Your trail guide says that this was formed by a water fall, but it was not. See comments below. A sample of a sandstone log that would have done this, is on display at Miller Hall Museum of Geology at Queens University, on the back wall. It is about a half m. long, and a third m. in diameter. This is 500 million year old conglomerate and orthoquartzites of the Upper Cambrian era.

A photo taken by Steve Manders at the location Ontario with coordinates [44.515721, -76.016644]. Additionally, you might be interested in finding other photos captured by different users near Ontario. Both sets of images could provide a richer perspective of the area and showcase various moments in time.

Your trail guide says that this was formed by a water fall, but it was not. See comments below. A sample of a sandstone log that would have done this, is on display at Miller Hall Museum of Geology at Queens University, on the back wall. It is about a half m. long, and a third m. in diameter. This is 500 million year old conglomerate and orthoquartzites of the Upper Cambrian era. by Steve Manders
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