The Fayûm and Lake MœrisBrown, R. H. (Robert Hanbury)
History
The Fayûm and Lake Mœris
Brown, R. H. (Robert Hanbury)
Fayyum (Egypt) -- Description and travel; Moeris, Lake (Egypt)
Mr. Whitehouse, in his latest expression of views, supposes the
Fayûm and the Wadi Raiân were filled to R.L. 30·00. I have given
reasons for concluding there was never any Nile water in the Wadi
Raiân. The evidence furnished also by Nile deposit and fresh-water
shells on the Fayûm side of the entrance at Lahûn shows that the
level of 30 was never reached.
The highest Nile deposit near and on the Fayûm side of Lahûn is
at about R.L. 26·00. The highest in the Fayûm near the Hawârah
pyramid, which is on the edge of the Fayûm basin, is at R.L. 24·50
or thereabouts. The highest level of the lake was probably never
more than one metre above this level, and it is therefore almost
certain that the water-level was never sufficiently high to flow
into the Wadi Raiân; and _if_ it ever did, it must have been but
rarely, when extraordinarily high and prolonged Niles occurred; so
that it must be concluded, if my views are correct, that the normal
condition of the Wadi Raiân was then, as now, that of a dry waterless
depression in the desert, and it cannot therefore be considered as
having been Lake Mœris, or a part of it even, _at any time_.
LINANT’S OBJECTIONS TO THEORY FAVOURED.
_Author’s Views of Lake Mœris generally stated._—I myself agree
with those who are of opinion that the Fayûm Province, or depression,
(including the Gharaq Basin and the neck from Lahûn to Hawârah),
was by itself Lake Mœris, and that within its limits and along its
borders was to be found the inhabited and cultivated region known as
the Arsinoïte Nome, which possibly also extended into the Nile Valley
along the course of the canal connecting the Nile with the lake.
The Fayûm then in its submerged state was, I believe, the Lake
Mœris of Herodotus, Strabo, Diodorus, and Pliny, the modern Lake
Qurûn being the persistent rudiment of this lake, and all that now
remains of its formerly extensive sheet of water. (See Plate XX.)
_Objections urged by Linant against these views._—This is no new
theory. It is found _passim_ before Linant Pasha in 1842 took great
pains to point out its absurdity, but it was his own assumptions
regarding the maximum height which the water surface of Lake Qurûn
could have reached, that created the absurdity. Assuming without
evidence that the villages on the second plateau were all in existence
at the time of Lake Mœris, he limits the level of Lake Qurûn to
the edge of the second plateau, which is the same thing as laying
down that its water surface never rose above R.L. + 10·00.
Having come to this conclusion, he might have spared himself all
his arguments against the theory, other than that which pointed out
that a reservoir in the Fayûm at this level could have been of no
utility in supplementing the low waters of the Nile.
Public-domain text, read in full here on John Shaqi.
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