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%)
page 269 of 378 (71%)
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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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