The Earth as Modified by Human ActionMarsh, George P. (George Perkins)
History
The Earth as Modified by Human Action
Marsh, George P. (George Perkins)
Conservation of natural resources; Human geography; Nature -- Effect of human beings on; Physical geography
This supposed increase in the frequency and quantity of rain in Lower
Egypt is, I think, an error, or at least not an established fact. I have
heard it disputed on the spot by intelligent Franks, whose residence in
that country began before the plantations of Mehemet Ali and Ibrahim
Pacha, and I have been assured by them that meterological observations,
made at Alexandria about the begiuning of this century, show an annual
fall of rain as great as is usual at this day. The mere fact that it did
not rain during the French occupation is not conclusive. Having
experienced a gentle shower of nearly twenty-four hours' duration in
Upper Egypt, I inquired of the local governor in relation to the
frequency of this phenomenon, and was told by him that not of drop of
rain had fallen at that point for more than two years previous.
The belief in the increase of rain in Egypt rests almost entirely on the
observations of Marshal Marmont, and the evidence collected by him in
1836. His conclusions have been disputed, if not confuted, by Joinard
and others, and are probably erroneous. See Foissac, Meteorologie,
German translation, pp. 634-639.
It certainly sometimes rains briskly at Cairo, but evaporation is
exceedingly rapid in Egypt--as any one who ever saw a Fellah woman wash
a napkin in the Nile, and dry it by shaking it a few moments in the air,
can testify; and a heap of grain, wet a few inches below the surface,
would probably dry again without injury. At any rate, the Egyptian
Government often has vast quantities of wheat stored at Boulak in
uncovered yards through the winter, though it must be admitted that the
slovenliness and want of foresight in Oriental life, public and private,
are such that we cannot infer the safety of any practice followed in the
East merely from its long continuance.
Grain, however, may be long kept in the open air in climates much less
dry than that of Egypt, without injury, except to the superficial
layers; for moisture does not penetrate to a great depth in a heap of
grain once well dried and kept well aired. When Louis IX. was making his
preparations for his campaign in the East, he had large quantities of
wine and grain purchased in the Island of Cyprus, and stored up for two
years to await his arrival. "When we were come to Cyprus," says
Joinville, Histoire de Saint Louis, Section 72, 73, "we found there
greate foison of the Kynge's purveyance. . . The wheate and the barley
they had piled up in greate heapes in the feeldes, and to looke vpon,
they were like vnto mountaynes; for the raine, the whyche hadde beaten
vpon the wheate now a longe whyle, had made it to sproute on the toppe,
so that it seemed as greene grasse. And whanne they were mynded to
carrie it to Egypte, they brake that sod of greene herbe, and dyd finde
under the same the wheate and the barley, as freshe as yf menne hadde
but nowe thrashed it."]
Total Climatic Influence of the Forest.
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