Is Mars habitable? A critical examination of Professor Percival Lowell's book "Mars and its canals," with an alternative explanation — John Shaqi
Is Mars habitable? A critical examination of Professor Percival Lowell's book "Mars and its canals," with an alternative explanationWallace, Alfred Russel
Science
Is Mars habitable? A critical examination of Professor Percival Lowell's book "Mars and its canals," with an alternative explanation
Wallace, Alfred Russel
Lowell, Percival, 1855-1916. Mars and its canals; Mars (Planet)
And Professor Pickering's photographs of April 9th and 10th, 1890,
proved that the southern calotte may assume its definitive proportions
in a single night.
[Footnote 6: Areas on Mars so named.]
"No attempt has yet been made to estimate the quantity of water
derivable from the melting of one of these formations; yet the
experiment is worth trying as a help towards defining ideas. Let us
grant that the average depth of snow in them, of the delicate Martian
kind, is twenty feet, equivalent at the most to one foot of water. The
maximum area covered, of 2,400,000 square miles, is nearly equal to that
of the United States, while the whole globe of Mars measures 55,500,000
square miles, of which one-third, on the present hypothesis, is under
cultivation, and in need of water. Nearly the whole of the dark areas,
as we know, are situated in the southern hemisphere, of which they
extend over, at the very least, 17,000,000 square miles; that is to say,
they cover an area, in round numbers, seven times that of the snow-cap.
Only one-seventh of a foot of water, accordingly, could possibly be
made available for their fertilisation, supposing them to get the entire
advantage of the spring freshet. Upon a stint of less than two inches of
water these fertile lands are expected to flourish and bear abundant
crops; and since they completely enclose the polar area they are
necessarily served first. The great emissaries for carrying off the
surplus of their aqueous riches, would then appear to be superfluous
constructions, nor is it likely that the share in those riches due to
the canals and oases, intricately dividing up the wide, dry, continental
plains, can ever be realised.
"We have assumed, in our little calculation, that the entire contents of
a polar hood turn to water; but in actual fact a considerable proportion
of them must pass directly into vapour, omitting the intermediate stage.
Even with us a large quantity of snow is removed aerially; and in the
rare atmosphere of Mars this cause of waste must be especially
effective. Thus the polar reservoirs are despoiled in the act of being
opened. Further objections might be taken to Mr. Lowell's irrigation
scheme, but enough has been said to show that it is hopelessly
unworkable."
It will be seen that the writer of this article accepted the existence
of water on Mars, on the testimony of Sir W. Huggins, which, in view of
later observations, he has himself acknowledged to be valueless. Dr.
Johnstone Stoney's proof of its absence, derived from the molecular
theory of gases, had not then been made public.
_Description of some of the Canals._
Public-domain text, read in full here on John Shaqi.
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