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Lake Michigan Bluff Recession

Bibliographic Data

ID8375766
AuthorsWilliam R Buckler (Bowling Green State University), Harold A Winters (United States Military Academy)
Year1983
Volume73
Issue1
Pages89-110
Publication date1983-03-01
Peer ReviewedYes
Open AccessNo
TypeARTICLE
VenueAnnals of the Association of American Geographers (JOURNAL)
Journal identifiersISSN: 0004-5608 • E-ISSN: 1467-8306
PublisherInforma UK Limited (PUBLISHER • GB)
DOI10.1111/j.1467-8306.1983.tb01398.x
OpenAlexW2134607511
LanguageEN
Citations received3
References cited8

Long-term recession rates of Lake Michigan's shorezone bluffs were investigated at 118 sites by comparing modern measurements with nineteenth-century Government Land Office surveys. These rates were evaluated spatially and related to selected shorezone characteristics. One hundred and six of the bluff sites are experiencing retreat that averages 0.4 m (1.3 ft) per year. Although amounts vary significantly, average values show that (1) rates are similar for opposite sides of the lake but (2) values differ between northern and southern Wisconsin. In addition, dune-encompassed bluffs tend to recede at lower long-term rates than nondune bluffs. Groundwater seepage, shoreline orientation and fetch, and shorezone protective structures are some of the factors found to influence bluff crest recession. Data from this study indicate that extensive Lake Michigan shorezone tracts will continue to experience bluff recession measurable in meters per decade unless lake levels are relatively low or unless protective devices of massive proportion are constructed along much of the shoreline

Archaeology · Bluff · Fetch · Geography · Geotechnical engineering · Hydrology (agriculture) · Physical geography · Recession · Shore · Aeolian processes and effects · Geology · Hydrology and Sediment Transport Processes · Oceanography · Soil erosion and sediment transport

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Unique citing works3
Citations per year0,07
Citation span1985 - 2024 (40)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 2

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