The most predominant influences on Finland's geography were the continental glaciers that scoured and gouged the country's surface.
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One cause of sea level change is the advance or retreat of continental glaciers caused by climate change.
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It features descriptions of Ice Age times, continental glaciers, and Sioux Quartzite glacial erratics-the oldest rocks in Kansas.
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An example of isostatic uplift would be post-glacial rebound following the melting of continental glaciers and ice sheets.
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All intermediate rock had eroded away before the till was deposited in a ground moraine by continental glaciers.
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Both are glacial remnants after the continental glaciers that scoured and gouged the country's surface 10, 000 years ago.
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Reminding of the period 250 800 years ago the boulder was carried there by a continental glacier from the south of Sweden.
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Over the last century, extensive field observations have provided evidence that continental glaciers covered large parts of Europe, North America, and Siberia.
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During the Pleistocene ( the last ice age ), huge sheets of ice called continental glaciers advanced over much of the earth.
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In successive Ice Ages, both valley and continental glaciers have widened the valleys and the notches of the Catskills and rounded the mountains.
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