Niagara Escarpment

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Rattlesnake Point near Milton, Ontario.
Blue Mountains near Collingwood, Ontario.
Niagara Escarpment (in red)

The Niagara Escarpment is a long escarpment, or cuesta, in the United States and Canada that runs predominantly east/west from New York State, through Ontario, Michigan, Wisconsin and Illinois. It is composed of the Lockport geological formation of Silurian age, and is similar to the Onondaga geological formation, which runs parallel to it and just to the south, through western New York and southern Ontario. The escarpment is most famous as the cliff over which the Niagara River plunges at Niagara Falls, for which it is named.

The Niagara Escarpment is the most prominent of several escarpments formed in the bedrock of the Great Lakes basin. From its easternmost point near Watertown, New York,[1] the escarpment shapes in part the individual basins and landforms of Lakes Ontario, Huron and Michigan. In Rochester, New York, there are three waterfalls over the escarpment where the Genesee River flows through the city. The escarpment thence runs westward to the Niagara River forming a deep gorge north of Niagara Falls, which itself cascades over the escarpment. In southern Ontario it spans the Niagara Peninsula, closely following the Lake Ontario shore through the cities of St. Catharines, Hamilton and Dundas, where it takes a sharp turn north in the town of Milton toward Georgian Bay. It then follows the Georgian Bay shore northwestwards to form the spine of the Bruce Peninsula and Manitoulin Island, as well as several smaller islands located in northern Lake Huron where it turns westwards into the Upper Peninsula of northern Michigan, south of Sault Ste. Marie. It then extends southwards into Wisconsin[2] following the Door Peninsula through the Bayshore Blufflands and then more inland from the western coast of Lake Michigan and Milwaukee, ending northwest of Chicago near the Wisconsin-Illinois border.


Study of rock exposures and drillholes demonstrates that there is no displacement of the rock layers at the escarpment: this is not a fault line but the result of unequal erosion. The escarpment's caprock is dolomitic limestone ("dolostone"), which is more resistant and overlies weaker, more easily eroded shale as a weathering-resistant "cap". The escarpment thus formed over millions of years through a process of differential erosion of rocks of different hardnesses. Through time the soft rocks weather away or erode by the action of streams. The gradual removal of the soft rocks undercuts the resistant caprock, leaving a cliff or escarpment. The erosional process is most readily seen at Niagara Falls, where the river has quickened the process. It can also be seen at the three waterfalls of the Genesee River at Rochester (additional resistant rock layers make more than one escarpment in some places). Also, in some places thick glacial deposits conceal the Niagara Escarpment, such as north of Georgetown, Ontario, where it actually continues under glacial till and reappears farther north.

The dolostone cap was laid down as sediment on the floor of a marine environment. In Michigan, behind (southwest of) the escarpment, the cuesta capstone slopes gently to form a wide basin, the floor of an Ordovician-Silurian-age tropical sea. (The escarpment essentially represents the remnant shoreline of that sea.) There the constant deposition of minute shells and fragments of biologically-generated calcium carbonate, mixed with sediment washed in by erosion of the virtually lifeless landmasses, eventually formed a limestone layer. During the Silurian period, some magnesium substituted for some of the calcium in the carbonates, slowly forming harder (dolomitic) sedimentary strata in the same fashion. Worldwide sea levels were at their all-time maximum in the Ordovician; as the sea retreated, erosion inevitably began.[3]

This dolostone basin contains Lakes Michigan, Huron and Erie. (The geological formations under Lakes Superior and Ontario were formed from volcanic rifts. Soft basalt line its canyon walls, bottoming at 1300 feet below sea level.)

Human geography

The Welland Canal allows ships to traverse the escarpment between Lake Erie and Lake Ontario on the Niagara Peninsula of Ontario. The escarpment was a major obstacle in the construction of the Erie Canal in New York and was traversed by a series of locks; the community which grew up at the site thus became known as Lockport, New York.

In southern Ontario, the Bruce Trail runs the length of the escarpment from Queenston on the Niagara River to Tobermory on the Bruce Peninsula. Highway 401, Canada's busiest, also crosses the Niagara Escarpment, beginning its long descent through rolling hills, farmland, and towns west of Milton. Rock exposed on the face of the escarpment can be seen along Highway 26 from Owen Sound eastwards towards Meaford, Ontario.

Hamilton, Ontario, is situated on the escarpment in such a way that the north end of the city is below and the south part above. Affectionately referred to as "The Mountain" by its residents, there are many roads or "mountain accesses" that join the urban core below with the suburban expansion above.

High Cliff State Park in Wisconsin shows how modern and prehistoric humans used the escarpment for not only cultural reasons but economic gains as well. There are a number of different animal and geometric effigy mounds and the remains of an early twentieth century limestone quarry and kiln within the park.

The relief and exposed edge is used by several wind farms stretching from Pipe, Wisconsin to Brownsville, Wisconsin. Wind speeds average 18 mph (about 29 km/h) along this stretch.

The Niagara Escarpment is a prominent feature just east of Fond du Lac, Wisconsin, and it is known there as "The Ledge".[4] Some local organizations take their name from it, including The Ledgers, the sports teams at St. Mary's Springs Academy, which is perched on the side of the escarpment.

Many resorts and ski areas in Ontario, Michigan, Wisconsin and New York are located along the escarpment.

Vineyard land

Niagara County, New York, near the eastern end of the escarpment, is the site of the 18,000 acres (7,284 ha) Niagara Escarpment AVA (American Viticultural Area).[5] Wines produced in this region range from traditional grape varieties such as Merlot, Cabernet Franc, Cabernet Sauvignon, Chardonnay, and Riesling, to fruit wines.

Ontario's Niagara Peninsula is the site of the largest wine-producing appellation (region) in Canada. Cool-climate varieties such as Riesling, Chardonnay, Gamay Noir, Pinot Noir and Cabernet Franc are among the more than 30 varietals produced across 13,600 hectares (33,606 acres). Three sub-appellations lay along the benchlands of the Niagara Escarpment. They are: Short Hills Bench, Twenty Mile Bench, and Beamsville Bench.[6]

Northeastern Wisconsin, at the western end of the escarpment, is the site of the 3,800 sq mi (9,800 km2) Wisconsin Ledge AVA.[7] Most of the region's vineyards lie upon the escarpment's eastern-facing slope that rise gently upward from the shores of Lake Michigan to the top of the Ledge, before dropping sharply off into Green Bay, and benefit greatly from constant air movement from Lake Michigan, which stores warmth during the summer. The presence of the lake produces a vacuum of sorts during the growing season: warm air over the lake rises, sucking colder air off the land and creating offshore breezes. Cold air cannot settle over the vineyards and there is a constant flow of warmer air, making the growing season here longer than in other parts of the state. The escarpment's glacial soils are made up of gravel, sand and clay over limestone bedrock. A subterranean aquifer provides mineral-rich ground water to the vines, encouraging deep root growth.[8][9]

World Biosphere Reserve

In February 1990, the Niagara Escarpment was designated a World Biosphere Reserve by UNESCO, making it one of 12 in Canada. Development and land use on and adjacent to the escarpment is regulated by the Niagara Escarpment Commission, an agency of the Ontario government.[10]

See also


External links