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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