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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Cape Verde Islands (1)
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Southern Africa
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South Africa
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Eastern Cape Province South Africa (1)
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KwaZulu-Natal South Africa
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Durban South Africa (1)
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Atlantic Ocean Islands
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Canary Islands (1)
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Cape Verde Islands (1)
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Indian Ocean (1)
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elements, isotopes
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carbon
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C-14 (1)
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isotopes
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radioactive isotopes
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C-14 (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene (1)
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Pleistocene
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upper Pleistocene (1)
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Paleozoic
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Carboniferous (1)
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Primary terms
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absolute age (1)
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Africa
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Cape Verde Islands (1)
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Southern Africa
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South Africa
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Eastern Cape Province South Africa (1)
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KwaZulu-Natal South Africa
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Durban South Africa (1)
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Atlantic Ocean Islands
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Canary Islands (1)
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Cape Verde Islands (1)
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carbon
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C-14 (1)
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Cenozoic
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Quaternary
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Holocene (1)
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Pleistocene
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upper Pleistocene (1)
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continental shelf (1)
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geophysical methods (1)
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Indian Ocean (1)
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isotopes
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radioactive isotopes
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C-14 (1)
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ocean circulation (1)
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Paleozoic
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Carboniferous (1)
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sea-level changes (3)
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sedimentary rocks
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carbonate rocks
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limestone
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microbialite (1)
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clastic rocks (2)
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sedimentary structures
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planar bedding structures
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bedding (1)
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laminations (1)
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sediments
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carbonate sediments (1)
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clastic sediments
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boulders (1)
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marine sediments (1)
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shorelines (2)
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rock formations
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Karoo Supergroup (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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limestone
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microbialite (1)
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clastic rocks (2)
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sedimentary structures
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sedimentary structures
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planar bedding structures
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bedding (1)
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laminations (1)
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sediments
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sediments
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carbonate sediments (1)
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clastic sediments
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boulders (1)
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marine sediments (1)
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Microbialites of modern siliciclastic rock coasts
Island-Encapsulating Eolian Sedimentary Systems of the Canary and Cape Verde Archipelagos
Longshore Size Grading On A Boulder Beach
Submerged shoreline preservation and ravinement during rapid postglacial sea-level rise and subsequent “slowstand”
Storm Swash Deposition On An Embayed Rock Coastline: Facies, Formative Mechanisms, and Preservation
The enormous and growing scale of human intervention in coastal processes is driven by a short-sighted societal desire to protect property in the face of shoreline recession. Underpinning this effort in both the design of engineering interventions and the amelioration of their impacts is the application of numerical models that purport to simulate and predict coastal processes. Coasts are complex systems in which (1) waves, currents, tides, and wind operate on a (2) finite or changing volume of sediment of specific character (3) within a particular geological context. Feedbacks exist within and between these three domains, and all are temporally and spatially variable. The simplifications and assumptions involved in reducing this complexity to equations and numerical models cause a deviation from reality such that models are unable to provide realistic predictions of coastal behavior. Nonetheless (and despite criticism from geologists), models have become entrenched in coastal engineering practice and are now a standard weapon in society's assault on the world's coasts. In this paper, we chart the development of several widely used models, highlight their shortcomings, and speculate on why they remain in use. The disconnect between reality and the mathematics of coastal process models is extreme, and a fundamental reassessment is required.