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65Trip D THE LATE PLEISTOCENE OF THE CHAMPLAIN VALLEY, VERMONT by W. Philip Wagner Department of Geology University of Vermont Burlington, Vermont INTRODUCTION The existing knowledge of Pleistocene
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Research the characteristics of the Late Wisconsinan Ice Sheet.
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The Late Wisconsinan Ice Sheet refers to the last major glacial period in North America that peaked approximately 20,000 years ago, covering large areas of Canada and parts of the northern United States.
The term 'filing' does not apply to the Late Wisconsinan Ice Sheet in a traditional sense, as it is a geological feature rather than a legal or fiscal document.
There is no form to fill out related to the Late Wisconsinan Ice Sheet, as it is a geological structure studied by scientists and researchers.
The study of the Late Wisconsinan Ice Sheet helps scientists understand past climate changes, glacial dynamics, and their impacts on sea levels and ecosystems.
Information related to the Late Wisconsinan Ice Sheet primarily involves geological data, sediment analysis, and climate history rather than a specific reporting requirement.
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