The Meeting-Place of Geology and HistoryDawson, John William, Sir
Religion
The Meeting-Place of Geology and History
Dawson, John William, Sir
Deluge; Prehistoric peoples
This next period, that known to geologists as the post-glacial or early
modern, was characterised by an entire change of physical conditions.
The continents of the northern hemisphere were higher and wider than
now. The details of this we have already considered, and have seen that
at this time the Mediterranean was divided into two basins, and a broad
fringe of low land, now submerged, lay around its eastern end. This was
the age of those early palæolithic or palæocosmic men whose remains are
found in the caverns and gravels of Europe and Asia. What was the
condition of Egypt at this time? The Nile must have been flowing in its
valley; but there was probably a waterfall or cataract at Silsilis in
Upper Egypt, and rapids lower down, and the alluvial plain was much less
extensive than now and forest-clad, while the river seems to have been
unable to reach the Mediterranean and to have turned abruptly eastward,
discharging into a lake where the Isthmus of Suez now is, and probably
running thence into the Red Sea, so that at this time the waters of the
Nile approached very near to those of the Jordan, a fact which accounts
for that similarity of their modern fauna which has been remarked by so
many naturalists. I have myself collected in the deposits of this old
lake, near Ismailia, fresh-water shells of kinds now living in the Upper
Nile. If at this time men visited the Nile valley, they must have been
only a few bold hunters in search of game, and having their permanent
homes on the Mediterranean plains now submerged.
Public-domain text, read in full here on John Shaqi.
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