{"blocks":[{"key":"flri5","text":"Observations from the neighbouring North Columbias may serve to illustrate the kind of activity that likely took place in southern parts of the region midweek. Here, observations show many storm and wind slab releases generally in the size 1.5-2.5 range with several reaching up to size 3. In the Trans-Canada corridor, a size 4 (VERY LARGE) avalanche ran on Mt. Laurie. Activity was likely less pronounced in the north of the Cariboos, which saw closer to 15 cm of new snow.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"bvbqm","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"c85rq","text":"Persistent slab releases have not figured too prominently in reports thus far, but observations are still limited and the few that have been reported are notable. Check out these MIN reports from the Dore River and the Gorge (near Revelstoke) for an example of the isolated deep releases we're concerned about.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":200,"length":10,"key":0},{"offset":215,"length":9,"key":1}],"data":{}},{"key":"3ura1","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"9se4j","text":"Looking forward to Sunday, it's worth continuing to give wind slabs a wide berth as you approach wind affected terrain, and to remain suspicious of steeper sheltered slopes where storm snow may have slabbed up over a layer of surface hoar. Using small test slopes to investigate the bond of the storm snow is a good plan, but be cautious about extending your observations to more committing terrain.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"d5m1a","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"amheu","text":"Forecast new snow will also add to (and obscure) our wind slab problem, while adding just a bit more load to our buried surface hoar. In the north of the region this new load could be critical.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"15htf","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"1dvjs","text":"Since field observations in this region are limited, please consider submitting your observations to the Mountain Information Network. ","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":105,"length":29,"style":"UNDERLINE"}],"entityRanges":[{"offset":105,"length":29,"key":2}],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/4e6d2fbb-0b96-4be7-8e32-71684c85b0c9"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/8bb3db8f-3391-441d-9f27-29d25fdce5b5"}},"2":{"type":"LINK","mutability":"MUTABLE","data":{"href":"https://www.avalanche.ca/mountain-information-network","target":"_blank","url":"https://www.avalanche.ca/mountain-information-network"}}}}