# Is Mars Habitable?

1907 rebuttal to Mars and its Canals. OCLC:2661357
Lowell's Map of Mars, at the opposition of 1903, showing Solis Lacus near the Top. (From "Nature,", Oct. 11th, 1906)
Is Mars Habitable?
A CRITICAL EXAMINATION OF PROFESSOR PERCIVAL LOWELL'S BOOK "MARS AND ITS CANALS," WITH AN ALTERNATIVE EXPLANATION
BY
ALFRED RUSSEL WALLACE
F.R.S., Etc.
AUTHOR OF "DARWINISM," "MAN'S PLACE IN THE UNIVERSE," ETC.
MACMILLAN AND CO., LIMITED ST. MARTIN'S STREET, LONDON
1907
GLASGOW: PRINTED AT THE UNIVERSITY PRESS BY ROBERT MACLEHOSE AND CO. LTD.
PREFACE.
This small volume was commenced as a review article on Professor Percival Lowell's book, Mars and its Canals with the object of showing that the large amount of new and interesting facts contained in this work did not invalidate the conclusion I had reached in 1902, and stated in my book on Man's Place in the Universe that Mars was not habitable.
But the more complete presentation of the opposite view in the volume now under discussion required a more detailed examination of the various physical problems involved, and as the subject is one of great, popular, as well as scientific interest, I determined to undertake the task.
This was rendered the more necessary by the fact that in July last Professor Lowell published in the Philosophical Magazine an elaborate mathematical article claiming to demonstrate that, notwithstanding its much greater distance from the sun and its excessively thin atmosphere, Mars possessed a climate on the average equal to that of the south of ​England, and in its polar and sub-polar regions even less severe than that of the earth. Such a contention of course required to be dealt with, and led me to collect information bearing upon temperature in all its aspects, and so enlarging my criticism that I saw it would be necessary to issue it in book form.
Two of my mathematical friends have pointed out the chief omission which vitiates Professor Lowell's mathematical conclusions—that of a failure to recognise the very large conservative and cumulative effect of a dense atmosphere. This very point however I had already myself discussed in Chapter VI., and by means of some remarkable researches on the heat of the moon and an investigation of the causes of its very low temperature, I have, I think, demonstrated the incorrectness of Mr. Lowell's results. In my last chapter, in which I briefly summarise the whole argument, I have further strengthened the case for very severe cold in Mars, by adducing the rapid lowering of temperature universally caused by diminution of atmospheric pressure, as manifested in the well-known phenomenon of temperate climates at moderate heights even close to the equator, cold climates at greater heights even on extensive plateaux, culminating in arctic climates and perpetual snow at heights where the air is still far denser than it is on the surface of Mars. This ​argument itself is, in my opinion, conclusive; but it is enforced by two others equally complete, neither of which is adequately met by Mr. Lowell.
The careful examination which I have been led to give to the whole of the phenomena which Mars presents, and especially to the discoveries of Mr. Lowell, has led me to what I hope will be considered a satisfactory physical explanation of them. This explanation, which occupies the whole of my seventh chapter, is founded upon a special mode of origin for Mars, derived from the Meteoritic Hypothesis, now very widely adopted by astronomers and physicists. Then, by a comparison with certain well-known and widely spread geological phenomena, I show how the great features of Mars—the 'canals' and 'oases'—may have been caused. This chapter will perhaps be the most interesting to the general reader, as furnishing a quite natural explanation of features of the planet which have been termed 'non-natural' by Mr. Lowell.
Incidentally, also, I have been led to an explanation of the highly volcanic nature of the moon's surface. This seems to me absolutely to require some such origin as Sir George Darwin has given it, and thus furnishes corroborative proof of the accuracy of the hypothesis that our moon has had an unique origin among the known satellites, in having been thrown off from the earth itself.
​I am indebted to Professor J. H. Poynting, of the University of Birmingham, for valuable suggestions on some of the more difficult points of mathematical physics here discussed, and also for the critical note (at the end of Chapter V.) on Professor Lowell's estimate of the temperature of Mars.
Broadstone, Dorset, October 1907.
TABLE OF CONTENTS.
CHAPTER I.
PAGE
    Mars the only planet the surface of which is distinctly visible—Early observation of the snow-caps and seas—The 'canals' seen by Schiaparelli in 1877—Double canals first seen in 1881—Round spots at intersection of canals seen by Pickering in 1892—Confirmed by Lowell in 1894—Changes of colour seen in 1892 and 1894—Existence of seas doubted by Pickering and Barnard in 1894.
CHAPTER II.
