Narrative of the Voyage of H.M.S. Rattlesnake, Commanded By the Late Captain Owen Stanley, R.N., F.R.S. Etc. During the Years 1846-1850. — Volume 2: Including Discoveries and Surveys in New Guinea, the Louisiade Archipelago, Etc. to Which Is Added the Account of Mr. E.B. Kennedy's Expedition for the Exploration of the Cape York Peninsula. By John Macgillivray, F.R.G.S. Naturalist to the Expedition. — John Shaqi
Narrative of the Voyage of H.M.S. Rattlesnake, Commanded By the Late Captain Owen Stanley, R.N., F.R.S. Etc. During the Years 1846-1850. — Volume 2: Including Discoveries and Surveys in New Guinea, the Louisiade Archipelago, Etc. to Which Is Added the Account of Mr. E.B. Kennedy's Expedition for the Exploration of the Cape York Peninsula. By John Macgillivray, F.R.G.S. Naturalist to the Expedition.MacGillivray, John
History
Narrative of the Voyage of H.M.S. Rattlesnake, Commanded By the Late Captain Owen Stanley, R.N., F.R.S. Etc. During the Years 1846-1850. — Volume 2: Including Discoveries and Surveys in New Guinea, the Louisiade Archipelago, Etc. to Which Is Added the Account of Mr. E.B. Kennedy's Expedition for the Exploration of the Cape York Peninsula. By John Macgillivray, F.R.G.S. Naturalist to the Expedition.
MacGillivray, John
Kennedy, Edmund Besley Court, 1818-1848; Natural history -- Oceania; Oceania -- Description and travel; Rattlesnake (Ship); Stanley, Owen
The most important practical result of Captain Stanley's survey of the
Louisiade Archipelago and the south coast of New Guinea, was the
ascertaining the existence of a clear channel of at least 30 miles in
width along the southern shores of these islands, stretching east and
west between Cape Deliverance and the north-east entrance to Torres
Strait--a distance of about 600 miles. This space was so traversed by the
two vessels of the expedition without any detached reefs being
discovered, that it does not seem probable that any such exist there,
with the exception of the Eastern Fields of Flinders, the position and
extent of which may be regarded as determined with sufficient accuracy
for the purposes of navigation, and the reefs alluded to in Volume 1,
which, if they exist at all, and are not merely the Eastern Fields laid
down far to the eastward of their true position, must be sought for
further to the southward. The shores in question may now be approached
with safety, and vessels may run along them either by day or night under
the guidance of the chart--without incurring the risk of coming upon
unknown reefs, such as doubtless exist in other parts of the Coral Sea
further to the southward--judging from the occasional discovery of a new
one by some vessel which had got out of the beaten track. Whalers will no
doubt find it worth their while--with the characteristic enterprise of
their class--to push into those parts of the Coral Sea now first thrown
open to them, and, although we have not as yet sufficient grounds to
warrant the probability of success in the fishery, yet I may mention that
whales were seen on several occasions from both of our vessels.
USEFUL PRODUCTIONS OF NEW GUINEA.
This naturally originates the question--to what extent do the Louisiade
Archipelago and the south-east coast of New Guinea afford a field for
commercial enterprise? What description of trade can be established there
by bartering European goods for the productions of these countries?
Unfortunately at present most of the evidence on this point is of a
negative kind. Besides articles of food, such as pigs, yams, and
coconuts, and weapons and ornaments of no marketable
value--tortoise-shell, flax, arrowroot, massoy bark, and feathers of the
birds of paradise were seen by us, it is true, but in such small
quantities as to hold out at present no inducement for traders to resort
to these coasts for the purpose of procuring them. That gold exists in
the western and northern portions of New Guinea has long been known, that
it exists also on the south-eastern shores of that great island is
equally true, as a specimen of pottery procured at Redscar Bay contained
a few small laminar grains of this precious metal. The clay in which the
gold is embedded was probably part of the great alluvial deposit on the
banks of the rivers, the mouths of which we saw in that neighbourhood,
doubtless originating in the high mountains behind, part of the Owen
Stanley Range.
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