Page 101 - (DK) Ocean - The Definitive Visual Guide
P. 101

COASTAL LANDSCAPES             99


                INDIAN OCEAN NORTHWEST                                      INDIAN OCEAN NORTHEAST    were later thrust upwards and tipped
                                            SATELLITE VIEW                                            over at an angle when India began to
             Tigris Euphrates               The delta’s seaward edge has    Krabi Coast               collide with mainland Asia some 50
                                            advanced by about 250km (150 miles)                       million years ago. Around Krabi and
             Delta                          in the past 3,000 years.                   TYPE  Primary coast  Phang Nga Bay to its north, chemical
                                                                                       FORMATION  Chemical   erosion of these limestone strata by
                           TYPE  Primary coast
                                                                                       erosion of limestone   rainwater, followed by sea-level rise,
                           FORMATION  Sediment                                         followed by drowning  has created thousands of craggy karst
                           deposition from Tigris,                                     EXTENT  160km
                           Euphrates, and Karun                                                       hills and islands. These include a
                                                                                       (100 miles)    number of isolated cone- and
                           EXTENT  150 km                               LOCATION  Andaman Sea coast of southwestern
                           (95 miles)                                                                 cylinder-shaped karst towers that rise
                                                                        Thailand                      out of the sea to heights of up to
             LOCATION  Parts of southeastern Iraq, northeastern
             Kuwait, and southwestern Iran                                                            210m (700ft) and groups of towers
                                                                        The area around Krabi on the western   that sit on broad masses of limestone.
             The Tigris Euphrates delta is a broad                      coast of southern Thailand is notable   Many of these karst formations are
             area of marshes and alluvial plain                         for its fantastic-looking formations of   elongated in a northeast-southwest
             at the northern head of the Arabian                        partially dissolved limestone, known    direction, reflecting the axis (or strike
             Gulf, formed from sediment deposited                       as karst. This limestone was originally   line) around which the original layers
             by three major rivers. An important                        formed about 260 million years ago.   of limestone were tipped.
             wildlife haven, the delta suffered great                   At that time, a shallow sea covered
             ecological damage between the 1970s                        what is now south Asia and slowly   KOH TAPU ISLAND
             and 2003 from various drainage and                         built up deposits of shells and coral   Some of the karst formations along this coast
             damming schemes carried out for                            that sediments washed in from the   have been weathered into unusual shapes,
             military and political purposes. Fisheries                 land subsequently buried. These   as in these examples at Koh Tapu Island in
             and several animal species became                          formed layers of limestone, which   Phang Nga Bay to the north of Krabi.
             threatened. Some recovery from the
             damage has occurred since 2003.


                INDIAN OCEAN SOUTHEAST     One of Australia’s best-known
                                           geological landmarks is a group of
             The Twelve Apostles           large sea stacks formed through the
                                           erosion of 20-million-year-old
                            TYPE  Secondary coast  limestone cliffs. Known as the Twelve
                            FORMATION  Wave   Apostles, even though there were
                            erosion of cliffs   originally only nine of them, the
                            producing large sea
                            stacks         stacks are up to 70m (230ft) tall.
                                           In 2005, one of the stacks collapsed,
                            EXTENT  3km (2 miles)
                                           leaving just eight. Collapses such as
             LOCATION  Near Port Campbell, southwest of   this are quite common and are an
             Melbourne, Victoria, southeastern Australia
                                           integral part of the erosion process.




                ONGOING EROSION
                The effects of wave erosion can
                clearly be seen at the bases of
                the remaining Apostles.




             VICTORIA HARBOUR                 PACIFIC OCEAN WEST        A number of natural harbours   from a satellite island, Ap Lei Chau.
             This view shows Victoria Harbour                           surround Hong Kong Island, which is   The margins of all these harbour areas
             with Hong Kong Island on the left    Hong Kong Harbour     the best-known part of the Hong   have been artificially modified by the
             and Kowloon on the right. Visited by                       Kong region of China. The largest,   construction of concrete piers,
             more than 200,000 ships per year, the       TYPE  Secondary coast  naturally deepest, and most sheltered   seawalls, jetties, and other structures.
             harbour is one of the world’s busiest.      FORMATION  Artificial   of these harbours is Victoria Harbour,   This coastline can be classified as
                                                         coast built around   which has an area of over 42 square   a secondary coast because it has been
                                                         various natural harbours   km (16 square miles) and is situated   modified by living organisms, in this
                                                         and nearby islands
                                                                        between Hong Kong Island and   case, humans. In the whole of the
                                                         EXTENT  40km (25 miles)  Kowloon Peninsula. Other smaller   Hong Kong region, more than 100km
                                           LOCATION  Southeast of Guangzhou, on the South   harbours include Aberdeen Harbour,   (60 miles) of coastline have been
                                           China Sea coast of southeastern China  which separates Hong Kong Island   artificially constructed or modified.  OCEAN ENVIRONMENTS
   96   97   98   99   100   101   102   103   104   105   106