Sandy shores show up as beaches in enclosed bays between rocky headlands or as long stretches of sand nearby to seaside dune units or sandy spits. Sandy shores are extremely dynamic environments, have a characteristic biodiversity and reexisting a distinct gradient of habitats. The environment is attrenergetic for housing, accommodays essential marine facilities and gives great opportunities for fisheries, recreation and drinking water sources, for this reason represents high economic worth. Natural breakthrough of sandy shores counts on the accumulation of sand that is transported to the shore from inland resources by rivers, and / or from marine sources by waves, currental fees and wind. The morphology of a sandy shore supports the habitats and eco-friendly processes in this setting. On the long term, sandy shore development is governed by the balance between the net supply of sediments and the demand also, created by sea level increase and also subsidence.
ReferencesLiteratureKomar, P. 1983. CRC handbook of seaside processes and also erosion. CRC.MacHarg, I, 1969. Deauthorize With Nature.Mulder, J.P.M, J.A. van Dalfsen, 2011. Current obstacles in seaside monitoring in the Netherlands; examples of pilot tasks. Coastal Engineering Practice 2011, ASCE 2011.Reading, H.G., 1996. Sedimentary environments: processes, facies, and also stratigraphy. John Wiley & Sons.Widdows, J., M. Brinsley, 2002.
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Impact of biotic and also abiotic procedures on sediment dynamics and the after-effects to the structure and functioning of the intertidal zone. Journal of Sea Research 48: pp 143 – 156.Net