Item talk:Q47216: Difference between revisions
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status_code: 200 | status_code: 200 | ||
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visibility: public | visibility: public | ||
USGS Staff Profile: | |||
'@context': https://schema.org | |||
'@type': Person | |||
affiliation: [] | |||
description: | |||
- '@type': TextObject | |||
abstract: Research Geologist with the Florence Bascom Geoscience Center | |||
additionalType: short description | |||
- '@type': TextObject | |||
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 | 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: | |||
- '@type': OrganizationalRole | |||
affiliatedOrganization: | |||
'@type': Organization | |||
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: | |||
- '@type': PropertyValue | |||
propertyID: GeoKB | |||
value: https://geokb.wikibase.cloud/entity/Q47216 | |||
- '@type': PropertyValue | |||
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 | |||
additionalType: self-claimed expertise | |||
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
ORCiD:
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USGS Staff Profile:
'@context': https://schema.org '@type': Person affiliation: [] description: - '@type': TextObject abstract: Research Geologist with the Florence Bascom Geoscience Center additionalType: short description - '@type': TextObject 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 hasCredential: [] hasOccupation: - '@type': OrganizationalRole affiliatedOrganization: '@type': Organization 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: - '@type': PropertyValue propertyID: GeoKB value: https://geokb.wikibase.cloud/entity/Q47216 - '@type': PropertyValue 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 additionalType: self-claimed expertise 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