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ween their last slopes and the beach. Between the ridges lie deep and beautiful valleys, watered by winding streams and teeming with luxuriant vegetation. The rocks of which the islands consist are all igneous, chiefly trachyte, dolerite, basalt, and lava. They are considered by geologists to present perhaps the most wonderful and instructive example of volcanic rocks to be seen on the globe. Yet, though the islands are judged to be of comparatively recent formation, there are no traces of volcanic action in them at the present time. The craters have disappeared: hot springs do not exist; and earthquakes are rare.[2] [2] W. Ellis, _Polynesian Researches_, i. 11 _sqq._; C. E. Meinicke, _op. cit._ ii. 152 _sq._; A. v. H[uegel], _op. cit._ p. 22; F. H. H. Guillemard, _op. cit._ p. 513. The Society Islands, and Tahiti in particular, are famous for the beauty of their natural scenery; indeed, by general consent they appear to rank as the fairest islands in the Pacific. Travellers vie with each other in praise of their enchanting loveliness. Tahiti, the largest island of the group, may be taken as typical of them all. It consists of two almost circular islands united by a very low and narrow neck of land: the northern and larger island is known as Tahiti the Great (Tahiti nui), the southern and smaller island is known as Tahiti the Little (Tahiti iti). In the centre of each island the mountains rise in craggy peaks, sometimes in the shape of pyramids or sugar-loaves, their rocky sides clothed with every variety of verdure, and enlivened here and there by cataracts falling from lofty cliffs, while the shore is washed by the white-crested waves of the Pacific breaking in foam on the coral reefs or dashing in spray on the beach. The scene is especially striking when beheld for the first time from the sea at sunrise on a fine morning. Then the happy combination of land and water, of precipices and plains, of umbrageous trees drooping their pendent boughs over the sea, and distant mountains shown in sublime outline and richest hues, all blended in the harmony of nature, produces in the beholder sensations of admiration and delight. The inland scenery is of a different character, but not less impressive. There the prospect is occasionally extensive, but more frequently circumscribed. There is, however, a startling boldness in the towering piles of basalt, often heaped in picturesque confusion near the source or margi
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