a, but the rest of the island consists
of low ground, excepting a round bluff head on the S.E. point. It produces
abundance of yams, and of the sweet root called _Tee_, but we got from
it no other sort of provisions.
Oreehow aad Tahoora are two small islands in the neighbourhood of Oneeheow.
The former is a single high hummock, joined by a reef of coral rocks to the
northern extremity of Oneeheow. The latter lies to the S.W., and is
uninhabited.
The climate of the Sandwich islands differs very little from that of the
West India islands, which lie in the same latitude. Upon the whole,
perhaps, it may be rather more temperate. The thermometer on shore in
Karakakooa Bay, never rose higher than 88 deg., and that but one day; its mean
height at noon was 83 deg.. In Wymoa Bay, its mean height at noon was 76 deg., and
when out at sea 75 deg.. The mean height of the thermometer at noon, in
Jamaica, is about 86 deg., at sea 80 deg..
Whether they be subject to the same violent winds and hurricanes, we could
not discover, as we were not there in, any of the stormy months. However,
as the natives gave us no positive testimony of the fact, and no traces of
their effects were any where visible, it is probable that, in this respect,
they resemble the Society and Friendly islands, which are, in a great
measure, free from these dreadful visitations.
During the four winter months that we remained amongst these islands, there
was more rain, especially in the interior parts, than usually falls during
the dry season in the islands of the West Indies. We generally saw clouds
collecting round the tops of the hills, and producing rain to leeward; but
after they are separated from the land by the wind, they disperse and are
lost, and others succeed in their place. This happened daily at Owhyhee;
the mountainous parts being generally enveloped in a cloud; successive
showers falling in the inland country, with fine weather, and a clear sky
at the sea-shore.
The winds in general were from E.S.E. to N.E.; though they sometimes varied
a few points each way to the N. and S, but these were light, and of short
duration. In the harbour of Karakakooa we had a constant land and sea-
breeze every day and night.
The currents seemed very uncertain, sometimes setting to windward, and at
other times to leeward, without any regularity. They did not appear to be
governed by the winds, nor any other cause that I can assign; they
frequently set to wind
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