This report documents the findings of a comprehensive survey that investigated the extent to which river ice influences channel bathymetry along the Fort Peck reach of the Missouri River. The Fort Peck reach stretches about 170 miles from Fort Peck Dam, Montana, to Lake Sakakawea, North Dakota. The reach comprises a channel of alluvial sinuous-braided morphology historically known for its shifting thalweg and erosion-prone banks. The survey, which entailed extensive monitoring and detailed measurements of channel bathymetry, ice conditions, and flow velocity distribution, was conducted at five sites during the winter of 1998-99. The observations and data, though still preliminary and incomplete, indicate fundamental processes whereby river ice formation may influence channel bathymetry along the Fort Peck reach, as well as other flow-regulated, alluvial-channel rivers. Prior to the survey, the river ice processes had only been conceptualized