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Most
of the offshore islands in Samoa are remnants of old volcano craters
of which some of them rises 200 m above sea level. Nu'usafee
island off the south coast has a different geology. It's believed to
have formed as a result of ground water seeping out through a
submerged freshwater spring. The calcium carbonate rich coral sand
has formed into rock after reacting with the fresh water. The island
is only a couple of meters above sea level at its highest point. The
offshore islands at Aleipata, Nu'utele, Namua, Fanuatapu and Nu'ulua
are old volcano craters.
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