    Observatory at Flagstaff, Arizona—Illustrated book on his observations of Mars—Volume on Mars and its canals, 1906—Non-natural features—The canals as irrigation works of an intelligent race—A challenge to the thinking world—The canals as described and mapped by Mr. Lowell—The double canals—Dimensions of the canals—They cross the supposed seas—Circular black spots termed oases—An interesting volume.
CHAPTER III.
    No permanent water on Mars—Rarely any clouds and no rain—Snow-caps the only source of water—No mountains, hills, or valleys on Mars—Two-thirds of the surface a desert—Water from the snow-caps too scanty to supply the canals—Miss Clerke's views as to the water-supply—Description of some of the chief canals—Mr. Lowell on the purpose of the canals—Remarks on the same—Mr. Lowell on relation of canals to oases and snow-caps —Critical remarks on the same.
CHAPTER IV.
    Water and air essential for animal life—Atmosphere of Mars assumed to be like ours—Blue tint near melting snow the only evidence of water—Fallacy of this argument—Dr. Johnstone Stoney's proof that water-vapour cannot exist on Mars—Spectroscope gives no evidence of water.
CHAPTER V.
    Problem of terrestrial temperature—Ice under recent lava—Tropical oceans ice-cold at bottom—Earth's surface-heat all from the sun—Absolute zero of temperature—Complex problem of planetary temperatures​—Mr. Lowell's investigation of the problem—Abstract of Mr. Lowell's paper—Critical remarks on Mr. Lowell's paper.
CHAPTER VI.
    Langley's determination of lunar heat—Rapid loss of heat by radiation on the earth—Rapid loss of heat on moon daring eclipse —Sir George Darwin's theory of the moon's origin—Very's researches on the moon's temperature—Application of these results to the case of Mars—Cause of great difference of temperatures of earth and moon—Special features of Mars influencing its temperature—Further criticism of Mr. Lowell's article—Very low temperature of arctic regions on Mars.
CHAPTER VII.
    Special features of the canals—Mr. Pickering's suggested explanation—The meteoritic hypotheses of origin of planets—Probable mode of origin of Mars—Structural straight lines on the earth—Probable origin of the surface-features of Mars—Symmetry of basaltic columns—How this applies to Mars—Suggested explanation of the oases—Probable function of the great fissures—Suggested origin of blue patches adjacent to snow-caps—The double canals—Concluding remarks on the canals.
CHAPTER VIII.
    The canals the origin of Mr. Lowell's theory—Best explained as natural features—Evaporation difficulty not met by Mr. Lowell—How did Martians live without the canals—Radiation due to scanty atmosphere not taken account of—Three independent proofs of low temperature and uninhabitability of Mars—Conclusion.
[Advertisements]
Mars and its Canals
By PERCIVAL LOWELL
Illustrated, 8vo. 10s. 6d. net.
JOURNAL OF THE BRITISH ASTRONOMICAL ASSOCIATION.—"Probably most readers of this book will take it up with a strong disbelief in the sensational theory of Mars, which has now for some years past been associated with Mr. Lowell's name. A perusal of its pages, however, should at least convince them that Mr. Lowell is no mere faddist, but a scientific observer, whose researches are entitled to the greatest respect. He has undoubtedly done much to advance our knowledge of Martian phenomena, and therefore, while wisely hesitating to accept too readily all his conclusions, his work should be welcomed as a notable and valuable contribution to our study of the planet."
TRIBUNE.—"Mr. Lowell sums up the result of his investigations in a manner admirably adapted to the needs of the interested layman—and surely there are few questions more interesting than this of the existence of another world, quasi-human, in our immediate neighbourhood. . . . His results and conclusions are the outcome of a seldom-surpassed skill in observing and of a lifelong devotion to one great subject. . . . Those who read Mr. Lowell's book without prejudice will admit that up to the present no other explanation of the Martian canals has been offered which can for a moment compare with it."
TIMES.—"Mr. Lowell has certainly produced a mass of evidence of a most striking and interesting kind. . . . There are many beautiful illustrations in the book, which should be welcomed by more than one class of readers."
ATHENÆUM.—"We heartily recommend our readers to procure the present book, study it for themselves, and draw their own conclusions."
DAILY MAIL.—"Its extraordinary interest and fascination hold the reader spellbound. Beyond all dispute it is the most striking astronomical work published for twenty years, and it possesses the rare merit of being written by an acknowledged expert in a popular style, with little technicality, so that it can be comprehended of every intelligent reader."
MACMILLAN AND CO. LTD., LONDON.
This work was published before January 1, 1929, and is in the public domain worldwide because the author died at least 100 years ago.
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