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Updated: June 24, 2025


Her tall masts, still standing bolt upright amid the coral-reefs, presented a gaunt spectacle, plainly visible from the Hero's decks as she threaded her way among the shoaly waters, while a similar though less tragical warning was the disaster that had overtaken two other vessels, the Astrolabe and the Zélée, which by a sudden ebb of the tide were thrown high and dry upon the sands, and remained in this frightful condition for eight days before the returning waters drifted them off.

The plains immediately bordering the Red Sea seem chiefly to consist of a sedimentary formation of the newer tertiary period. The shore is, with the exception of a few parts, fringed by coral-reefs.

The united lengths of these volcanic belts is about ninety degrees, or one-fourth of the entire circumference of the globe. Their width is about fifty miles; but, for a space of two hundred miles on each side of them, evidences of subterranean action are to be found in recently elevated coral-rock, or in barrier coral-reefs, indicating recent submergence.

The number of the species of Holothuria, and of the individuals which swarm on every part of these coral-reefs, is extraordinarily great; and many shiploads are annually freighted, as is well-known, for China with the trepang, which is a species of this genus.

The principal towns are Pitan, Kinarubatan, Kulepan, and the famous town of Sugut. The coast is so full of coral-reefs, and has been so very indifferently surveyed, that it is only frequented by prows; there is a road from Sugut to Bankaka in Maludu Bay. Much wax, tripan, sago, &c., is produced here.

In these cases, it would appear as if the volcanoes had come into action, and had become extinguished on the same spots, according as the elevating or subsiding movements prevailed. There are some other coasts on the map, where volcanoes in a state of action concur with proofs of recent elevation, besides those coloured red from being fringed by coral-reefs.

During my investigations on coral-reefs, I had occasion to consult the works of many voyagers, and I was invariably struck with the fact, that with rare exceptions, the innumerable islands scattered throughout the Pacific, Indian, and Atlantic Oceans, were composed either of volcanic, or of modern coral-rocks.

The captain said they imagined we had passed Aden in the dark, and thinking they should soon be among rocks or coral-reefs had stopped; a dreadful uproar then arose, and everyone on the ship shouted different directions for steering. My husband desired them to steer north that we might find land, as none of them had any idea of our longitude.

There was one place that I wished, particularly, to visit before I left, and that was what the people in Nassau called the Coral-reef. There were lots of coral-reefs all about the islands, but this one was easily visited, and for this reason, I suppose, was chosen as a representative of its class.

If during the prolonged subsidence of a shore, coral-reefs grew for the first time on it, or if an old barrier-reef were destroyed and submerged, and new reefs became attached to the land, these would necessarily at first belong to the fringing class, and, therefore, be coloured red, although the coast was sinking: but I have no reason to believe, that from this source of error, any coast has been coloured wrongly with respect to movement indicated.

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