What the valley floor is made of
North of the Polson moraine, the Flathead Valley's near-surface ground is glacial: till, outwash, and fine lake-bed silts and clays laid down by an ancestral Flathead Lake that ponded behind the moraine as the ice retreated — commonly with lake beds sitting directly on till. (Not Glacial Lake Missoula, which flooded the valleys south of Polson.)
Montana Bureau of Mines and Geology, Ground-Water Assessment Atlas 2