The underlying bedrock of Michigan is mostly hidden from view by unconsolidated material deposited during continental glaciation. However, there are a number of places in the Lower Peninsula where the bedrock can be seen such as in rock quarries and in outcrops along rivers and lakes. In the western Upper Peninsula, a considerable amount of bedrock is visible.
    The geologic formations of Michigan span more than 3.5 billion years, from some of the oldest Precambrian rocks to loose, unconsolidated drift left behind by the continental ice sheets of the Pleistocene period.
The following series of maps illustrates the general configuration of the geologic basement of the Great Lakes region, and of Michigan.

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gr-lakes-reg-geol-legend.jpg (53816 bytes)

Source:  Image Courtesy of  Randy Schaetzl, Professor of Geography - Michigan State University

The diagram below shows what the structure of the rocks would look like, along transects A-B and C-D.
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Source:  Unknown

Two major rock types are found in Michigan. The Lower Peninsula and the eastern parts of the Upper Peninsula are underlaid by a series of sedimentary rock layers: The Michigan Basin. These rock formations, consisting largely of shales, limestones, and sandstones, were deposited on the bottom of ancient seas that covered Michigan on and off for millions of years. The basin is estimated to be about 14,000 ft (4,267 m) thick, and its rocks rest on the top of a very old Precambrian surface. The various layers of sedimentary rock are piled up on top of one another like a series of saucers.
    The ancient igneous and metamorphic rocks that compose the Precambrian, or Canadian, Shield in the western part of the Upper Peninsula make up the second category of rocks and are estimated to be at least 3.5 billion years old. The igneous rocks are hard, crystalline, resistant to erosion, and are largely made up of granites and metamorphic rocks--rocks that have been changed through heat and pressure--composed mainly of gneisses and schists. The higher areas in the Upper Peninsula are the remnants of ancient peaks that have been worn down over millions of years by the erosive action of wind, water, and moving ice. Thus, the Porcupine and Huron mountains in the western half of the Upper Peninsula have been greatly altered over their long geologic history through uplift and erosion and are now only remnants of once-high mountains.
    Both major types of rocks found in Michigan are important to humans. The igneous type contains valuable minerals such as iron ore and copper, and the sedimentary rocks contain petroleum, natural gas, salt, gypsum, and limestone.

Source:  Unknown

Source:  Unknown

The major rock structures of the Great lakes region are shown in the map below. Notice the Michigan Basin, the Keweenaw
Fault, the Superior Syncline, the Kankakee, Findlay and Cincinnati Arches, and the three iron ranges of the UP. The Wisconsin
Dome is labelled the "Wisconsin Arch" on the map.
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Source:  Unknown

And finally, the map below is a detailed depiction of the Paleozoic rocks of Michigan.


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Source:  Unknown

As you now know, the geology of Michigan is dominated by two rock formations: the sedimentary Michigan Basin, which covers the entire Lower Peninsula and the eastern half of the Upper Peninsula, and the old crystalline, igneous shield found in the western Upper Peninsula. These rocks are covered to various depths by material deposited during the Ice Age. The preglacial topography was much disturbed by the power of these vast ice sheets as they eroded and leveled certain areas and deposited materials in other sections of the state. The present surface is characterized by ridges of sand, gravel, and clay known as moraines, which were deposited as the ice advanced and retreated in the state.
    Within the major landform regions, the great variety of glacial features, each used somewhat differently by humans, results in a large number of smaller regions, some even microscopic in size. In a small area, such as a county, three of four or more local landform categories can be identified.

Parts of the text on this page have been modified from L.M. Sommers' book entitled, "Michigan: A Geography".

This material has been compiled for educational use only, and may not be reproduced without permission.  One copy may be printed for personal use.  Please contact Randall Schaetzl ( for more information or permissions.