{"blocks":[{"key":"a27ea","text":"Light new snow amounts and bouts of elevated wind may have formed small new wind slabs in exposed leeward terrain while creating lightly wind-affected surfaces elsewhere. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"6asct","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"c3k1f","text":"Previous small wind slabs have largely stabilized, but concern still exists for the ability of large triggers like cornices or machines to trigger older large, hard wind slabs in alpine areas.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"cga5i","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"70s8","text":"There are no deeper concerns around White Pass.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"at5u6","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"bo477","text":"Substantial spatial variability likely still exists in the snowpack around the Tutshi Lake/Paddy Peak area. Terrain here should be assessed on a slope by slope basis, as lingering snowpack weaknesses may still exist.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":79,"length":22,"key":0}],"data":{}},{"key":"t1ca","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"b1fbk","text":"The Wheaton's continental snowpack is dominated by hard wind slabs overlying sugary facets and depth hoar. It's an untrustworthy snowpack structure that requires conservative terrain selection and diligent travel habits.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/95db6586-8aa6-11eb-8bbf-f2099c185405"}}}}