Explanation:
A fault is a product of brittle deformation in which a displacement occurs within the earth.
A normal and reverse fault both have an hanging wall and a foot wall.
- In a normal fault, the footwall moves upward and the hanging wall moves downward thereby causing extension.
- In a reverse fault, the footwall moves downward and the hanging wall moves upward thereby causing shortening.
- The footwall is the block on a side of the fault surface where a miner can stand whereas the hanging wall is the block on the other side.
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In northeastern Ontario there was a large glacial lake, Iroquois, that existed approximately around 13000 years ago. It was a proglacial lake. It was practically an enlargement of today's lake Ontario. It formed because the St. Lawrence River was blocked by an ice sheet, and it drained to the southeast, through a channel passing today's Rome, New York, through the Mohawk River and then in Hudson River. As evidence, there's the sand ridges of Rome, the relief forms in the plains around lake Ontario, the soil structure, the glacial remains.
