Storm Deposits in Context of Seasonal through Decadal Water-Level Variances and Beach Geomorphic Change, Southwestern Lake Michigan.

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Title: Storm Deposits in Context of Seasonal through Decadal Water-Level Variances and Beach Geomorphic Change, Southwestern Lake Michigan.
Authors: Mattheus, C.R. (AUTHOR) mattheus@illinois.edu, Spitzer, E. (AUTHOR), Rosario, L. (AUTHOR), Pearce, K. (AUTHOR)
Source: Journal of Coastal Research. 2025, Vol. 41 Issue 6, p967-988. 22p.
Subjects: Shorelines, Lakes, Surveying (Engineering), Sediment transport, Sedimentary rocks, Coastal changes
Geographic Terms: Lake Michigan, Great Lakes (North America), Illinois, Michigan
Abstract: Mattheus, C.R.; Spitzer, E.; Rosario, L., and Pearce, K., 2025. Storm deposits in context of seasonal through decadal water-level variances and beach geomorphic change, southwestern Lake Michigan. Decadal changes in base water level, which are up to 2 m in magnitude, and storms capable of generating waves >3 m in height affect many beach shorelines of the North American Great Lakes. Still, few geomorphic studies have addressed coastal morphodynamics under such complex and ever-changing lake hydrodynamic conditions. With extensive topographic monitoring activities underway since 2018 along Illinois's portion of Lake Michigan coast, new avenues to systematically categorize and contextualize geomorphic change dynamics are available. This study offers a detailed assessment of beach topographic evolution along a historically progradational section of unobstructed shoreline along Illinois Beach State Park, located along the downdrift portion of a migrating ridge-plain promontory. Insights from pre- and poststorm topographic and colocational subsurface geophysical assessments are evaluated in context of seasonal through decadal patterns of geomorphic change. Study insights provide context for the effects of storms on beach-profile evolution over various lake-level positions, providing an architectural blueprint for subsurface depositional structures. This serves as a prerequisite for late Holocene paleo-reconstructions. lake-level rise-induced backshore accretion by way of shoreline-overwash processes occurred with minor changes to the shoreline position, with sand influx–facilitating profile aggradation in response to >1.5 m of lake-level rise between 2012 and 2020. Subsequent beach-profile adjustments, from 2020 to 2023, occurred only along the foreshore during rising and peak water levels, in response to ∼1 m fall in lake level. Pre- and poststorm subsurface reflection geophysical records, from the ∼3 m wave event in October 2023, resolve an ∼0.5 m thick storm deposit atop a ravinement surface, only a part of which is accounted for by topographic profile comparisons. Paleo-tempestite preservation potentials are reduced with post-2020 lowering of lake level by ∼1 m; nonetheless, the addition of ground-penetrating radar in monitoring provides a more thorough assessment of event-based geomorphic change. [ABSTRACT FROM AUTHOR]
Copyright of Journal of Coastal Research is the property of KnowledgeWorks Global, Ltd and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
Database: Engineering Source
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  Data: Storm Deposits in Context of Seasonal through Decadal Water-Level Variances and Beach Geomorphic Change, Southwestern Lake Michigan.
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  Data: <searchLink fieldCode="AR" term="%22Mattheus%2C+C%2ER%2E%22">Mattheus, C.R.</searchLink> (AUTHOR)<i> mattheus@illinois.edu</i><br /><searchLink fieldCode="AR" term="%22Spitzer%2C+E%2E%22">Spitzer, E.</searchLink> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Rosario%2C+L%2E%22">Rosario, L.</searchLink> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Pearce%2C+K%2E%22">Pearce, K.</searchLink> (AUTHOR)
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  Data: <searchLink fieldCode="JN" term="%22Journal+of+Coastal+Research%22">Journal of Coastal Research</searchLink>. 2025, Vol. 41 Issue 6, p967-988. 22p.
