The Voyage Of The Beagle By Charles Darwin





































































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[5] Kotzebue's First Voyage, vol. iii. p. 222.

[6] The large claws or pincers of some of these crabs are - Page 383
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[5] Kotzebue's First Voyage, Vol.

Iii.

P. 222.

[6] The large claws or pincers of some of these crabs are most beautifully adapted, when drawn back, to form an operculum to the shell, nearly as perfect as the proper one originally belonging to the molluscous animal. I was assured, and as far as my observations went I found it so, that certain species of the hermit-crab always use certain species of shells.

[7] Some natives carried by Kotzebue to Kamtschatka collected stones to take back to their country.

[8] See Proceedings of Zoological Society, 1832, p. 17.

[9] Tyerman and Bennett. Voyage, etc. vol. ii. p. 33.

[10] I exclude, of course, some soil which has been imported here in vessels from Malacca and Java, and likewise, some small fragments of pumice, drifted here by the waves. The one block of greenstone, moreover, on the northern island must be excepted.

[11] These were first read before the Geological Society in May, 1837, and have since been developed in a separate volume on the "Structure and Distribution of Coral Reefs."

[12] It is remarkable that Mr. Lyell, even in the first edition of his "Principles of Geology," inferred that the amount of subsidence in the Pacific must have exceeded that of elevation, from the area of land being very small relatively to the agents there tending to form it, namely, the growth of coral and volcanic action.

[13] It has been highly satisfactory to me to find the following passage in a pamphlet by Mr. Couthouy, one of the naturalists in the great Antarctic Expedition of the United States: - "Having personally examined a large number of coral-islands and resided eight months among the volcanic class having shore and partially encircling reefs. I may be permitted to state that my own observations have impressed a conviction of the correctness of the theory of Mr. Darwin." - The naturalists, however, of this expedition differ with me on some points respecting coral formations.

CHAPTER XXI

MAURITIUS TO ENGLAND

Mauritius, beautiful appearance of - Great crateriform ring of Mountains - Hindoos - St. Helena - History of the changes in the Vegetation - Cause of the extinction of Land-shells - Ascension - Variation in the imported Rats - Volcanic Bombs - Beds of Infusoria - Bahia - Brazil - Splendour of Tropical Scenery - Pernambuco - Singular Reef - Slavery - Return to England - Retrospect on our Voyage.

APRIL 29th. - In the morning we passed round the northern end of Mauritius, or the Isle of France. From this point of view the aspect of the island equalled the expectations raised by the many well-known descriptions of its beautiful scenery. The sloping plain of the Pamplemousses, interspersed with houses, and coloured by the large fields of sugar-cane of a bright green, composed the foreground. The brilliancy of the green was the more remarkable because it is a colour which generally is conspicuous only from a very short distance. Towards the centre of the island groups of wooded mountains rose out of this highly cultivated plain; their summits, as so commonly happens with ancient volcanic rocks, being jagged into the sharpest points.

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