Narrative of the surveying voyages of His Majesty's ships Adventure and Beagle, between the years 1826 and 1836. Volume I. Proceedings of the First Expedition, 1826-1830 — John Shaqi
Narrative of the surveying voyages of His Majesty's ships Adventure and Beagle, between the years 1826 and 1836. Volume I. Proceedings of the First Expedition, 1826-1830King, Philip Parker
History
Narrative of the surveying voyages of His Majesty's ships Adventure and Beagle, between the years 1826 and 1836. Volume I. Proceedings of the First Expedition, 1826-1830
King, Philip Parker
Adventure and Beagle expedition (1826-1830); Beagle Expedition (1831-1836); Fuegians; Indians of South America -- Patagonia (Argentina and Chile); Natural history -- South America; Patagonia (Argentina and Chile) -- Description and travel; South America -- Description and travel
On the charts of this part of the coast the shore is described to be formed
of "chalk hills, like the coast of Kent." To geologists, therefore,
especially, as they were not disposed to believe that such was the fact,
this was a question of some interest. From our anchorage the appearance of
the land favoured our belief of the existence of chalk. The outline was
very level and steep; precipitous cliffs of whitish colour, stratified
horizontally, with their upper part occasionally worn into hollows,
strongly resembled the chalk cliffs of the English coasts.
The gale prevented our landing for three days, when (19th) a few minutes
sufficed to discover that the cliffs were composed {8} of soft clay,
varying in colour and consistence, and disposed in strata running
horizontally for many miles without interruption, excepting where
water-courses had worn them away. Some of the strata were very fine clay,
unmixed with any other substance, whilst others were plentifully strewed
with round siliceous gravel,[8] without any vestige of organic remains. The
sea beach, from high-water mark to the base of the cliffs, is formed by
shingle, with scattered masses of indurated clay of a green colour.[9]
Between the high and low tide marks there is a smooth beach of the same
green clay as the masses above-mentioned, which appears to have been
hardened by the action of the surf to the consistence of stone. Generally
this beach extends for about one hundred yards farther into the sea, and is
succeeded by a soft green mud, over which the water gradually deepens. The
outer edge of the clay forms a ledge, extending parallel with the coast,
upon the whole length of which the sea breaks, and over it a boat can with
difficulty pass at low water.
The very few shells we found were dead. Strewed about the beach were
numbers of fish, some of which had been thrown on shore by the last tide,
and were scarcely stiff. They principally belonged to the genus _Ophidium_;
the largest that we saw measured four feet seven inches in length, and
weighed twenty-four pounds. Many caught alongside the ship were, in truth,
coarse and insipid; yet our people, who fed heartily upon them, called them
ling, and thought them palatable. The hook, however, furnished us with a
very wholesome and well-flavoured species of cod (_Gadus_). Attached to the
first we found two parasitical animals; one was a _Cymothoa_, the other a
species of _Lernæa_, which had so {9} securely attached itself under the
skin, as not to be removed without cutting off a piece of the flesh with
it. An undescribed species of _Muræna_ was also taken.
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