"Mud glaciers" in the context of the Colorado River/Lake Powell are massive,, thick accumulations of trapped sediment (clays, sand, silt) that build up in reservoirs, acting like slow-moving, viscous flows. They represent a significant,100-million-ton-per-year sediment buildup that reduces reservoir storage capacity, particularly in Lake Powell, acting as a major, yet sometimes debated, management challenge. 
 
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