Item talk:Q47216
From geokb
ORCID:
'@context': http://schema.org '@id': https://orcid.org/0000-0002-1050-3627 '@reverse': creator: - '@id': https://doi.org/10.3133/ofr20211120 '@type': CreativeWork identifier: '@type': PropertyValue propertyID: doi value: 10.3133/ofr20211120 name: "Implementation plan of the National Cooperative Geologic Mapping Program\ \ strategy\u2014Great Lakes (Central Lowland and Superior Upland Physiographic\ \ Provinces)" - '@id': https://doi.org/10.3133/sim3383 '@type': CreativeWork identifier: '@type': PropertyValue propertyID: doi value: 10.3133/sim3383 name: Surficial geologic map of Berrien County, Michigan, and the adjacent offshore area of Lake Michigan - '@id': https://doi.org/10.1080/00045608.2015.1115388 '@type': CreativeWork identifier: '@type': PropertyValue propertyID: doi value: 10.1080/00045608.2015.1115388 name: 'Loamy, Two-Storied Soils on the Outwash Plains of Southwestern Lower Michigan: Pedoturbation of Loess with the Underlying Sand' - '@id': https://doi.org/10.3133/ofr20061260f '@type': CreativeWork identifier: '@type': PropertyValue propertyID: doi value: 10.3133/ofr20061260f name: Surficial geologic map of the Norton-Manomet-Westport-Sconticut Neck 23-quadrangle area in southeast Massachusetts - '@type': CreativeWork name: Geologic evolution of the Great Lakes - '@id': https://doi.org/10.1007/s10933-006-9045-2 '@type': CreativeWork identifier: '@type': PropertyValue propertyID: doi value: 10.1007/s10933-006-9045-2 name: "Response of the St. Joseph River to lake level changes during the last\ \ 12,000\_years in the Lake Michigan basin" - '@id': https://doi.org/10.1111/1467-8306.00296 '@type': CreativeWork identifier: '@type': PropertyValue propertyID: doi value: 10.1111/1467-8306.00296 name: Measurement, Correlation, and Mapping of Glacial Lake Algonquin Shorelines in Northern Michigan - '@id': https://doi.org/10.4095/299510 '@type': CreativeWork identifier: '@type': PropertyValue propertyID: doi value: 10.4095/299510 name: 'Glacial geology mapping in Berrien County, Michigan: Resolving the third dimension for increasing the accuracy of resource assessment' - '@id': https://doi.org/10.3133/ofr99349 '@type': CreativeWork identifier: '@type': PropertyValue propertyID: doi value: 10.3133/ofr99349 name: 'Mapping the glacial geology of the Central Great Lakes region in three dimensions: A model for state-federal cooperation' - '@id': https://doi.org/10.1130/2016.2520(37) '@type': CreativeWork identifier: '@type': PropertyValue propertyID: doi value: 10.1130/2016.2520(37) name: A multiagency and multijurisdictional approach to mapping the glacial deposits of the Great Lakes region in three dimensions '@type': Person affiliation: - '@type': Organization alternateName: EGPSC identifier: '@type': PropertyValue propertyID: RINGGOLD value: '2928' name: US Geological Survey - '@type': Organization identifier: '@type': PropertyValue propertyID: RINGGOLD value: '273878' name: Michigan Geological Survey - '@id': grid.480518.0 '@type': Organization name: International Association of Sedimentologists - '@id': https://doi.org/10.13039/100005720 '@type': Organization name: Geological Society of America - '@type': Organization identifier: '@type': PropertyValue propertyID: RINGGOLD value: '503220' name: SEPM Society for Sedimentary Geology - '@type': Organization identifier: '@type': PropertyValue propertyID: RINGGOLD value: '62653' name: International Glaciological Society alumniOf: - '@type': Organization alternateName: Geology identifier: '@type': PropertyValue propertyID: RINGGOLD value: '4175' name: Western Michigan University - '@type': Organization alternateName: Geological Science identifier: '@type': PropertyValue propertyID: RINGGOLD value: '3078' name: Michigan State University familyName: Kincare givenName: Kevin mainEntityOfPage: https://orcid.org/0000-0002-1050-3627
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
