LITMIR.BIZ

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and Late.133 A third new volcanic island seems to have been formed to the south of Tufoa in 1886.134 Another new island was thrown up from the sea about the beginning of the twentieth century; it was partly washed away again, but has again materially increased in size.135 It is noteworthy that the volcanoes, new or old, all occur in a line running roughly north and south at a considerable distance to the west of, but parallel to, the main body of the Tongan archipelago. They clearly indicate the existence of submarine volcanic action on a great scale. Even in the coralline islands traces of volcanic agency have come to light in the shape of pumice-stones, which have been dug out of the solid coral rock at considerable depths.136 In the lofty island of Eua an extensive dyke of basalt is found inland underlying the coral formation.137

      These facts lend some countenance to the view that the whole archipelago forms the summit or visible ridge of a long chain of submarine volcanoes, and that the islands, even those of coralline formation, have been raised to their present level by volcanic action.138 That very acute observer, Captain Cook, or one of the naturalists of the expedition, noticed that in the highest parts of Tongataboo, which he estimated roughly at a hundred feet above sea-level, he often met with "the same coral rock, which is found at the shore, projecting above the surface, and perforated and cut into all those inequalities which are usually seen in rocks that lie within the wash of the tide."139 Again, on ascending the comparatively lofty island of Eua, Captain Cook observes: "We were now about two or three hundred feet above the level of the sea, and yet, even here, the coral was perforated into all the holes and inequalities which usually diversify the surface of this substance within the reach of the tide. Indeed, we found the same coral till we began to approach the summits of the highest hills; and, it was remarkable, that these were chiefly composed of a yellowish, soft, sandy stone."140 In the island of Vavau it was remarked by Captain Waldegrave that the coral rock rises many feet above the present level of the sea, and he adds: "The action of fire is visible on it, and we saw several instances of its crystallisation."141

      The view that even the coralline islands of the Tongan archipelago have been elevated by volcanic agency is not necessarily inconsistent with Darwin's theory that coral reefs are formed during periods of subsidence, not of elevation;142 for it is quite possible that, after being raised ages ago by volcanic forces, these islands may be now slowly subsiding, and that it has been during the period of subsidence that they have become incrusted by coral reefs. Yet the occurrence of coral rocks, bearing all the marks of marine action, at considerable heights above the sea, appears indubitably to prove that such a general subsidence has been in some places varied by at least a temporary elevation.

      In thus postulating elevation by volcanic action, as well as subsidence, to explain the formation of the Tongan islands I am glad to have the support of a good observer, the late Rev. Dr. George Brown, who spent the best years of his life in the Pacific, where his experience both of the larger and the smaller islands was varied and extensive. He writes: "I have seen islands composed of true coralline limestone, the cliffs of which rise so perpendicularly from the blue ocean that the natives have to ascend and descend by ladders in going from the ocean to the top, or vice versa. A large steamer can go so close to some of these cliffs that she could be moored alongside of them in calm weather. It is not at all improbable, I think, that in these islands we have the two factors in the formation of islands, viz. subsidence, during which these immense cliffs were formed, and subsequent upheaval. This is the only way, I think, in which we can account for these perpendicular cliffs in the midst of deep blue ocean."143

      I have dwelt at what may seem undue length on the volcanic phenomena of the Tonga islands because the occurrence of such phenomena in savage lands has generally influenced the beliefs and customs of the natives, quite apart from the possibility, which should always be borne in mind, that man first obtained fire from an active volcano. But even if, as has been suggested, the Tonga islands formed the starting-point from which the Polynesian race spread over the islands of the Pacific,144 it seems very unlikely that the Polynesians first learned the use of fire when they reached the Tongan archipelago. More probably they were acquainted, not only with the use of fire, but with the mode of making it long before they migrated from their original home in Southern Asia. A people perfectly ignorant of that prime necessity could hardly have made their way across such wide stretches of sea and land. But it is quite possible that the myth which the Tongans, in common with many other Polynesians, tell of the manner in which their ancestors procured their first fire, was suggested to them by the spectacle of a volcano in eruption. They say that the hero Maui Kijikiji, the Polynesian Prometheus, first procured fire for men by descending into the bowels of the earth and stealing it from his father, Maui Atalanga, who had kept it there jealously concealed.145

      § 2. The Tonga Islanders, their Character, Mode of Life, and Government

      Physically the Tonga islanders are fine specimens of the Polynesian race and generally impress travellers very favourably. Captain Cook, the first to observe them closely, describes them as very strong and well made, some of them really handsome, and many of them with truly European features and genuine Roman noses.146 At a later date Commodore Wilkes, the commander of the United States Exploring Expedition, speaks of them as "some of the finest specimens of the human race that can well be imagined, surpassing in symmetry and grace those of all the other groups we had visited"; and farther on he says: "A larger proportion of fine-looking people is seldom to be seen, in any portion of the globe; they are a shade lighter than any of the other islanders; their countenances are generally of the European cast; they are tall and well made, and their muscles are well developed."147 Still later, in his account of the voyage of the Challenger, Lord George Campbell expressed himself even more warmly: "There are no people in the world," he says, "who strike one at first so much as these Friendly Islanders. Their clear, light, copper-brown coloured skins, yellow and curly hair, good-humoured, handsome faces, their tout ensemble, formed a novel and splendid picture of the genus homo; and, as far as physique and appearance go, they gave one certainly an impression of being a superior race to ours."148 A Catholic missionary observes that "the natives of Tonga hardly differ from Europeans in stature, features, and colour; they are a little sallower, which may be set down to the high temperature of the climate. It is difficult to have a very fresh complexion with thirty degrees of heat, Réaumur, as we have it during four or five months of the year."149 In appearance the Tonga islanders closely resemble the Samoans, their neighbours on the north; some find them a little lighter, but others somewhat darker in colour than the Samoans.150 According to the French explorer, Dumont d'Urville, who passed about a month in Tongataboo in 1827, the Polynesian race in Tonga exhibits less admixture with the swarthy Melanesian race than in Tahiti and New Zealand, there being far fewer individuals of stunted stature, flat noses, and frizzly hair among the Tongans than among the other Polynesians.151 Even among the Tongans the physical superiority of the chiefs to the common people is said to be conspicuous; they are taller, comelier, and lighter in colour than the lower orders. Some would explain the difference by a difference in upbringing, noblemen being more carefully nursed, better fed, and less exposed to the sun than commoners;152 but it is possible that they come of a different and better stock.

      Intellectually the Tongans are reported to "surpass all the other South Sea islanders in their mental development, showing great skill in the structure of their dwellings and the manufacture of their implements, weapons,

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