Coral reefs of the Loyalty islands
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ID: 308786
1952
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Abstract
The Loyalty islands northeast of New Caledonia, and the nearby Astrolabe reefs (considered incipient atolls), appear to be developed on an uplifted and tilted fault block of the sea floor. Of the three main islands, one is a coral atoll; the others were formed by growth of fringing reefs around a central core of serpentine rock which is exposed on Mare island.
| Reference Key |
openalex_W2132131119
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|---|---|
| Authors | F. R. Haeberle |
| Journal | american journal of science |
| Year | 1952 |
| DOI |
10.2475/ajs.250.9.656
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| URL | |
| Keywords | Keywords not found |
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