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
We remained at this anchorage for upwards of a week, during which a rate
for the chronometers was obtained, and the Bramble returned.
WEATHER DURING WESTERLY MONSOON.
The weather during our stay was very variable and unsettled; rain fell on
several occasions. The wind was usually from the westward, varying
between North-West and South-West, and on one occasion during the night
we had a sudden and very violent squall from the westward, which for a
time was thought to be the beginning of a hurricane, but the gale
moderated very gradually next day. When the wind during the day was light
and from seaward, a land breeze generally came off at night, occasionally
with rain. The cause of this last seems to be the influence exerted upon
the winds here by Mount Owen Stanley and the ranges connected with it,
from which the clouds accumulated during the prevalence of the seabreeze,
are reflected after its subsidence. The low and well wooded district
between the mountains and the sea receives the passing influence of these
clouds surcharged with moisture, and the climate there and in all the low
maritime districts of the south-east part of New Guinea backed by high
land, is probably always a moist one, little affected by the prevalence
of either the North-West or South-East monsoon. The observations made
during our last visit to determine the height of Mount Owen Stanley and
not considered very satisfactory, were repeated under more favourable
conditions, but with nearly the same result. This mountain, the highest
of the range of the same name, is somewhat flat-topped (as viewed from
our anchorage) about six miles in length, and the mean of five
observations from different stations gave 13,205 feet as the height of
the highest part above the level of the sea.
PARIWARA ISLAND.
On the largest Pariwara Island, although abundance of rain had fallen
lately, there was no water left in any pool or hole in the rock. Nor
although the soil, from the additional moisture, looked darker and richer
than during my former visit in September, was there any perceptible
improvement in the vegetation. A few fork-tailed red-fronted swallows
(Hirundo neoxena) were hawking about, and a large yellow and black
butterfly (Papilio epius, common in collections from India and China) was
abundant. Many Torres Strait pigeons were observed from the ship to
resort nightly to the second largest of the group, which is covered with
trees and seems quite inaccessible from the steepness of its low cliffs.
On several successive evenings about sunset, and until it became too dark
to distinguish them, immense numbers of frigate-birds were observed
flying over Redscar Head, and going out to the North-North-East. This
being a gregarious bird only when associated at a breeding place, and
there being no known sandbank or islet in the direction which they were
pursuing, rendered their object a subject for much conjecture.
MANY NATIVES VISIT US.
Public-domain text, read in full here on John Shaqi.
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