Item talk:Q47216

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     name: Surficial geologic map of Berrien County, Michigan, and the adjacent offshore
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     name: "Response of the St. Joseph River to lake level changes during the last\
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   name: Michigan State University
 familyName: Kincare
 givenName: Kevin
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 updated_date: '2024-05-16T08:04:51.539336'

USGS Staff Profile:

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   abstract: Research Geologist with the Florence Bascom Geoscience Center
   additionalType: short description
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   abstract: I am currently mapping the glacial geology of the Manistee National
     Forest and Sleeping Bear Dunes National Lakeshore in northwest lower Michigan
     as well as ongoing work in the St. Joseph River basin of southwest Michigan
     and northern Indiana. I am also working with the Great Lakes Geologic Mapping
     Coalition which includes all 8 states that have Great Lakes coastline.
   additionalType: staff profile page introductory statement
 - '@type': TextObject
   abstract: 'My research goals are to: 1) develop local/regional Quaternary stratigraphic
     frameworks in each map area, 2) improve our ability to predict the 3-D stratigraphy
     and distribution of material units (gravel, sand, silt-clay, till) in glacial
     systems, 3) better assess how stratigraphic features affect flow of ground water
     through the system, and 4) assure that the most consistent geologic models are
     used in collaborative studies.The existing literature does not deal with one
     of the basic facts of drainage basins developed in glacial landscapes.  Where
     glaciers were unconstrained by bedrock uplands (e.g. much of the upper Midwest),
     drainage basins are often sequentially constructed from their distal to proximal
     areas rather than the classical evolution by headward erosion of streams and
     springs over long periods of time.  Glacial retreat adds sections to the basin
     in step-wise fashion as the glacier margin moves basinward.  The pattern, common
     in the literature, of regional slope and stream-network development corresponding
     to a pre-existing structural or stratigraphic pattern does not apply to these
     drainages.  Rivers draining today into the Lake Michigan basin were constructed
     in discrete parts during retreat of the Lake Michigan lobe and, in the case
     of the St. Joseph and Manistee Rivers, further imprinted by a buried Saginaw
     lobe terrain as well as the addition of outwash from the proximal edge by the
     Huron/Erie lobe.  Each discrete part has a distinct depositional history that
     may not match that of the previously or subsequently added segments.   One of
     the major outcomes of our research is that a realistic model of post-glacial
     drainage basin development must reflect abrupt contrasts of sediment properties
     and slope gradients related to each successive ice-marginal position.'
   additionalType: personal statement
 email: kkincare@usgs.gov
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     name: Florence Bascom Geoscience Center
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   roleName: Research Geologist
   startDate: '2024-05-12T16:14:51.421453'
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   additionalType: self-claimed expertise
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   additionalType: self-claimed expertise
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   additionalType: self-claimed expertise
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   name: glacial chronology
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   startDate: '2024-05-12T16:14:51.418867'
 name: Kevin Kincare, Ph.D.
 url: https://www.usgs.gov/staff-profiles/kevin-kincare