Curiosities of Science, Past and Present: A Book for Old and YoungTimbs, John
Science
Curiosities of Science, Past and Present: A Book for Old and Young
Timbs, John
Science
The importance of glacier agency in the past as well as the present
condition of the earth, is undoubtedly very great. One of our most
accomplished and ingenious geologists has, indeed, carried back the
existence of Glaciers to an epoch of dim antiquity, even in the
reckoning of that science whose chronology is counted in millions of
years. Professor Ramsay has shown ground for believing that in the
fragments of rock that go to make up the conglomerates of the Permian
strata, intermediate between the Old and the New Red Sandstone, there
is still preserved a record of the action of ice, either in glaciers
or floating icebergs, before those strata were consolidated.--_Saturday
Review_, No. 142.
FLOW OF THE MER DE GLACE.
Michel Devouasson of Chamouni fell into a crevasse on the Glacier
of Talefre, a feeder of the Mer de Glace, on the 29th of July 1836,
and after a severe struggle extricated himself, leaving his knapsack
below. The identical knapsack reappeared in July 1846, at a spot on
the surface of the glacier _four thousand three hundred_ feet from
the place where it was lost, as ascertained by Professor Forbes, who
himself collected the fragments; thus indicating the rate of flow of
the icy river in the intervening ten years.--_Quarterly Review_, No.
202.
THE ALLUVIAL LAND OF EGYPT: ANCIENT POTTERY.
Mr. L. Horner, in his recent researches near Cairo, with the view of
throwing light upon the geological history of the alluvial land of
Egypt, obtained from the lowest part of the boring of the sediment at
the colossal statue of Rameses, at a depth of thirty-nine feet, this
curious relic of the ancient world; the boring instrument bringing up
a fragment of pottery about an inch square and a quarter of an inch in
thickness--the two surfaces being of a brick-red colour, the interior
dark gray. According to Mr. Horner’s deductions, this fragment, having
been found at a depth of 39 feet (if there be no fallacy in his
reasoning), must be held to be a record of the existence of man 13,375
years before A.D. 1858, reckoning by the calculated rate of increase of
three inches and a half of alluvium in a century--11,517 years before
the Christian era, and 7625 before the beginning assigned by Lepsius
to the reign of Menos, the founder of Memphis. Moreover it proves in
his opinion, that man had already reached a state of civilisation, so
far at least as to be able to fashion clay into vessels, and to know
how to harden it by the action of strong heat. This calculation is
supported by the Chevalier Bunsen, who is of opinion that the first
epochs of the history of the human race demand at the least a period
of 20,000 years before our era as a fair starting-point in the earth’s
history.--_Proceedings of Royal Soc._, 1858.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account