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Ball’s Falls (tee hee) Conservation Area is located in the Twenty Valley watershed in Jordan, Ontario. The area is named after John and George Ball, soldiers who received land for their loyalty to the British Crown in 1783.

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The Niagara Escarpment was formed and existed before glaciations, approximately 430 – 415 million years ago.

The Niagara Escarpment was formed before the formation of the Niagara Falls and before the dinosaur extinction.

Only five kilometers west of Lewiston, New York, the escarpment is so steep that it raises 73 meters (240 feet) above sea level in 0.4 kilometers (1/4 mile).

The eastern portion of the Niagara Escarpment at Watertown, New York is 147 meters (483 feet) above sea level is higher than in the west at Hamilton, Ontario the escarpment is 35 meters (116 feet) above sea level.

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