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Look Inside The Niagara Escarpment EarthCache

Hidden : 11/26/2007
Difficulty:
1.5 out of 5
Terrain:
2 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Look back thousands of years into history.

The Niagara Escarpment is a long escarpment or cuesta in the United States and Canada that runs westward 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 the western portion of New York and southern Ontario. The escarpment is most famous as the cliff over which the Niagara River plunges to form Niagara Falls, for which it is named.

Niagara Escarpment
The Niagara Escarpment is the most prominent of several escarpments formed in the bedrock of the Great Lakes. It is traceable from its easternmost point in New York State, starting well east of the Genesee River Valley near Rochester, creating a large (and two small) waterfall on the Genessee River in that city, thence running westwards to the Niagara River forming a deep gorge north of Niagara Falls, which itself cascades over the escarpment. In Southern Ontario it stretches along the Niagara Peninsula hugging close to the Lake Ontario shore near the cities of St. Catharines and Hamilton where it takes a sharp turn north toward Georgian Bay. It then follows the Georgian Bay shore north-westwards to form the spine of the Bruce Peninsula, Manitoulin, St. Joseph Island and other 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 following the Door Peninsula and then more inland from the western coast of Lake Michigan and Milwaukee ending northwest of Chicago near the Wisconsin-Illinois border.

From this location you will be able to see inside the escarpment. The bridge crosses the gap made by the entrance to a local quarry and allows the Bruce Trail to continue un-interrupted through the area. Looking out over the quarry you will be able to see back in time many thousands of years by looking at the cross-section of the exposed limestone.

As an experiment, measure the distance from the bridge to the base of the quarry by estimating the distance vertically, and then measuring it horizontally using your GPS.

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