The Three Voyages of William Barents to the Arctic Regions (1594, 1595, and 1596)Veer, Gerrit de
History
The Three Voyages of William Barents to the Arctic Regions (1594, 1595, and 1596)
Veer, Gerrit de
Barentsz, Willem, approximately 1550-1597; Northeast Passage
In this report the learned Professor comes to widely different
conclusions from those of Lütke with respect to the identification of
the several stations visited by the Dutch; the great point of
difference between them being, that Baer bases his arguments almost
exclusively on the distances along the western coast of Novaya Zemlya
recorded by De Veer, especially in the Table given near the end of his
third voyage. [185]
This Table, however, we cannot but regard as little better than a mere
list of the various stations reached by the Dutch on their return
voyage; the distances, and even the bearings, therein recorded, being
quite untrustworthy, as may indeed be perceived on the most cursory
inspection. Every allowance has, of course, to be made for any
inaccuracies that may exist in that Table, in consideration of the
circumstances under which the return voyage was made; but, even were we
to assume the distances sailed by them in their two small open boats to
have been correctly noted down, still there is a sufficient reason for
contending that those distances, in themselves, are no sure guide, but,
on the contrary, only lead to very erroneous conclusions. For, on a
comparison of them with the differences of latitude recorded by De
Veer,—which, as being the results of astronomical observations made by
so experienced a navigator as Barents was, are subject only to the
imperfections of the instruments employed by him,—it will be seen that
the former, especially between Langenes and Cape Nassau, are throughout
much too small. No reason is given by De Veer for this discrepancy;
and, indeed, it would be difficult to account for it, were it not for
the fact established by the observations of Admiral Lütke, that a very
powerful current from south to north sets along the western coast of
Novaya Zemlya as far as Cape Nassau. The velocity of this current was
ascertained by that intelligent seaman to be as much as sixty miles per
diem, [186] and owing to it he frequently found himself in a latitude
from forty-five to fifty-five miles further north than was shown by his
dead reckoning. [187] A remarkable confirmation of this fact is
afforded by Henry Hudson’s journal of his visit to Novaya Zemlya,
printed in the Appendix to the present work, [188] in which, under the
date of 28th June 1608, it is stated that, between eight o’clock on the
previous evening and four o’clock in the morning, they were drawn back
to the northwards, by a stream or tide, as far as they were the last
evening at four o’clock. Applying this, then, to the case of our Dutch
navigators, we obtain a satisfactory explanation of the apparent
discrepancies in their several data.
Public-domain text, read in full here on John Shaqi.
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