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Cross-references
Bassett Edges
Beach Rock
Conglomerates
Coral Cay Classification and Evolution
Mangroves
Moats
Shingle Ridges
LYELL, CHARLES (1797–1875)
James Bowen
Southern Cross University, Lismore, NSW, Australia
Born in Edinburgh, Lyell became the dominant geologist
of the early nineteenth century with his great three-volume
Principles of Geology, published during the years
1830–1833. To explain the puzzle of atoll formation, he
argued that the circular or oval forms of the numerous
coral isles of the Pacific, with lagoons in their center,
“naturally suggest the idea that they are nothing more than
the crests of submarine volcanos, having the rims and bottoms of their craters overgrown by corals” built by an infinitely slow process on the summits of submerged
volcanoes on the ocean floor by “branched madrepores.”
In the case of archipelagos and similar distributions, Lyell
believed they had been formed from the ejection of volcanic ashes and sand which served as the foundations for yet
further reefs.
He also sought to explain the other great question
puzzling explorers: why “there should be so immense an
area in eastern Oceania, studded with minute islands,
without one single spot where there is a wider extent of
land than belongs to such islands as Tahiti, Hawaii, and
a few others, which either have been, or are still the seats
of active volcanoes?” The answer he provided was that
LYELL, CHARLES (1797–1875)
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