Evolution (Biology); Glacial epoch; Human beings -- Origin; Human evolution
Almost every one of these ancient boats was formed out of a single
oak-stem, hollowed out by blunt tools, probably stone axes, aided by
the action of fire; a few were cut beautifully smooth, evidently with
metallic tools. Hence a gradation could be traced from a pattern of
extreme rudeness to one showing great mechanical ingenuity. Two of them
were built of planks, one of the two, dug up on the property of Bankton
in 1853, being 18 feet in length, and very elaborately constructed. Its
prow was not unlike the beak of an antique galley; its stern, formed of
a triangular-shaped piece of oak, fitted in exactly like those of our
day. The planks were fastened to the ribs, partly by singularly shaped
oaken pins, and partly by what must have been square nails of some kind
of metal; these had entirely disappeared, but some of the oaken pins
remained. This boat had been upset, and was lying keel uppermost,
with the prow pointing straight up the river. In one of the canoes, a
beautifully polished celt or axe of greenstone was found, in the bottom
of another a plug of cork, which, as Mr. Geikie remarks, "could only
have come from the latitudes of Spain, Southern France, or Italy."*
(* Geikie, "Quarterly Journal of the Geological Society"
volume 18 1862 page 224.)
There can be no doubt that some of these buried vessels are of far more
ancient date than others. Those most roughly hewn, may be relics of
the stone period; those more smoothly cut, of the bronze age; and the
regularly built boat of Bankton may perhaps come within the age of
iron. The occurrence of all of them in one and the same upraised marine
formation by no means implies that they belong to the same era, for
in the beds of all great rivers and estuaries, there are changes
continually in progress brought about by the deposition, removal, and
redeposition of gravel, sand, and fine sediment, and by the shifting of
the channel of the main currents from year to year, and from century
to century. All these it behoves the geologist and antiquary to bear in
mind, so as to be always on their guard, when they are endeavouring
to settle the relative date, whether of objects of art or of organic
remains embedded in any set of alluvial strata. Some judicious
observations on this head occur in Mr. Geikie's memoir above cited,
which are so much in point that I shall give them in full, and in his
own words.
Public-domain text, read in full here on John Shaqi.
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