{"blocks":[{"key":"2dre7","text":"On Saturday, a natural size 2.5 persistent slab was reported on a northeast aspect in the alpine. This avalanche propagated 300 m wide and is assumed to have failed on the February crust/facet layer. A variety of natural loose wet avalanches up to size 2 were also reported. One of these triggered a slab which failed down 50-80 cm, presumably on the crust/facet layer. Some natural cornice failures were also reported which had occurred sometime in the past three days and had triggered slabs on the slopes below. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"3ji6a","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"3q0dn","text":"On Friday, three size 1.5-2 persistent slab avalanches were human triggered and failed on a weak crust/facet layer buried late-February. This MIN report describes one of them which was on a west aspect at around 1950 m and released down 50 cm. Another was on an east aspect at around 1800 m elevation and the third was on a steep convex feature at treeline. Some human-triggered loose dry avalanches were observed on north aspects and some solar-triggered loose wet avalanches were observed on steep sun-exposed slopes. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":142,"length":10,"key":0}],"data":{}},{"key":"32gke","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"dq42o","text":"On Thursday, several persistent slab avalanches were reported up to size 2.5. Four of these were natural and the rest were human-triggered including one which was remotely triggered. Two of the naturals were on south aspects which were triggered by loose wet avalanches stepping down. Most of the rest of the activity was on northerly aspects. The majority of the activity appears to have occurred between 1600 and 2000 m elevation. Slab thickness was typically 30-70 cm and the failure plane was a combination of the mid-February and late-February weak layers which may be acting as more of a single thick weak layer. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/97a9a56b-621c-4836-a2bf-ea829c869ae5"}}}}