Evolution (Biology); Glacial epoch; Human beings -- Origin; Human evolution
Having offered these general remarks on the alluvium of the Thames, I
may now say something of the implements hitherto discovered in it. In
the British Museum there is a flint weapon of the spear-headed form,
such as is represented in Figure 8, which we are told was found with
an elephant's tooth at Black Mary's, near Gray's Inn Lane, London. In a
letter dated 1715, printed in Herne's edition of "Leland's Collectanea,"
volume 1 page 73, it is stated to have been found in the presence of Mr.
Conyers, with the skeleton of an elephant.*
(* Evans, "Archaeologia" 1860.)
So many bones of the elephant, rhinoceros, and hippopotamus have been
found in the gravel on which London stands, that there is no reason to
doubt the statement as handed down to us. Fossil remains of all these
three genera have been dug up on the site of Waterloo Place, St. James's
Square, Charing Cross, the London Docks, Limehouse, Bethnal Green, and
other places within the memory of persons now living. In the gravel and
sand of Shacklewell, in the north-east district of London, I have myself
collected specimens of the Cyrena fluminalis in great numbers (see
Figure 17 c), with the bones of deer and other mammalia.
In the alluvium also of the Wey, near Guildford, in a place called Pease
Marsh, a wedge-shaped flint implement, resembling one brought from
St. Acheul by Mr. Prestwich, and compared by some antiquaries to a
sling-stone, was obtained in 1836 by Mr. Whitburn, 4 feet deep in sand
and gravel, in which the teeth and tusks of elephants had been found.
The Wey flows through the gorge of the North Downs at Guildford to join
the Thames. Mr. Austen has shown that this drift is so ancient that one
part of it had been disturbed and tilted before another part was thrown
down.*
(* "Quarterly Journal of the Geological Society" volume 7
1851 page 278.)
Among other places where flint tools of the antique type have been met
with in the course of the last three years, I may mention one of an oval
form found by Mr. Whitaker in the valley of the Darent, in Kent, and
another which Mr. Evans found lying on the shore at Swalecliff, near
Whitstable, in the same county, where Mr. Prestwich had previously
described a freshwater deposit, resting on the London Clay, and
consisting chiefly of gravel, in which an elephant's tooth and the bones
of a bear were embedded. The flint implement was deeply discoloured
and of a peculiar bright light-brown colour, similar to that of the old
fluviatile gravel in the cliff.
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