Dynamics of beach-ridge formation along a migrating strandplain with implications for paleo-environmental assessment, Illinois Beach State Park, southwestern Lake Michigan

被引:8
作者
Mattheus, Christopher R. [1 ]
Braun, Katherine N. [1 ,2 ]
Theuerkauf, Ethan J. [3 ]
机构
[1] Univ Illinois, Prairie Res Inst, Illinois State Geol Survey, 701 North Point Dr, Winthrop Harbor, IL 60096 USA
[2] Univ Wisconsin, Dept Geog, 550 N Pk St, Madison, WI 53706 USA
[3] Michigan State Univ, Dept Geog, 673 Auditorium Rd,Rm 122, E Lansing, MI 48824 USA
关键词
Ridge-and-swale topography; Strand migration; Littoral transport; Radiocarbon; GIS; Lake level; GREAT-LAKES; PLAIN EVIDENCE; INDIANA COAST; BARRIER-SPIT; LEVEL; ICE; COMPLEX; ERIE; VARIABILITY; SHORELINE;
D O I
10.1016/j.jglr.2022.10.004
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This paper provides insights into shoreline morphodynamics and ridge-plain physiographic compart-mentalization along the migrating Zion Beach-ridge Plain, a mainland-attached strand along the high-energy, wave-dominated SW coast of Lake Michigan. Results of UAS-based topographic monitoring dur-ing the recent decadal lake-level high (2018-2020) captured the earliest phase of the ridge-formation process along several beach sites. This process-based study of net-erosional (i.e., littoral updrift) and net-accretionary (i.e., littoral downdrift) parts of the system offers much-needed context for assessing relict strand architectures. Embayed beach-ridge plains of the Laurentian Great Lakes have long served as paleo-environmental archives. They form from water-level changes and can be used to interpret iso-stacy. The preservation of beach ridges here is facilitated by unidirectional infilling. Much less is known about how nearshore littoral processes impact unconfined strand systems and whether useful paleoen-vironmental information absent within embayed system analogs might be elucidated from their complex architecture. We herewith promote a model of punctuated development. Major episodes of shoreline transgression are manifested as continuous ridgelines of topographic prominence that, along the north-ern, erosive strand, truncate older ridges and are onlapped by younger ones. These major discontinuities reflect environmental changes greater in magnitude than decadal water-level oscillations observed to have formed ridgelines in recent decades. The temporal offset across the most lakeward of these major erosional strandlines is on the order of 1 kyrs and it formed between 1.8 ka and 0.9 ka, based on available C-14 ages, coincidental with a regional shift in dominant storm-wind pattern to one promoting higher -energy littoral dynamics.& COPY; 2022 International Association for Great Lakes Research. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:147 / 162
页数:16
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