Introduction:
| This is what a continental glacier looks like | 
During the past 1 million years there have been three episodes of continental glaciation that has covered the northern hemisphere with vast ice sheets more than two miles thick. Over much of the Midwest  these continental glaciers southern boundaries are today marked by the Missouri Ohio 
The Abitibi:
To the north in Canada Midwest  of the United States Missouri Ohio   Rivers Ohio River  with lesser amounts spread across the states from western New York Missouri 
| A gold mine in the Abitibi Gold Belt, Canada | 
The glacier explains the presence of gold in the northern United   States Ontario 
Gold in the Midwest :
| A terminal moraine in the foreground where the glacier stopped and just dumped its load. | 
A terminal moraine is characterized by a hummocky appearance of many small hills and valleys and large deposits of sand and gravel. Subsequent reworking of the material by streams in a terminal moraine has resulted in the concentration of gold in the channels of streams throughout the area. Most of the gold is concentrated in an area north of the Ohio River , and just to its north, however enough gold was dragged down from Canada Great Lakes  and in thin deposits across the states.  .
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