity has tapered, however, daytime warming, sun, cornice fall, and human triggers from steep, rocky slopes, with a shallow or thin-to-thick snowpack may still be able to trigger this weak layer. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://avalanche.ca/glossary#aspect"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://avalanche.ca/mountain-information-network/submissions/f331278b-1bcf-4273-8d37-1c1b716fbefe"}}}}