Geology 1020: Sigatoka River Valley by Michael Rayasi

How it was formed...

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fiji.jpg

A map dividing Fiji's plate boundaries. As you can see on the map, where the Sigatoka River Valley is located, the boundary has shifted slightly to the right.
University of Texas Library. Online Maps of Current Interest.2008.
 

How it was formed...

 

Around 8 million years ago the Pacific crust was subducted from the ‘Rim of Fire’ plate boundary, creating Fiji. Due to subduction along the Vityaz arc­ trench system, there was a blockage because of a thick oceanic crust. This then reversed subduction on Vitu Levu(Fiji's largest island, which contains the Sigatoka River Valley)[1]. Because of this subduction, the Sigatoka River Valley was formed and this river valley is constantly expanding.



[1] Director of Mineral Resources.Fiji's Geology: Regional Setting.Ministry of Lands

      and Mineral Resources.Internet.

      http://www.mrd.gov.fj/gfiji/geology/educate/geo_fiji.html 

     (accessed November 2007)

aboutus2.jpg

A picture of the Sigatoka River Valley where it narrows.

Sigatoka River Safari Ltd. 2007.

http://www.sigatokariver.com/gallery.php 

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A village located in the Sigatoka River Valley area known as the ‘Salad Bowl’ which is one of Fiji’s largest croplands.

Sigatoka River Safari Ltd. 2007.

http://www.sigatokariver.com/gallery.php