Skip to content

Lake Erie Earthcache EarthCache

This cache has been archived.

H to the Bizzle!: Putting this one in the history books. Thanks to all who found this earth cache over the years.

H to the Bizzle!

More
Hidden : 11/7/2006
Difficulty:
1 out of 5
Terrain:
1 out of 5

Size: Size:   not chosen (not chosen)

Join now to view geocache location details. It's free!

Watch

How Geocaching Works

Please note Use of geocaching.com services is subject to the terms and conditions in our disclaimer.

Geocache Description:

This Earth Cache will take you to a park on Squaw Island, over looking the end of Lake Erie, a magnificent geological feature.

Lake Erie, the great body of fresh water forming Ohio's north coast, is the fourth largest of the five Great Lakes; nevertheless, Lake Erie should not be considered an also-ran, as it is the 12th largest freshwater lake in the world. Lake Erie provides a nearly unlimited water supply to communities along its shore, is an unmatched recreational and sport-fishing mecca, and provides significant quantities of sand and gravel for construction."

"Geologists, however, view Lake Erie in its present form as a very recent feature---less than 4,000 years old---"

"Erie owes its fundamental existence to the presence of a basin or lowland that originated long before the Pleistocene Ice Age began about 2 million years ago. This lowland was the valley of an east-flowing river, known as the Erigan River, that some geologists speculate was the downstream portion of the preglacial Teays River."

"The first of the major glacial advances obliterated this drainage system and deepened and enlarged the basin. Succeeding glaciations further deepened and enlarged it. Lake Erie, the southernmost of the Great Lakes, is also the shallowest because the ice was relatively thin (therefore lacking significant erosive power) when it reached so far south."

"The Lake Erie basin is underlain by Silurian and Devonian carbonates (limestone and dolomite) on the west and by Devonian shales on the east. The carbonate rocks are generally more resistant to erosion than are the shales; therefore, the western basin is comparatively shallow, averaging less than 25 feet in depth. Glacial ice was able to scoop out to a greater extent the less resistant shales underlying the central and eastern basins. The deepest point in Lake Erie is 210 feet in the eastern basin. (http://www.dnr.state.oh.us/geosurvey/lakeerie/lefact1.htm)

To log this Earth Cache, have a photo taken of yourself overlooking the end of Lake Erie and also measure the length from the bottom of the breakwall to the edge of the water to show what the depth was for that day. During the winter time you may include a picture of yourself with the ice boom taking place.

Be sure to find ERIE’S END (GC5FFF) while in the area.

Additional Hints (No hints available.)