The shaping of Michigan's geological landscape began more than one million
years ago, during the great Ice Age. Her features were sculpted by four massive
continental glaciers scouring across the Midwest. Michigan experienced the last
great ice sheet, known as the Wisconsin Glacier, about fourteen thousand years
ago. This huge ice mass was a mile thick and almost four million miles square.
Its northernmost head touched Hudson Bay, and its icy tongue reached toward the
banks of the Ohio River. As this "river of ice" crept over the underlying rocks,
its base scraped millions of tons of earth like a giant bulldozer over the land.
This debris composed of soil, pebbles, cobbles and boulders was pushed forward,
grinding rocks into glacial dust, while boulders scratched their signatures on
the bedrock.
Then the climate began to warm. Meltwater carried the soils and rocks away
from the melting glacier, depositing its drift over the landscape. As this blend
of soils and rocks was dropped away from the ice, the low hills, or moraines,
were created across the state. Michigan's glacial drift averages 200 to 300
feet; however, the thickness of drift has measured over 1,000 feet in a few
Michigan locations and is non-existant in others. The grinding of boulders created particles of various sizes
and weights. The heaviest pieces fell first, forming stony ridges which formed
the stream's flow direction and the edge of the glacier as it melted. Lighter
materials were carried farther, dropping along the way as the flowing water
slowed. These materials dried in sheets forming vast, flat multi colored areas
of sand, silt, clay and a mixture of the three called outwash plains.
The weight of the glacier over the Michigan basin was lessening, and the
earth began to rebound, like a sponge returning to its original shape when the
squeezing stops. The Michigan landscape began to emerge like a slowly rising
phoenix. Plants began to appear on the drying landscape. Communities formed as
various plants found a suitable growing environment near each other.