The Moon: A Popular TreatiseServiss, Garrett Putman
Science
The Moon: A Popular Treatise
Serviss, Garrett Putman
Moon
“This is the reason,” I continued, “why the march of day across the
moon, always keeping sharp on the heels of night, is a spectacle so
imposing and unparalleled. It is this wonderful march that we are going
to follow with the aid of the photographs. I shall now ask you to give
your attention to photograph No. 3. It was made more than a day and a
half later than the others, measured by the age of the moon, which, in
this case, was about five days and a half. You notice how in the
interval the sunlight has swept eastward over the moon’s surface. The
_Mare Crisium_ is recognizable in the lowest or most northerly, of three
large, dark plains. The small white oval a considerable distance above
it is our old acquaintance Langrenus, whose floor and walls are now very
brilliant in the full sunshine, which falls upon them at a high angle.
Vendelinus and Petavius are less conspicuous. The broad, dark plain
which has come into view eastward from Langrenus is the _Mare
Fœcunditatis_, which we may translate ‘Sea of Fecundity’! You certainly
cannot aver that on this occasion the invention of the old astronomers
failed in the matter of romantic suggestiveness. The name calls up
pictures of a great body of tranquil water, fanned by gentle,
stimulating breezes, filled with fish of every variety, dotted with
vine- and flower-garlanded islets, and bordered by well-watered shores,
rich with vegetation, and supporting a numerous and happy population.
Some such idea of the _Mare Fœcunditatis_ may have been in the minds of
its sponsors a couple of centuries ago. But telescopes have become too
powerful in our day to permit us to be any longer deceived as to the
actual nature of this singular lunar region. Like the _Mare Crisium_, it
may have been the bed of a sea many years ago, but at the present time
it contains no water, and its shores present an endless succession of
fire-scarred cliffs, peaks, and volcanoes. The only ‘islands’ in it are
extinct craters.”
“But,” said my companion, smiling, “where then is its history?”
“Ah!” I replied, “is not this old sea itself history enough? When it has
receded sufficiently into the past, all history loses its details, and
presents only its setting and its grand primary elements. Suppose that,
some ages in the future, you should be an inhabitant of a distant
planet, surveying with a telescope the dried-up basin of the Atlantic
Ocean. Provided only that you were convinced, in your own mind, that it
had once been an ocean, with fertile, inhabited shores, and with ships
sailing upon it, you would be singularly lacking in imagination if you
could not reconstruct its history for yourself. The details could safely
be left to your invention and you could change them from time to time to
suit your varying moods. Terrestrial historians have sometimes done
that.”
[Illustration:
NO. 3. JULY 29, 1903; MOON’S AGE 5.54 DAYS.
]
“But do _you_ believe that the _Mare Fœcunditatis_ was ever such a sea,
and the scene of such events?”
Public-domain text, read in full here on John Shaqi.
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