{"blocks":[{"key":"c2qh2","text":"Avalanche hazard is highly variable and dependent on snowfall amounts and freezing lines experienced locally by this recent storm. Cooler temperatures and the passing of the storm mean that the natural avalanche cycle have tapered.  However, reports are coming in reporting the poor bond of the new snow to rain crusts near the surface. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"ffhok","text":"Additionally, on Wednesday avalanche control work was able to trigger large avalanches on the Nov 5 rain crust deep persistent layer in northerly shallow rocky terrain around 2000m.  This elevation would have been below the recent inversion, which further weakening the crust.  Elsewhere, numerous reports have come in describing the poor bond of new snow to the recent rain crusts producing small to large avalanches.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"167t8","text":"On Tuesday, at the peak of the cycle, reports of large avalanches (Size 2) naturally and from skier controlled and explosive control work on Tuesday .  A few Very Large (Size 3) Natural avalanches were reported running to valley bottom along the highway corridor.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"egdp9","text":"Our eyes and ears in the mountains are limited this winter due to fewer professional observations. If you go out in the mountains, please share your observations on the Mountain Information Network (MIN). Photos are especially helpful! Thank you so much for all the great MINs submitted so far!","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":236,"length":17,"style":"BOLD"}],"entityRanges":[{"offset":169,"length":34,"key":0}],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"href":"https://avalanche.ca/mountain-information-network/submit","target":"_blank","url":"https://avalanche.ca/mountain-information-network/submit"}}}}