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GL / Great Lakes Geology
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Last updated in September, 2000

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    This page presents the geologic characteristics of the Great Lakes. The geologic setting of the Great Lakes basins began far earlier, with the formation of the bedrock in which these basins occur. The foundation for the present Great Lakes basin was set about 3 billion years ago, during the Precambrian Era. Most bedrocks are composed of sedimentary rock of Paleozoic age.  The sedimentary rocks in the Great Lakes formed in a series of of ever-changing oceans that began about 600 million years ago and ended about 225 million years ago. 
   The rock surrounding Lake Superior, the northernmost and deepest of the Great Lakes, is much older igneous and metamorphic rock, Pre-Cambrian in age (one to two billion years old). These igneous and metamorphic rocks were formed by mountain-making processes-volcanoes, intrusions and metamorphism-that were active through much of Pre-Cambrian time. Igneous and metamorphic rocks are the most resistant rocks of all in the Great Lakes region, so the land around the Lake Superior basin is especially high and hilly. These very old rocks actually occur down below the younger, Paleozoic sedimentary rock in the south, forming the so-called Pre-Cambrian "basement" rocks there.
(Forsyth, 1996; The Great Lakes: An Environmental Atlas and Resource Book, 1995).
 
1. What is the oldest fossil that found in the Great Lakes?
2. What is major physical features of Great Lakes rocks?
3. What was Earth's environment like when the rocks of the Great Lakes basin were formed?
 
GS-006 The fossil fauna of the islands region of western Lake Erie.

GS-017 Kelley's Island glacial grooves.

GS-018 Guide to Put-in-Bay (South Bass Island, Ohio): Historical places, natural features, and island ecology.

EP-079 The Great Lake Erie. 
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Chapter 2. The Geological Setting of the Great Lakes 

EP-014 Geography of The Great Lakes

To request these materials, please visit OSG website

 
1. Earth Systems - Education Activities for Great Lakes Schools

Land & Water Interactions in the Great Lakes

  •  When did the rocks in the Great Lakes basin form? 
  •  How were sedimentary rocks in the Great Lakes basin formed? 
  •  How did rocks and rivers shape the Great Lakes? 
  •  What evidence of glaciation exits in the Great Lakes region?
  • What evidence of glaciation and geologic processes can be found on Great Lakes beaches?      

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Geology and Mineral Resources
Source: The Great Lakes: An Environmental Atlas and Resource Book (1995) 

 

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Relief, Drainage and Urban Areas
Source: The Great Lakes: An Environmental Atlas and Resource Book (1995)

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Geologic Time Chart. 
The Great Lakes basin is a relatively young ecosystem having formed during the last 10,000 years. Its foundation was laid through many millions of years and several geologic eras. This chart gives a relative idea of the age of the eras.
source The Great Lakes: An Environmental Atlas and Resource Book (1995)

1. Natural Process in the Great Lakes: Geology
http://www.epa.gov/glnpo/atlas/glat-ch2.html#1

2. Digital geologic map and mineral deposits of the Lake Superior region
http://minerals.usgs.gov/pubs/of97-455/superior.html

3. Great Lakes Science Center - USGS 
http://www.glsc.usgs.gov/

4. Great Lakes Environmental Research Laboratory (GLERL)
http://www.glerl.noaa.gov/pr/about/mission.html

5. Great Lakes Forecasting System (GLFS)
http://superior.eng.ohio-state.edu/nf-index.html


Copyright 1999. Ohio Sea Grant College Program and Earth Systems Education Program of The Ohio State University


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