Page 94 - (DK) Ocean - The Definitive Visual Guide
P. 94

92      COASTS AND THE SEASHORE


               Coastal Landscapes



               A GREAT VARIETY OF LANDSCAPES ARE FOUND along the coastlines                                            FRINGING REEF
               of the world’s oceans. Coasts are shaped by processes such as sea-level                                 This reef-fringed
                                                                                                                       coast, around the
               change and wave erosion, as well as by land-based processes such                                        south Pacific island
                                                                                                                       of Bora Bora, is a
               as weathering, erosion and deposition by rivers, glacier advance                                        secondary coast, as
               and retreat, the flow of lava from volcanoes, and tectonic faulting.                                    it has been modified
                                                                                                                       by the activities of
               Some coastal features are made by living organisms, including                                           living organisms,
               the reefs built by corals and the harbors, coastal defenses, and                                        notably corals.
               artificial islands built by humans.


               Classification of Coasts

               Coasts can be classified as either primary or secondary. Primary coasts
               have formed as a result of land-based processes, such as the deposition
               of sediment from rivers (forming deltas), land erosion, volcanic action,
               or rifting and faulting in Earth’s crust. Coasts formed as a result of
               recent sea-level change, which include drowned coasts and emergent
               coasts (see pp.88–89), are also usually considered primary, as are
               coastlines consisting mainly of wind-deposited sand, glacial till, or
               the seaward ends of glaciers. Coasts are considered secondary if they
               have been heavily shaped by marine erosional
               or depositional processes, or by the activities of
               organisms, such as corals, mangroves, or, indeed,
               people. A few coasts—for example, emergent
               coasts that have undergone significant marine
               erosion—display both primary and secondary
               features and so fit into an intermediate category.                                              VOLCANIC COAST
                                                                                          ARTIFICIAL COAST     This land-eroded volcanic
                                                                                          Singapore Harbor, in Southeast   cone is in the Galápagos Islands.
                                                                                          Asia, is an example of a coast   The entire coastline around these
                                                                                          that has been heavily shaped    islands was formed by volcanic
                                                                                          by human activity. Before    activity and so is a primary coast.
                                                                                          human intervention, it was
                                                                                          a mangrove-lined estuary.





















        OCEAN ENVIRONMENTS  SEA ARCH













                 This spectacular arch in southern England
                 is known as Durdle Door. A remnant of
                 a once much larger headland, it is a
                 classic feature of a marine-eroded coast.
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