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If you face it square, it is possible to see nothing but water, a coarse beach and dunes towering 40 and 50 feet in the background.
An increase of mean water level by 0.1 m will increase the area available to benthic invertebrates by 13 m, and with a 30-m wide coarse beach zone the usable area would change by 44% (Figure 4C).
Three taxa were used for assessing water level change in coarse beach habitat: benthic invertebrates (e.g., insects, mollusks, and crustaceans), rock bass (Ambloplites rupestris, shallow rocky habitat fish), and killdeer (Charadrius vociferous, shore zone bird).
Average water level in Lake Ontario from May through October was 74.94±0.1 m with a coarse beach slope of approximated 0.0075 (half the slope of sandy beach [29]).
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The killdeer is a shoreline bird that forages and nests on coarse beaches.
Fish that inhabit the littoral zone of coarse beaches forage among the interstitial spaces of the substrate to find invertebrates.
Shallow and turbulent waters with coarse material provide habitat for a variety of invertebrates and fish [38], [39], and the exposed coarse beaches support some birds.
Coarse beaches are composed of rocky material, typically with particle sizes of gravel to cobble, that are resistant to wave action and do not move readily with water level changes (Figure 1).
Thirty years ago the place was empty: a long coarse sand beach protecting a placid lagoon and surrounded by wooded mountains.
Instead, a complex balance of processes is responsible for the profile evolution of coarse-grained beaches with no single dominant process.
Wave exposure, geological background and coastal configuration were found to be important components in coarse-clastic pocket beach response to forcings.
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CEO of Professional Science Editing for Scientists @ prosciediting.com