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Chapters (26)
  1. CAPTAIN COOK'S JOURNAL.FIRST VOYAGE.
  2. CAPTAIN COOK'S JOURNAL DURING HIS FIRST VOYAGE ROUND THE WORLD MADE IN H.M. BARK "ENDEAVOUR" 1768-71A Literal Transcription of the Original MSS.EDITED BY CAPTAIN W.J.L. WHARTON, R.N., F.R.S.
  3. PREFACE.
  4. SKETCH OF CAPTAIN COOK'S LIFE.
  5. PERSONS WHO LEFT ENGLAND IN H.M.S. ENDEAVOUR, 26TH AUGUST, 1768.
  6. A JOURNAL OF THE PROCEEDINGS OF HIS MAJESTY'S BARK ENDEAVOUR,ON A VOYAGE ROUND THE WORLD, BY LIEUTENANT JAMES COOK,COMMANDER, COMMENCING THE 25TH OF MAY, 1768.
  7. CHAPTER 1. ENGLAND TO RIO JANEIRO.
  8. CHAPTER 2. RIO JANEIRO TO TAHITI.
  9. MODERN CHART OF SOUTH PACIFIC OCEAN SHOWING TRACK OF H.M.S. ENDEAVOUR, 1769 TO 1770.
  10. CHAPTER 3. TAHITI.
  11. FACSIMILE OF SATURDAY, 3RD JUNE, 1769.
  12. CHART OF THE ISLAND OTAHEITE, BY LIEUTENANT JAMES COOK, 1769. REPRODUCTION OF THE ORIGINAL PUBLISHED CHART.
  13. TAHITI: TYPES OF CANOES.
  14. CHAPTER 4. TAHITI TO NEW ZEALAND.
  15. CHAPTER 5. EXPLORATION OF NORTH ISLAND OF NEW ZEALAND.
  16. CHAPTER 6. EXPLORATION OF MIDDLE ISLAND OF NEW ZEALAND.
  17. WAR CANOE OF NEW ZEALAND.
  18. CHAPTER 7. PASSAGE FROM NEW ZEALAND TO NEW HOLLAND.
  19. CHAPTER 8. EXPLORATION OF EAST COAST OF AUSTRALIA.
  20. CHAPTER 9. FROM TORRES STRAIT TO BATAVIA.
  21. TRACK OF ENDEAVOUR FROM TORRES STRAIT TO JAVA. AUGUST AND SEPTEMBER 1770.
  22. FACSIMILE OF TUESDAY, 23RD OCTOBER, 1770.
  23. CHAPTER 10. BATAVIA TO CAPE OF GOOD HOPE.
  24. CHAPTER 11. CAPE OF GOOD HOPE TO ENGLAND.
  25. INDEX.
  26. CHART OF NEW ZEALAND, EXPLORED IN 1769 AND 1770, BY LIEUTENANT J. COOK, COMMANDER OF HIS MAJESTY'S BARK ENDEAVOUR, ENGRAVED BY I. BAYLY.REPRODUCTION OF THE ORIGINAL PUBLISHED CHART.

The meeting of Westerly winds within the general Limits of the Easterly Trade is a little extraordinary, and has induced former Navigators, when they met with them, to think that they were caused by the nearness of some large Tracks of Land: but I rather think they were owing to another Cause. It hath been found both by the Dolphin and us that the trade winds in those parts of this Sea doth not extend further to the Southward than 20 degrees, and without which we generally meet with a wind from the westward. Now, is it not reasonable to suppose that when these winds blow strong they must encroach upon and drive back the Easterly winds as to cause the variable winds and South-Westerly swells I have been speaking of? It is well known that the Trade winds blow but faint for some distance within their limits, and are therefore easily stopt by a wind from the Contrary direction. It is likewise known that these limits are subject to vary several degrees, not only at different seasons of the Year, but at one and the same season. Another reason why I think that these South-West winds are not caused by the nearness of any large Track of land, is in their being always accompanied with a large swell from the same Quarter, and we find a much greater surf beating upon the Shores of the South-West sides of the Islands situated just within the Limits of the Trade winds than upon any other part of them.

The tides are perhaps as inconsiderable in these Seas as in any part of the world. A South or South by West moon makes high water in Royal Bay, but the water does not rise upon a perpendicular above 10 or 12 inches, except on some very Extraordinary occasions.