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Glenridge in St. Catharines in Niagara Region, Ontario — Central Canada (North America)
 

History of the Niagara Escarpment

 
 
History of the Niagara Escarpment - Marker image. Click for full size.
Photographed by Kevin Westell, July 12, 2026
1. History of the Niagara Escarpment - Marker
Inscription. Glenridge Quarry Naturalization Site
Niagara Region
History of the Niagara Escarpment
The story of the Niagara Escarpment began 450 million years ago when an upheaval in the earth's crust resulted in the formation of a great range of mountains along the eastern edge of North America.

Did You Know? The old-growth forests, located along the cliffs of the Escarpment, include trees that are more than 1,000 years old!

Geological Overview: Over time, the range of mountains were scoured by the forces of wind, rain, and ice. Rivers carried the eroded material westward. When the rivers met a large and shallow sea, known as the Michigan Basin, they deposited the mountain's sediment and formed an immense river delta. These sediments then hardened into the red shale and sandstone rocks that form the base of the Escarpment.

Over the next 100 million years, the warm seas withdrew and left a wide, fat plain in their wake. New rivers carved out narrow valleys in the plain. Ice, wind, and water worked along the river's outer edge to slowly remove weaker shale layers underlying more resistant
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caprock. Large blocks of dolostone broke off the top and created the vertical face that characterizes the Escarpment. The mechanism, known is the capping process, continues today.

The Ice Ages characterized the next 325 million years. In fact, the last three kilometres of thick sheet ice melted away only 12,000 years ago. Since the receding of the glaciers, the forces of erosion have continued to change the face of the Escarpment.

Water's chemical action slowly dissolves porous dolostone and constantly creates new caves and crevices. The Niagara Gorge was carved by the force of running water over the last 13,000 years. Patches of gleaming white ice along the exposed face of the Escarpment indicate that frost action has broken off another piece of rock and sent it hurtling to the slope below.

Today's Living History: Today's Niagara Escarpment is home to a wide variety of plants and animals. There are over 36 species of reptiles and amphibians, 53 species of mammals, 90 species of fish, and more than 300 species of birds. Many of these species are rare and can't be found anywhere else Ontario. Topography
Glenridge Quarry Naturalization Site - Entrance to Trails image. Click for full size.
Photographed by Kevin Westell, July 12, 2026
2. Glenridge Quarry Naturalization Site - Entrance to Trails
Photo faces north, from the parking lot's drop-off loop. Six information panels are near the sun shelter.
and soils associated with the Escarpment combine with other elements to produce an ideal habitat for plant materials characteristic of the Carolinian Forest Zone.

Snapshots of the Niagara Escarpment Development Through Time
- 450 Million Years Ago
--- Mountains along the eastern edge of North America
--- Michigan Basin and Delta
- 425 Million Years Ago
--- Sea
- 325 Million Years Ago
--- River
- Ice Age
--- Glacier
- Present
--- Escarpment
 
Topics. This historical marker is listed in this topic list: Natural Features. A significant historical year for this entry is 9999 BCE.
 
Location. 43° 7.16′ N, 79° 14.363′ W. Marker is in St. Catharines, Ontario, in Niagara Region. It is in Glenridge. It can be reached from Sir Isaac Brock Way, on the right when traveling west. Marker is in a cluster of panels, 100 metres north of the road, at the parking lot and trailhead. Touch for map. Marker is at or near this postal address: 1860 Sir Isaac Brock Way, St Catharines ON L2T 1W2, Canada. Touch for directions.

Regionally, this marker is on Ontario’s Golden Horseshoe and in Niagara Canada.
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It is also in Central Canada. Globally, it is in North America, the Western Hemisphere, the Western World, and the Anglosphere. Historically, it finds itself in what was once a British colony, the Viceroyalty of New France, the Haudenosaunee (Iroquois) Confederacy, and Rupert’s Land.

Other nearby markers. At least 8 other markers are within walking distance of this marker: About the Glenridge Quarry Naturalization Site (here, next to this marker); Land Acknowledgement (here, next to this marker); History of the Site - Use as a Quarry and a Landfill (a few steps from this marker); Weather Station: Stormy Weather (approx. 0.3 kilometers away); A Brief History of Time (approx. 0.3 kilometers away); Renewable Energy: Solar and Wind Power (approx. 0.3 kilometers away); The Solar System (approx. 0.4 kilometers away); Renewable Energy: Water Power (approx. 0.4 kilometers away). Touch for a list and map of all markers in St. Catharines.
 
More about this marker. Captions:
Left: Bruce Trail in Grimsby at Beamer Memorial Conservation Area
Left Centre: Niagara Falls
Right Centre: Balls Falls Conservation Area
Background: Niagara Glen Nature Reserve
 
 
Credits. This page was last revised on July 13, 2026. It was originally submitted on July 13, 2026, by Kevin Westell of St. Catharines, Ontario. This page has been viewed 4 times since then. Photos:   1, 2. submitted on July 13, 2026, by Kevin Westell of St. Catharines, Ontario.
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Jul. 15, 2026