From the Earth to the Moon

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Book by Jules Verne - From the Earth to the Moon, page 46

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depression which would probably have given access to the interior
of the crater.

In passing over the surrounding plains, Barbicane noticed a
great number of less important mountains; and among others a
little ringed one called Guy Lussac, the breadth of which
measured twelve miles.

Toward the south, the plain was very flat, without one
elevation, without one projection. Toward the north, on the
contrary, till where it was bounded by the "Sea of Storms," it
resembled a liquid surface agitated by a storm, of which the
hills and hollows formed a succession of waves suddenly congealed.
Over the whole of this, and in all directions, lay the luminous
lines, all converging to the summit of Copernicus.

The travelers discussed the origin of these strange rays; but they
could not determine their nature any more than terrestrial observers.

"But why," said Nicholl, "should not these rays be simply spurs
of mountains which reflect more vividly the light of the sun?"

"No," replied Barbicane; "if it was so, under certain conditions
of the moon, these ridges would cast shadows, and they do not
cast any."

And indeed, these rays only appeared when the orb of day was in
opposition to the moon, and disappeared as soon as its rays
became oblique.

"But how have they endeavored to explain these lines of light?"
asked Michel; "for I cannot believe that savants would ever be
stranded for want of an explanation."

"Yes," replied Barbicane; "Herschel has put forward an opinion,
but he did not venture to affirm it."

"Never mind. What was the opinion?"

"He thought that these rays might be streams of cooled lava
which shone when the sun beat straight upon them. It may be so;
but nothing can be less certain. Besides, if we pass nearer to
Tycho, we shall be in a better position to find out the cause of
this radiation."

"Do you know, my friends, what that plain, seen from the height
we are at, resembles?" said Michel.

"No," replied Nicholl.

"Very well; with all those pieces of lava lengthened like rockets,
it resembles an immense game of spelikans thrown pellmell.
There wants but the hook to pull them out one by one."

"Do be serious," said Barbicane.

"Well, let us be serious," replied Michel quietly; "and instead
of spelikans, let us put bones. This plain, would then be
nothing but an immense cemetery, on which would repose the
mortal remains of thousands of extinct generations. Do you
prefer that high-flown comparison?"

"One is as good as the other," retorted Barbicane.

"My word, you are difficult to please," answered Michel.

"My worthy friend," continued the matter-of-fact Barbicane, "it
matters but little what it _resembles_, when we do not know what
it _is_."

"Well answered," exclaimed Michel. "That will teach me to
reason with savants."

But the projectile continued to advance with almost uniform
speed around the lunar disc. The travelers, we may easily
imagine, did not dream of taking a moment's rest. Every minute
changed the landscape which fled from beneath their gaze.
About half past one o'clock in the morning, they caught a glimpse
of the tops of another mountain. Barbicane, consulting his map,
recognized Eratosthenes.

It was a ringed mountain nine thousand feet high, and one of
those circles so numerous on this satellite. With regard to
this, Barbicane related Kepler's singular opinion on the
formation of circles. According to that celebrated
mathematician, these crater-like cavities had been dug by the
hand of man.

"For what purpose?" asked Nicholl.

"For a very natural one," replied Barbicane. "The Selenites
might have undertaken these immense works and dug these enormous
holes for a refuge and shield from the solar rays which beat
upon them during fifteen consecutive days."

"The Selenites are not fools," said Michel.

"A singular idea," replied Nicholl; "but it is probable that
Kepler did not know the true dimensions of these circles, for
the digging of them would have been the work of giants quite
impossible for the Selenites."

"Why? if weight on the moon's surface is six times less than on
the earth?" said Michel.

"But if the Selenites are six times smaller?" retorted Nicholl.

"And if there are _no_ Selenites?" added Barbicane.

This put an end to the discussion.

Soon Eratosthenes disappeared under the horizon without the
projectile being sufficiently near to allow close observation.
This mountain separated the Apennines from the Carpathians. In the
lunar orography they have discerned some chains of mountains, which
are chiefly distributed over the northern hemisphere. Some, however,
occupy certain portions of the southern hemisphere also.

About two o'clock in the morning Barbicane found that they were
above the twentieth lunar parallel. The distance of the
projectile from the moon was not more than six hundred miles.
Barbicane, now perceiving that the projectile was steadily
approaching the lunar disc, did not despair; if not of reaching
her, at least of discovering the secrets of her configuration.





CHAPTER XIII


LUNAR LANDSCAPES


At half-past two in the morning, the projectile was over the
thirteenth lunar parallel and at the effective distance of five
hundred miles, reduced by the glasses to five. It still seemed
impossible, however, that it could ever touch any part of the disc.
Its motive speed, comparatively so moderate, was inexplicable to
President Barbicane. At that distance from the moon it must have
been considerable, to enable it to bear up against her attraction.
Here was a phenomenon the cause of which escaped them again.
Besides, time failed them to investigate the cause. All lunar
relief was defiling under the eyes of the travelers, and they
would not lose a single detail.

Under the glasses the disc appeared at the distance of five
miles. What would an aeronaut, borne to this distance from the
earth, distinguish on its surface? We cannot say, since the
greatest ascension has not been more than 25,000 feet.

This, however, is an exact description of what Barbicane and his
companions saw at this height. Large patches of different
colors appeared on the disc. Selenographers are not agreed upon
the nature of these colors. There are several, and rather
vividly marked. Julius Schmidt pretends that, if the
terrestrial oceans were dried up, a Selenite observer could not
distinguish on the globe a greater diversity of shades between
the oceans and the continental plains than those on the moon
present to a terrestrial observer. According to him, the color
common to the vast plains known by the name of "seas" is a dark
gray mixed with green and brown. Some of the large craters
present the same appearance. Barbicane knew this opinion of the
German selenographer, an opinion shared by Boeer and Moedler.
Observation has proved that right was on their side, and not on
that of some astronomers who admit the existence of only gray on
the moon's surface. In some parts green was very distinct, such
as springs, according to Julius Schmidt, from the seas of
"Serenity and Humors." Barbicane also noticed large craters,
without any interior cones, which shed a bluish tint similar to
the reflection of a sheet of steel freshly polished. These colors
belonged really to the lunar disc, and did not result, as some
astronomers say, either from the imperfection in the objective
of the glasses or from the interposition of the terrestrial atmosphere.

Not a doubt existed in Barbicane's mind with regard to it, as he
observed it through space, and so could not commit any optical error.
He considered the establishment of this fact as an acquisition
to science. Now, were these shades of green, belonging to
tropical vegetation, kept up by a low dense atmosphere? He could
not yet say.

Farther on, he noticed a reddish tint, quite defined. The same
shade had before been observed at the bottom of an isolated
enclosure, known by the name of Lichtenburg's circle, which is
situated near the Hercynian mountains, on the borders of the
moon; but they could not tell the nature of it.

They were not more fortunate with regard to another peculiarity
of the disc, for they could not decide upon the cause of it.

Michel Ardan was watching near the president, when he noticed
long white lines, vividly lighted up by the direct rays of the sun.
It was a succession of luminous furrows, very different from the
radiation of Copernicus not long before; they ran parallel with
each other.

Michel, with his usual readiness, hastened to exclaim:


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