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Voyages in the Southern Hemisphere, Vols. II - IIIVoyaging Accounts
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On this day ...
4 - 5 June 1770


Endeavour Voyage Maps

James Cook's Journal Ms 1, National Library of Australia

Transcript of Cook's Journal

Joseph Banks's Journal

Sydney Parkinson's Journal


Range from Botany Bay to Trinity Bay


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Range from Botany Bay to Trinity Bay (continued)

but without staying to look into it, we continued our course to the westward, for the farthest land we could see in that direction, which bore W. by N. ½ N. and appeared very high. At noon, we were about three leagues from the shore, by observation in latitude 19° 47’ S. and Cape Gloucester bore S. 63 E. distant seven leagues and an half. At six in the evening, we were abreast of the westermost point just mentioned, at about three miles distance, and because it rises abruptly from the low lands which surround it, I called it CAPE UPSTART. It lies in latitude 19° 39’ S. longitude 212° 32’ W. fourteen leagues W.N.W. from Cape Gloucester, and is of a height sufficient to be seen at the distance of twelve leagues: inland there are some high hills or mountains, which, like the Cape, afford but a barren prospect. Having passed this Cape, we continued standing to the W.N.W. as the land lay, under an easy sail, having from sixteen to ten fathom, till two o’clock in the morning, when we fell into seven fathom; upon which we hauled our wind to the northward, judging ourselves to be very near land: at day-break, we found our conjecture to be true, being within little more than two leagues of it. In this part of the coast the land, being very low, is nearer than it appears to be, though it is diversified with here and there a hill. At noon, we were about four leagues from the land, in fifteen fathom water, and our latitude, by observation, was 19° 12’ S. Cape Upstart bearing S. 32° 30’ E. distant twelve leagues. About this time some very large columns of smoke were seen rising from the low lands. At sun-set, the preceding night, when we were close under Cape Upstart, the variation was nearly 9° E. and at sun-rise this day, it was no more than 5° 35’; I judged therefore that it had been influenced by iron ore, or other magnetical matter, contained under the surface of the earth.


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© Derived from Vols. II-III of the London 1773 edition: National Library of Australia call no. FERG 7243, page 538, 2004
Published by kind permission of the Library
To cite this page use: https://paulturnbull.org/project/southseas/journals/hv23/538.html