Niagara Falls Geological History
The Story of the Falls began 600 million years ago. The future site of the Great Lakes stood at the centre of a broad, shallow sea that covered much of North America. Beneath these waters were the already ancient Pre-Cambrian rocks of the Canadian Shield-the bowl- shaped basement of our continent.
For 100 million years, rain and wind and the lapping of waves ground rocks into powder. This material collected, layer after layer, in the concave sea bottom, depositing soft sediments over top of the harder Pre-Cambrian rock.
Suddenly, the Earth shook, pushing forth the Appalachian mountains. Rivers flowed in new patterns, carrying mud westward. Where the rivers intermingled, huge muddy deltas formed, sprawling over 600 kilometres, from east of what is now Lake Ontario to beyond the present shore of Lake Huron. That mud, cemented by the eons, forms the distinctive purple-red shale called the Queenston Formation and the sandy ledge-forming rocks of Niagara Gorge.
The waters over the future site of the Falls were tropical, for Central North America lay much closer to the equator than it does today. In this warm sea, tiny creatures built massive honeycombed reefs that appeared as gray and white shoals in the troughs of waves. As these coral makers died, the churning of water broke up their homes, sent in a rain of lime dust to the sea floor. The Lockport Dolomite, which forms the caprock of the Niagara Escarpments, consists largely of these ground up coral reefs.
By 300 million years ago, the inland sea had drained away. Its legacy: a saucer of sediments atop the Pre-Cambrian shield nearly five kilometres deep. Fifty million years later, while the first reptiles were slowly establishing their dominion over the planet, great rivers crisscrossed central North America, etching patterns into this soft, sandy rock and undermining the harder limestones. This random erosion formed the basins for Lakes Michigan and Huron, and later, Erie and Ontario.










































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