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At Last by Charles Kingsley
page 80 of 501 (15%)
that more would be recognised, up and down the island, by the eye of
a practised geologist.

The southern end of Grenada--of whatsoever rock it may be composed--
shows evidence of the same wave-destruction as do the Grenadines.
Arches and stacks, and low horizontal strata laid bare along the
cliff, in some places white with guano, prove that the sea has been
at work for ages, which must be many and long, considering that the
surf, on that leeward side of the island, is little or none the
whole year round. With these low cliffs, in strongest contrast to
the stately and precipitous southern point of St. Lucia, the
southern point of Grenada slides into the sea, the last of the true
Antilles. For Tobago, Robinson Crusoe's island, which lies away
unseen to windward, is seemingly a fragment of South America, like
the island of Trinidad, to which the steamer now ran dead south for
seventy miles.

It was on the shortest day of the year--St. Thomas's Day--at seven
in the morning (half-past eleven of English time, just as the old
women at Eversley would have been going round the parish for their
'goodying'), that we became aware of the blue mountains of North
Trinidad ahead of us; to the west of them the island of the Dragon's
Mouth; and westward again, a cloud among the clouds, the last spur
of the Cordilleras of the Spanish Main. There was South America at
last; and as a witness that this, too, was no dream, the blue water
of the Windward Islands changed suddenly into foul bottle-green.
The waters of the Orinoco, waters from the peaks of the Andes far
away, were staining the sea around us. With thoughts full of three
great names, connected, as long as civilised man shall remain, with
those waters--Columbus, Raleigh, Humboldt--we steamed on, to see
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