niagara escarpment geology - Search
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    Highly fractured sandstone, shale and carbonates
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    The Niagara Escarpment is a geological feature located in southern Ontario, Canada, and the northeastern United States. It is composed of highly fractured sandstone, shale and carbonates deposited during the Ordovician and Silurian periods. The escarpment is not a fault line but the result of unequal erosion. It has a caprock of dolostone which is more resistant and overlies weaker, more easily eroded shale rocks. The present appearance of the Niagara Escarpment is the result of erosion that’s occurred over the past 250 million years.

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