Below treeline (& possibly up to 2400m): High freezing levels and rain events created a rain crust (or two).  New snow is not bonding well to these near surface rain crusts.  This is more of a concern if the new snow over crust is more than 20cm, however even stuffs are being reported as running \"far and fast\".","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":15,"style":"BOLD"},{"offset":39,"length":2,"style":"BOLD"},{"offset":107,"length":3,"style":"BOLD"}],"entityRanges":[],"data":{}},{"key":"en5ue","text":"At and near tree line, the 15-40cm of new snow fell on a widespread layer of large surface hoar crystals.  While some lower elevation areas have seen this Surface Hoar destroyed by the rains, it is likely intact in higher, drier, colder locations near tree line and elsewhere.  Shooting cracks, remote triggering and settlements (whumphing) are classic signs of instability that buried surface hoar is present and potentially reactive. Snow that has been wind affected may be most reactive.  ","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":21,"style":"BOLD"}],"entityRanges":[{"offset":83,"length":12,"key":0},{"offset":278,"length":15,"key":1},{"offset":353,"length":20,"key":2}],"data":{}},{"key":"2dihu","text":"At upper elevations where recent winds transported new snow, storm slabs formed in lee features (Northerly and Easterly slopes) and will be more reactive where they sit over a crust.","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":20,"style":"BOLD"}],"entityRanges":[{"offset":176,"length":5,"key":3}],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary?q=surface+hoar#surface-hoar"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary/#shooting-cracks"}},"2":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary?q=remote#signs-of-instability"}},"3":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https