— — the cliff the glacier left standing.
“A long ridge of dolostone running roughly 725 kilometres across southern Ontario, from the falls at Niagara to the tip of the Bruce Peninsula. UNESCO named it a World Biosphere Reserve in 1990. The Bruce Trail follows its edge for nearly 900 kilometres of marked footpath. Some of the eastern white cedars clinging to the cliff face are over a thousand years old, the oldest trees in eastern North America.
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The Niagara Escarpment is a continuous ridge of Silurian dolostone capping softer shale beneath. In Ontario it runs from Queenston above the Niagara River north through Hamilton, Milton, Collingwood, and out along the Bruce Peninsula to Tobermory. Total length in the province is roughly 725 kilometres. UNESCO designated the corridor a World Biosphere Reserve in 1990, the first in Canada. The Niagara Escarpment Commission has regulated land use along the corridor since 1973.
The caprock is Lockport dolostone, formed in a shallow tropical sea about 420 million years ago. Erosion of the softer Queenston shale below leaves the dolostone overhanging in cliff bands up to 70 metres high. The same rock layer carries the Niagara River over the falls and forms the cliffs at Rattlesnake Point and the Devil's Pulpit at Cheltenham Badlands. Ancient eastern white cedars cling to the exposed cliff face.
The Bruce Trail follows the escarpment from Queenston to Tobermory, about 900 kilometres of marked footpath maintained by the Bruce Trail Conservancy since 1967. Provincial parks along the route include Niagara Glen, Rattlesnake Point, Mono Cliffs, Bruce Peninsula, and Fathom Five. Toronto is the closest international airport. The grottos at Bruce Peninsula National Park are busiest from late June to early September; a parking reservation is required between May and October.