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Dissertation Defense |
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Candidate: Linda Nicks Degree of: Doctor of Philosophy
Committee: Dr. Alan Kehew, Chair Abstract: The objective of the dissertation was to map the glacial geology in southern St. Joseph County, Michigan. St. Joseph County was selected because the county has only been mapped at a scale of 1:500,000 and has significant problems involving the surficial geology, including point-source and non point-source contamination of shallow, vulnerable aquifers. The study area lies at the convergence of three lobes of the Laurentide Ice Sheet; the Lake Michigan, Saginaw and Huron-Erie Lobes. The Sturgis Moraine is a prominent ridge transecting the study area. The topography is dissected by southwest-trending channels. The moraine is an important resource in St. Joseph County because of its ability to store and discharge groundwater and supports major streams in the area. The study area consists of a complex succession of coarse-grained sediments (aquifers) and fine-grained tills (aquitards) at depth. All diamictons and till exist in the subsurface and are rarely observed in outcrop. Thick accumulations of sand and gravel in the study area indicate that glacial meltwater deposition played a predominant role in shaping the landscape. The largest contribution from meltwater deposition was from the Saginaw Lobe and the least from the Huron-Erie Lobe indicated by the relative size of the channels and deposits.
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