Page 5 - 2008 NZ Subantarctic Islands
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New  Zealand,  the  Philippines,  Indonesia,  Malaysia,  and  much

                   smaller bits. They postulate that New Zealand was torn away from
                   Gondwanaland about 160 million years ago at a time when much

                   of  what  would  become  that  country  was  more  like  continental
                   shelf  than  a  large  island.  Over  the  millennia,  more  of  it  sank

                   beneath the ocean and became ocean bottom. Because of all the
                   pushing and pulling of  the Australian and  Pacific tectonic plates
                   and the subsequent earthquakes, synclines (deep trenches), and

                   volcanic  eruptions  beneath  the  sea,  the  many  islands  forming
                   New Zealand today were forced upwards until they reached sea

                   level and above. Isn’t that rather akin to how Maui hooked the
                   sea bottom and pulled it up above the waves?


                   A further detail in the Maori story concerns the damage that the

                   two elder brothers wreaked on Maui’s “big fish” by trying to hack
                   bits off and gouge deep to obtain the meat. That’s their story to
                   explain the mountains and fjords and plains that form the islands.

                   Geologists  say  these  features  are  the  creation  of  the  volcanic
                   action caused by the constant pressure of the two tectonic plates,

                   the  Australian  plate  moving  southwest  and  the  Pacific  plate
                   moving northerly. The fissures and earthquakes cause mountains

                   to  continue  rising  and  lakes  to  form  in  depressions  and  the
                   coastline  to  change  continuously  over  geologic  time.  Geologists

                   say  that  the  city  of  Christchurch  on  the  eastern  coast  of  New
                   Zealand’s  South  island  is  moving  in  a  different  direction  from
                   Wellington  on  the  southern  tip  of  the  North  Island  by  about  4

                   millimeters a year!  That’s rather quickly in geologic time!   The
                   geologists postulate that this strange journey occurs because the

                   North Island rides the Australian plate and half the South Island
                   sits  on  the  Pacific  plate.  1000  years  ago  when  the  Maoris

                   discovered  Aotearoa,  they  postulated  that  the  island  was  a  gift
                   from the ocean!  Modern plate tectonic theory does not disagree.


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