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Bales of hay on hummocky terrain near the terminal moraine in central Portage County Wisconsin. Look closely to find a hawk perched on hay bale.
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Through the eons, Wisconsin topography has been molded by glaciation. Some 15,000 years ago, the western edge of the Green Bay Lobe extended to just east of Stevens Point Wisconsin. The leading edge of the glacier carried a considerable amount of glacial till that would eventually be deposited on the landscape during times of ice melt. At the terminus of glacier migration, large terminal moraines formed at the site of till release. In other areas of successive glacier advance and retreat, a more irregular deposition of the till formed irregular shaped hills known as hummocks, a geological term for hilly.
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