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Attraction · Blue Mountain, Ontario

Niagara Escarpment

A UNESCO biosphere reserve and long limestone ridge running from Niagara Falls to Tobermory, with Blue Mountain — Ontario's highest ski hill — built on one of its highest points.

Photos of Niagara Escarpment

Visitor guide

About Niagara Escarpment

The Niagara Escarpment is an arc-shaped ridge, or cuesta, about 1,050 km long, running through New York, Ontario, Michigan and Wisconsin. Roughly 725 km of it lies in Ontario, from Queenston on the Niagara River through Hamilton and the Blue Mountain area to Tobermory on the Bruce Peninsula. UNESCO designated it a World Biosphere Reserve in 1990.

How it formed

The escarpment is not a fault. The rock layers show no displacement. It formed through uneven erosion: a resistant dolostone caprock of the Silurian-age Lockport Formation sits over softer shale, which wears away faster and leaves a cliff behind. The Michigan Basin behind the ridge was once the floor of a tropical sea, so the escarpment is, in effect, an old shoreline. Niagara Falls spills over the same escarpment, with the Niagara River cutting its gorge through it.

A wooded section of the Bruce Trail along the Niagara Escarpment in Ontario

Living with the ridge

People have used the escarpment as a barrier and a landmark. The Welland Canal lets ships climb it between Lake Erie and Lake Ontario, and the Erie Canal's locks crossed it at Lockport, New York. In Hamilton, locals call the ridge the Mountain, and incline railways carried people up and down it, the first opening in 1892 and the last closing in 1936. Further north, Blue Mountain, a promontory near Collingwood, is known for skiing and its Scenic Caves. The slopes also support the Niagara Peninsula's vineyards.

Protection and planning

Ontario was early to protect the ridge by law. The Niagara Escarpment Planning and Development Act was passed on 22 June 1973 and set up the Niagara Escarpment Commission, and the Niagara Escarpment Plan was approved on 12 June 1985. The Commission describes the plan area as about 195,000 hectares. The Commission says the plan area takes in portions of 23 local municipalities within seven regions and counties, plus the City of Hamilton.

Cedars and ecology

Wikipedia describes the cliffs as holding the oldest forest ecosystem in eastern North America. Ontario's oldest known tree is reported to be an eastern white cedar dating to 688 AD, growing on the cliffs, although tree-ring dating claims are best read with care. The cliffs, wetlands, caves and varied microclimates shelter a long list of plants and animals, and the ridge links protected areas such as Bruce Peninsula National Park and Mono Cliffs Provincial Park.

The Bruce Trail

The Bruce Trail follows the escarpment from Queenston to Tobermory. The main trail is about 885 to 890 km, with side trails adding several hundred more, and sources describe it as Canada's oldest and longest marked hiking trail. The idea came in 1959 from Ray Lowes, who first shared it with Robert Bateman at a Federation of Ontario Naturalists meeting, and the first committee met in September 1960, and the Tobermory cairn was unveiled in 1967 for Canada's Centennial. The Bruce Trail Conservancy, based in Dundas, maintains it with volunteers, and about half of it crosses public land, while the rest relies on landowner agreements that can be withdrawn.

Visiting tips

For first-time visitors, easy ways to meet the escarpment include the lookouts and parks near Blue Mountain and Collingwood, the Hamilton and Niagara viewpoints, and short sections of the Bruce Trail. Trail conditions, parking and access change with the season, so check the Bruce Trail Conservancy, the conservation authority or Ontario Parks for current hours, tickets and access.

Voyzo's private tours use a private vehicle and driver with door-to-door pickup, so a group can see the escarpment from Niagara through to Georgian Bay without worrying about trail shuttles or parking.

Frequently Asked Questions About Niagara Escarpment

The Niagara Escarpment is about 1,050 kilometres long in total, and roughly 725 kilometres of that length is in Ontario.
It formed through uneven erosion rather than faulting, as a hard Silurian-age dolostone caprock wore away more slowly than the softer shale beneath it.
Yes, UNESCO designated it a World Biosphere Reserve in 1990.
Yes, the water of the Niagara River drops over the escarpment at Niagara Falls, and the river has carved its gorge through the ridge.
The Bruce Trail follows it from Queenston to Tobermory, with a main trail of about 885 to 890 kilometres.
The Niagara Escarpment Planning and Development Act was passed on 22 June 1973, and the Niagara Escarpment Plan was approved on 12 June 1985.
A private vehicle and driver with door-to-door pickup can take your group to escarpment viewpoints, from Niagara to Blue Mountain, at your own pace.
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