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Coastal geomorphology of Beqa and Yanuca Islands, South Pacific Ocean, and its significance for the tectonic history of the Vatulele- Beqa Ridge
Journal article   Peer reviewed

Coastal geomorphology of Beqa and Yanuca Islands, South Pacific Ocean, and its significance for the tectonic history of the Vatulele- Beqa Ridge

Patrick Nunn
Pacific Science, Vol.44(4), pp.348-365
1990
url
http://scholarspace.manoa.hawaii.edu/bitstream/handle/10125/1288/v44n4-348-365.pdf?sequeView
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Abstract

Data referring to elevations of emerged shoreline indicators along the coasts of Beqa and Yanuca islands in southern Fiji were collected and indicate the presence of former mean sea levels at elevations (and shoreline names) of 0.96 m (MUA1), 1.93 m(BUL1), 2.63 m (MUA2), 4.32 m (MUA3), 5.94 (MUA4), and 7.79 m (MUA5) above present mean sea level. Age is believed to increase with increasing elevation. Investigations of the Beqa lagoon floor and comparison of shoreline levels between eastern Beqa, western Beqa, Yanuca, and Vatulele island (at the western end of the Vatulele-Beqa Ridge) suggest that downfaulting along faults and grabens trending a little west of north has occurred both during and since the time of shoreline emergence. -from Author

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