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This photo is looking up the slope from the toe of the debris. The debris was 6-8 feet deep and 40 feet wide.  The slide ran 300 feet vertical and was 50 feet wide at the crownline.  Average slope angle at the starting zone was 40 gress and 36 degrees steepness at the trigger point. The avalanche released on a layer of small-grained facets 1.5 to 2 feet from the surface. Photo: GNFAC
 

Northern Madison, 2014-02-17

Consistent snowfall and strong winds pushed many slopes past their breaking point in the mountains near Quake Lake. These slides were breaking 2-3 feet deep and propagating hundreds of feet wide. Photo GNFAC
 

Southern Madison, 2014-02-16

A skier near Bacon Rind in the southern Madison Range triggered this slide from the top of the slope. The slide failed on a layer of surface hoar. Photo M. Carey

Southern Madison, 2014-02-16