Some of the
natives were observed much darker than others, and there appeared
a mixture of some races. Their numerals were as follows:--
"1 Tashi.
2 Rua.
3 Toru.
4 Fa.
5 Hima.
6 Ono.
7 Fithu.
8 Warru.
9 Hiva.
10 Tanga, foru."
The isolated basaltic rocks in the centre of the valley may give rise to
some curious speculations on the origin of this island. It has long been
decided that basaltic rocks are of igneous origin, in opposition to the
theory of Werner--that they were deposited by the ocean on the summits
of elevated mountains. May not the occurrence of these basalt rocks
therefore illustrate the more immediate volcanic origin of Tucopia?
The second Cut represents the PIERCY ISLANDS, two barren islets situated
a short distance off Cape Bret, (New Zealand,) near the entrance of the
Bay of Islands: one is of very small size, and appears connected to the
other by a ledge of rocks visible at low water. The larger one is quoin
shaped, and has a remarkable perforation, seen in the sketch.
[1] Member of the Royal College of Surgeons in London, &c.
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