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Narrative of a Survey of the Intertropical and Western Coasts of Australia - Performed between the years 1818 and 1822 — Volume 1 by Phillip Parker King
page 269 of 378 (71%)

The sea-breeze set in from North-West with the change of tide; as soon as
the sun's meridional altitude was observed we got under sail and steered
to the West-South-West; but were soon after obliged to alter the course
to avoid a shoal on which the sea was breaking within fifty yards of us.
After passing this danger we found ourselves in a deep channel the
seaward limit of which was formed by an extensive reef connected with
Jones' Island. At sunset we anchored within one mile and a half of the
shore in five fathoms and a half, soft sandy mud, off the entrance of a
considerable bight or bay; which appeared to be so nearly blocked up by a
reef of dry rocks that it was doubtful whether we should be able to
penetrate without going round the Eclipse Islands; these islands were so
named in consequence of an eclipse of the moon that took place in the
evening; and the flat-topped mount which is conspicuous on the principal
island of the group was named Eclipse Hill.

October 3.

The next morning was passed in examining the reefs to the southward; we
first landed on the south-east end of Long Island, where a set of
bearings and a tolerable view up the bay were obtained. Long Island is of
a rugged character and formed principally of large water-worn masses of
quartzose sandstone superincumbent upon a basis of the same rock. The
spaces between them were occupied by a variety of plants, the examination
of which fully employed Mr. Cunningham: natives' traces and fireplaces,
and the remains of a turtle-feast were observed; but there were no signs
of the islands having been very recently visited by the Indians: we
afterwards landed upon some dry rocks that lie in the mid-channel, and
whilst I was occupied in taking bearings the boat's crew fished, but with
little success on account of the rapidity of the tide.
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