Evolution (Biology); Glacial epoch; Human beings -- Origin; Human evolution
A remarkable absence of lamination and stratification was observed
almost universally in the sediment brought up from all points except
where the sandy layers above alluded to occurred. Mr. Horner attributes
this want of all indication of successive deposition to the extreme
thinness of the film of matter which is thrown down annually on the
great alluvial plain during the season of inundation. The tenuity of
this layer must indeed be extreme, if the French engineers are tolerably
correct in their estimate of the amount of sediment formed in a century,
which they suppose not to exceed on the average 5 inches. When the
waters subside, this thin layer of new soil, exposed to a hot sun, dries
rapidly, and clouds of dust are raised by the winds. The superficial
deposit, moreover, is disturbed almost everywhere by agricultural
labours, and even were this not the case, the action of worms, insects,
and the roots of plants would suffice to confound together the deposits
of two successive years.
All the remains of organic bodies, such as land-shells, and the bones
of quadrupeds, found during the excavations belonged to living species.
Bones of the ox, hog, dog, dromedary and ass were not uncommon, but no
vestiges of extinct mammalia. No marine shells were anywhere detected;
but this was to be expected, as the borings, though they sometimes
reached as low as the level of the Mediterranean, were never carried
down below it--a circumstance much to be regretted, since where artesian
borings have been made in deltas, as in those of the Po and Ganges, to
the depth of several hundred feet below the sea level it has been
found, contrary to expectation, that the deposits passed through were
fluviatile throughout, implying, probably, that a general subsidence of
those deltas and alluvial formations has taken place. Whether there has
been in like manner a sinking of the land in Egypt, we have as yet no
means of proving; but Sir Gardner Wilkinson infers it from the position
in the delta on the shore near Alexandria of the tombs commonly called
Cleopatra's Baths, which cannot, he says, have been originally built so
as to be exposed to the sea which now fills them, but must have stood on
land above the level of the Mediterranean. The same author adduces, as
additional signs of subsidence, some ruined towns, now half under water,
in the Lake Menzaleh, and channels of ancient arms of the Nile submerged
with their banks beneath the waters of that same lagoon.
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.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account