Item talk:Q47216: Difference between revisions

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orcid:
ORCiD:
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   meta:
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     status_code: 200
Line 1,207: Line 1,207:
         source: null
         source: null
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usgs_staff_profile:
USGS Staff Profile:
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    url: https://www.usgs.gov/staff-profiles/kevin-kincare
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    timestamp: '2024-01-30T15:59:44.601858'
   affiliation: []
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  description:
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    name: Kevin Kincare, Ph.D.
     abstract: Research Geologist with the Florence Bascom Geoscience Center
    name_qualifier: null
    additionalType: short description
     titles:
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    - Research Geologist
     abstract: I am currently mapping the glacial geology of the Manistee National
    organizations:
      Forest and Sleeping Bear Dunes National Lakeshore in northwest lower Michigan
    - !!python/tuple
      as well as ongoing work in the St. Joseph River basin of southwest Michigan
      - Florence Bascom Geoscience Center
      and northern Indiana. I am also working with the Great Lakes Geologic Mapping
      - https://www.usgs.gov/centers/florence-bascom-geoscience-center
      Coalition which includes all 8 states that have Great Lakes coastline.
    email: kkincare@usgs.gov
     additionalType: staff profile page introductory statement
    orcid: 0000-0002-1050-3627
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     intro_statements:
     abstract: 'My research goals are to: 1) develop local/regional Quaternary stratigraphic
    - I am currently mapping the glacial geology of the Manistee National Forest and
       frameworks in each map area, 2) improve our ability to predict the 3-D stratigraphy
      Sleeping Bear Dunes National Lakeshore in northwest lower Michigan as well as
      and distribution of material units (gravel, sand, silt-clay, till) in glacial
      ongoing work in the St. Joseph River basin of southwest Michigan and northern
      systems, 3) better assess how stratigraphic features affect flow of ground water
      Indiana. I am also working with the Great Lakes Geologic Mapping Coalition which
      through the system, and 4) assure that the most consistent geologic models are
      includes all 8 states that have Great Lakes coastline.
      used in collaborative studies.The existing literature does not deal with one
     expertise_terms:
      of the basic facts of drainage basins developed in glacial landscapes.  Where
    - erosion
      glaciers were unconstrained by bedrock uplands (e.g. much of the upper Midwest),
    - sedimentation
      drainage basins are often sequentially constructed from their distal to proximal
    - unconsolidated deposits
      areas rather than the classical evolution by headward erosion of streams and
    - stratigraphy
      springs over long periods of time.  Glacial retreat adds sections to the basin
    - glacial chronology
      in step-wise fashion as the glacier margin moves basinward.  The pattern, common
    professional_experience: []
      in the literature, of regional slope and stream-network development corresponding
    education: []
       to a pre-existing structural or stratigraphic pattern does not apply to these
    affiliations: []
      drainages.  Rivers draining today into the Lake Michigan basin were constructed
    honors: []
       in discrete parts during retreat of the Lake Michigan lobe and, in the case
    abstracts: []
      of the St. Joseph and Manistee Rivers, further imprinted by a buried Saginaw
     personal_statement: 'My research goals are to: 1) develop local/regional Quaternary
      lobe terrain as well as the addition of outwash from the proximal edge by the
       stratigraphic frameworks in each map area, 2) improve our ability to predict
      Huron/Erie lobe.  Each discrete part has a distinct depositional history that
      the 3-D stratigraphy and distribution of material units (gravel, sand, silt-clay,
       may not match that of the previously or subsequently added segments.  One of
      till) in glacial systems, 3) better assess how stratigraphic features affect
       the major outcomes of our research is that a realistic model of post-glacial
      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
       drainage basin development must reflect abrupt contrasts of sediment properties
       and slope gradients related to each successive ice-marginal position.'
       and slope gradients related to each successive ice-marginal position.'
    additionalType: personal statement
  email: kkincare@usgs.gov
  hasCredential: []
  hasOccupation:
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    affiliatedOrganization:
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      name: Florence Bascom Geoscience Center
      url: https://www.usgs.gov/centers/florence-bascom-geoscience-center
    roleName: Research Geologist
    startDate: '2024-05-12T16:14:51.421453'
  identifier:
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    propertyID: GeoKB
    value: https://geokb.wikibase.cloud/entity/Q47216
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    propertyID: ORCID
    value: 0000-0002-1050-3627
  jobTitle: Research Geologist
  knowsAbout:
  - '@type': Thing
    additionalType: self-claimed expertise
    name: erosion
  - '@type': Thing
    additionalType: self-claimed expertise
    name: sedimentation
  - '@type': Thing
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    name: unconsolidated deposits
  - '@type': Thing
    additionalType: self-claimed expertise
    name: stratigraphy
  - '@type': Thing
    additionalType: self-claimed expertise
    name: glacial chronology
  memberOf:
    '@type': OrganizationalRole
    member:
      '@type': Organization
      name: U.S. Geological Survey
    name: staff member
    startDate: '2024-05-12T16:14:51.418867'
  name: Kevin Kincare, Ph.D.
  url: https://www.usgs.gov/staff-profiles/kevin-kincare

Revision as of 19:06, 12 May 2024

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   abstract: Research Geologist with the Florence Bascom Geoscience Center
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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
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   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.'
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