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I. An Ever Changing Landscape |
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12,000 years ago |
Early arrivals found a forest of thick spruce and bogs in what is now southwestern Minnesota. To the north and east, they found wet tundra with dwarfed spruce and, to the north and west, a huge glacial lake. |
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10,000 years ago |
Minnesota's climate warmed, glacial lakes drained and spruce, fir and tundra landscapes were replaced by a growing deciduous forest of birch, aspen and coniferous trees, such as balsam fir. As the land continued to warm, those forests were replaced by huge stands of white pine, red pine and jack pine. By 8,000 years ago, those trees were giving way to oaks, maples and beech. |
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7,000 years ago |
The climate had warmed so much that prairie ecosystems, called oak savannas, could be found occasionally as far north as what is now the U.S.-Canadian border. |
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5,000 years ago |
The Minnesota climate and the forest ecosystem began another slow change. The climate cooled, and northern prairies receded southward. The northern forests, called the North Woods, evolved once again into hardwoods and eventually into vast stands of red, white and jack pines, white and black spruce, balsam fir, tamarack and white cedar interspersed with mixed hardwoods of birch, maple, oak, elm, aspen, and basswood. |
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4,000 years ago to modern era |
Major climate change slowed and the balance between field and forest remained relatively steady until the present day. European Americans entered these Tall Grass Prairies, Big Woods and North Woods. With increased populations, advancing technology, and a different cultural attitude, they changed the forests and fields again. |
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Minnesota Historical Society · 345 W. Kellogg Blvd., St. Paul, MN 55102-1906 · 651-259-3000 Copyright © 2002 |