This appearance results from clays and silts suspended in its waters. These fine-grained sediments result from the erosion of soft clay-rich rocks along the Milk River basin in southern Alberta, such as the Foremost, Oldman and Dinosaur Park formations.
This appearance results from clays and silts suspended in its waters These fine-grained sediments result from the erosion of soft clay-rich rocks along the Milk River basin in southern Alberta such as the Foremost Oldman and Dinosaur Park formations