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View
an animation
of the valley formation.
Requires the flash plug-in. Download here. |
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| Ice
Age - Glacial Advances and Retreats
To understand the present Minnesota River Valley, you have to step back
in time when glaciers covered Minnesota. During
the ice age, the climate was colder and glacial ice covered a large portion
of North America. There were four major periods of glaciation where glaciers
advanced and retreated across the landscape.
The most recent glacial advance, called the Wisconsin Glaciation, spanned
from about 100,000-10,000 years ago. Throughout the Wisconsin Glaciation,
lobes of glacial ice pushed in different directions across Minnesota's
landscape. The landscape we see today is dramatically shaped by these
glaciers. The map shows the maximum extent of the ice coverage during
the last glacial advance (Wisconsin glaciation).
Learn more about the history of glaciers in
Minnesota
Map adapted from Richard W. Ojakangas and Charles L. Matsch's
Minnesota's Geology. University of Minnesota Press, Minneapolis,
1982. |
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Lake
Agassiz
About 12,000 years ago, the glaciers melted back to the
topographic divide (near the North Dakota/South Dakota border). Glacial
meltwater was trapped and accumulated, creating Lake Agassiz.
To get an idea of
the immense size of Lake Agassiz, it was bigger than all of the present
day Great Lakes combined.
The
map shows the total area covered by Lake Agassiz (about 123,500 square
miles). It had a maximum depth of about 400 feet. The borders of the lake
changed with the shifting ice margins so the lake was never this large
at any one time.
Map adapted from John Tester's Minnesota's Natural Heritage.
University of Minnesota Press, Minneapolis, 1995. |
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River
Warren
Lake
Agassiz drained in a variety of directions over the years. From 11,500-11,000
and 9,900-9,200 years ago, Lake Agassiz drained through the Minnesota
River Valley. Lake Agassiz overtopped a moraine dam (near present day
Browns Valley) and an outlet river was created. This outlet, called Glacial
River Warren, drained south and carved the Minnesota River Valley. The
drainage shifted to Hudson Bay about 8,500 years ago.
Map
adapted from Richard W. Ojakangas and Charles L. Matsch's Minnesota's
Geology. University of Minnesota Press, Minneapolis, 1982. |
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River
Warren
This diagram illustrates the scale of the mighty River Warren. The torrent
of water that flowed out of Lake Agassiz carved out the large Minnesota
River Valley that spans up to five miles across in some places (scroll
over image for labels). A huge volume of water filled the valley from
bank to bank.
Note the present day Minnesota River is comparatively tiny, shown meandering
through the large valley carved by mighty Glacial River Warren.
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Cross
Section of River Warren and Present Minnesota River
This cross section of the Minnesota River at the Mandota Bridge
illustrates the small size of the modern Minnesota River compared to the
scale of the massive River Warren.
Graphic adapted from Edmund Bray's Billions of Years in Minnesota: The
Geological Story of the State. Science Museum of Minnesota, St. Paul,
1980.
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References:
Bray, Edmund. Billions of Years in Minnesota: The Geological Story of
the State. Science Museum of Minnesota, St. Paul, 1980.
Ojakangas, Richard W. and Charles L. Matsch. Minnesota's Geology.
University of Minnesota Press, Minneapolis, 1982.
Tester, John. Minnesota's Natural Heritage. University of Minnesota
Press, Minneapolis, 1995. |
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home
This
page was last updated 11/15/04
Minnesota River Basin
Data Center | Minnesota State University, Mankato
184 Trafton Science Center S, Mankato, MN 56001 | Phone: (507)389-5492
| FAX: (507)389-5493 | Email: mrbdc@mnsu.edu
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