Bethany Hills, Omemee Esker and Fleetwood Creek Stop 2: opposite Lake Peterborough Glacial Lake Peterborough had many attributing spillways attached to it, feeding melt pissing and sediment from the ice margin and or other glacial lakes. Much of the sediment that was deposited in Glacial Lake Peterborough came from either from the stagnant ice blocks located on the oak Ridges moraine or from the Lake Algonquin drainage system. Much of the deposition in this lake was dominated by sediment stratification, which may have been largely influenced by thermic stratification.
As a result of thermal stratification occurring in this glacial lake sediment inputs were greatly influenced depending on the different sediment densities between the lake bottom water to that of the debut meltwater and if the inflow density was less/more than the bottom water than the lake water bottom, than new transport and depositional classs were created Depending on the type of path that was created, it would...If you want to get a full essay, order it on our website: Ordercustompaper.com
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