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The utility of ShoreZone maps for change detection was assessed by independent reviewers in 2009 and 2011, and findings include: 1) the NOAA Coast63 digital shoreline used by ShoreZone in Alaska poorly resolves features less than 50 meters, i.e., many small scale features are not represented and thus cannot be accurately described; 2) ShoreZone ...
The littoral zone, also called litoral or nearshore, is the part of a sea, lake, or river that is close to the shore. [1] In coastal ecology, the littoral zone includes the intertidal zone extending from the high water mark (which is rarely inundated), to coastal areas that are permanently submerged — known as the foreshore — and the terms are often used interchangeably.
Looe Key is a coral reef located within the Florida Keys National Marine Sanctuary. It lies to the south of Big Pine Key. This reef is within a Sanctuary Preservation Area (SPA). Part of Looe Key is designated as "Research Only," an area which protects some of the patch reefs landward of the main reef.
Semi-transparent orthographic projection, centered on 40° N, 40° W, using shoreline data from GSHHG ("crude level") GSHHG (Global Self-consistent, Hierarchical, High-resolution Geography Database; formerly Global Self-consistent, Hierarchical, High-resolution Shoreline Database (GSHHS)) is a high-resolution shoreline data set amalgamated from two data bases (the CIA world database WDBII, and ...
The Ballantine scale is a biologically defined scale for measuring the degree of exposure level of wave action on a rocky shore. Devised in 1961 by W. J. Ballantine, then at the zoology department of Queen Mary University of London, London, U.K., the scale is based on the observation that where shoreline species are concerned "Different species growing on rocky shores require different degrees ...
Isostatic change could be due to post-glacial adjustment. [2] Another common cause of isostatic change that can result in a submergent coastline is tectonic action. [2] Events such as earthquakes or volcanic eruptions may cause land subsidence therefore causing isostatic sea level increases. [2] Eustatic sea level rise can also be caused by ...
Somalia has the longest coastline in Africa. [11]The Earth has approximately 620,000 kilometres (390,000 mi) of coastline. Coastal habitats, which extend to the margins of the continental shelves, make up about 7 percent of the Earth's oceans, [12] but at least 85% of commercially harvested fish depend on coastal environments during at least part of their life cycle. [13]
Longshore drift from longshore current is a geological process that consists of the transportation of sediments (clay, silt, pebbles, sand, shingle, shells) along a coast parallel to the shoreline, which is dependent on the angle of incoming wave direction. Oblique incoming wind squeezes water along the coast, generating a water current that ...