e rocks seen by the Fredensberg Castle in 1777 are certainly the
Montebello Isles, which answer the Dane's description exactly; for they
are very low and rocky and abound in reefs, one of which extends a long
distance to the north-west from Trimouille Island. There remains no doubt
in my mind but that Barrow's Island and Trimouille Island, and the
numerous reefs around them, are the identical Tryal Rocks which have been
the theme and dread of every voyager to the eastern islands for the two
last centuries.* Captain Flinders** spent some days in an ineffectual
search for them and has, I think, decidedly proved their non-existence
between the parallels of 20 1/4 and 21 degrees, and the meridians of 103
1/2 and 106 1/2 degrees. The above islands accord exactly as to latitude;
and the only argument against the probability of this supposition is
their longitude; but during the month of July the current sets with great
strength to the westward and might occasion considerable errors in ships'
reckonings, which, in former days, were so imperfectly kept that no
dependence can be placed upon them.
(*Footnote. The Tryal Rocks obtained their name from the English ship
Tryal, said to have been lost upon them in 1622 (vide Horsburg's Indian
Directory volume 1 page 100). This danger having been once laid down
will, perhaps, never be erased from the chart, although it is generally
believed not to exist. It has been placed in various positions according
to the account which the compiler gives most credence to. In Arrowsmith's
large chart of the South Sea it is laid down in 20 degrees 40 minutes
South and 104 1/2 degrees East.)
(**Footnote. Flinders volume 2 pages 261 to 263.)
1820. November 1.
The following afternoon the man at the masthead reported breakers in the
West-North-West, and when I went to examine from thence I was for some
time equally deceived: the helm was put up and we bore down towards them
but, as we approached, they vanished and we found we had been deceived by
the reflection of the sun's rays upon the water.* After being
sufficiently assured of our mistake, the course was resumed.
(*Footnote. The deceptious appearances that are frequently observed at
sea, such as the reflection of the sun, ripplings occasioned by the
meeting of two opposite currents, whales asleep upon the surface of the
water, shoals of fish, fog-banks, and the extraordinary effect of mirage,
than which, as an optical illusion, nothing is mo
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