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  Data: <searchLink fieldCode="DE" term="%22Shorelines%22">Shorelines</searchLink><br /><searchLink fieldCode="DE" term="%22Lakes%22">Lakes</searchLink><br /><searchLink fieldCode="DE" term="%22Surveying+%28Engineering%29%22">Surveying (Engineering)</searchLink><br /><searchLink fieldCode="DE" term="%22Sediment+transport%22">Sediment transport</searchLink><br /><searchLink fieldCode="DE" term="%22Sedimentary+rocks%22">Sedimentary rocks</searchLink><br /><searchLink fieldCode="DE" term="%22Coastal+changes%22">Coastal changes</searchLink>
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  Data: <searchLink fieldCode="DE" term="%22Lake+Michigan%22">Lake Michigan</searchLink><br /><searchLink fieldCode="DE" term="%22Great+Lakes+%28North+America%29%22">Great Lakes (North America)</searchLink><br /><searchLink fieldCode="DE" term="%22Illinois%22">Illinois</searchLink><br /><searchLink fieldCode="DE" term="%22Michigan%22">Michigan</searchLink>
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: Mattheus, C.R.; Spitzer, E.; Rosario, L., and Pearce, K., 2025. Storm deposits in context of seasonal through decadal water-level variances and beach geomorphic change, southwestern Lake Michigan. Decadal changes in base water level, which are up to 2 m in magnitude, and storms capable of generating waves >3 m in height affect many beach shorelines of the North American Great Lakes. Still, few geomorphic studies have addressed coastal morphodynamics under such complex and ever-changing lake hydrodynamic conditions. With extensive topographic monitoring activities underway since 2018 along Illinois's portion of Lake Michigan coast, new avenues to systematically categorize and contextualize geomorphic change dynamics are available. This study offers a detailed assessment of beach topographic evolution along a historically progradational section of unobstructed shoreline along Illinois Beach State Park, located along the downdrift portion of a migrating ridge-plain promontory. Insights from pre- and poststorm topographic and colocational subsurface geophysical assessments are evaluated in context of seasonal through decadal patterns of geomorphic change. Study insights provide context for the effects of storms on beach-profile evolution over various lake-level positions, providing an architectural blueprint for subsurface depositional structures. This serves as a prerequisite for late Holocene paleo-reconstructions. lake-level rise-induced backshore accretion by way of shoreline-overwash processes occurred with minor changes to the shoreline position, with sand influx–facilitating profile aggradation in response to >1.5 m of lake-level rise between 2012 and 2020. Subsequent beach-profile adjustments, from 2020 to 2023, occurred only along the foreshore during rising and peak water levels, in response to ∼1 m fall in lake level. Pre- and poststorm subsurface reflection geophysical records, from the ∼3 m wave event in October 2023, resolve an ∼0.5 m thick storm deposit atop a ravinement surface, only a part of which is accounted for by topographic profile comparisons. Paleo-tempestite preservation potentials are reduced with post-2020 lowering of lake level by ∼1 m; nonetheless, the addition of ground-penetrating radar in monitoring provides a more thorough assessment of event-based geomorphic change. [ABSTRACT FROM AUTHOR]
– Name: AbstractSuppliedCopyright
  Label:
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  Data: <i>Copyright of Journal of Coastal Research is the property of KnowledgeWorks Global, Ltd and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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RecordInfo BibRecord:
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      – Type: doi
        Value: 10.2112/JCOASTRES-D-25-00013.1
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      – Code: eng
        Text: English
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      Pagination:
        PageCount: 22
        StartPage: 967
    Subjects:
      – SubjectFull: Shorelines
        Type: general
      – SubjectFull: Lakes
        Type: general
      – SubjectFull: Surveying (Engineering)
        Type: general
      – SubjectFull: Sediment transport
        Type: general
      – SubjectFull: Sedimentary rocks
        Type: general
      – SubjectFull: Coastal changes
        Type: general
      – SubjectFull: Lake Michigan
        Type: general
      – SubjectFull: Great Lakes (North America)
        Type: general
      – SubjectFull: Illinois
        Type: general
      – SubjectFull: Michigan
        Type: general
    Titles:
      – TitleFull: Storm Deposits in Context of Seasonal through Decadal Water-Level Variances and Beach Geomorphic Change, Southwestern Lake Michigan.
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            NameFull: Spitzer, E.
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            NameFull: Rosario, L.
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            – D: 01
              M: 11
              Text: 2025
              Type: published
              Y: 2025
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