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Round the Moon, A
Chapter XII - Orographic Details
Jules Verne
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       Chapter XII - Orographic Details
       The course taken by the projectile, as we have before remarked, was
       bearing it toward the moon's northern hemisphere. The travelers
       were far from the central point which they would have struck,
       had their course not been subject to an irremediable deviation.
       It was past midnight; and Barbicane then estimated the distance
       at seven hundred and fifty miles, which was a little greater than
       the length of the lunar radius, and which would diminish as it
       advanced nearer to the North Pole. The projectile was then not
       at the altitude of the equator; but across the tenth parallel,
       and from that latitude, carefully taken on the map to the pole,
       Barbicane and his two companions were able to observe the moon
       under the most favorable conditions. Indeed, by means of glasses,
       the above-named distance was reduced to little more than
       fourteen miles. The telescope of the Rocky Mountains brought
       the moon much nearer; but the terrestrial atmosphere singularly
       lessened its power. Thus Barbicane, posted in his projectile,
       with the glasses to his eyes, could seize upon details which were
       almost imperceptible to earthly observers.
       "My friends," said the president, in a serious voice, "I do not
       know whither we are going; I do not know if we shall ever see
       the terrestrial globe again. Nevertheless, let us proceed as if
       our work would one day by useful to our fellow-men. Let us keep
       our minds free from every other consideration. We are
       astronomers; and this projectile is a room in the Cambridge
       University, carried into space. Let us make our observations!"
       This said, work was begun with great exactness; and they
       faithfully reproduced the different aspects of the moon,
       at the different distances which the projectile reached.
       At the time that the projectile was as high as the tenth
       parallel, north latitude, it seemed rigidly to follow the
       twentieth degree, east longitude. We must here make one
       important remark with regard to the map by which they were
       taking observations. In the selenographical maps where, on
       account of the reversing of the objects by the glasses, the
       south is above and the north below, it would seem natural that,
       on account of that inversion, the east should be to the left
       hand, and the west to the right. But it is not so. If the map
       were turned upside down, showing the moon as we see her, the
       east would be to the left, and the west to the right, contrary
       to that which exists on terrestrial maps. The following is the
       reason of this anomaly. Observers in the northern hemisphere
       (say in Europe) see the moon in the south-- according to them.
       When they take observations, they turn their backs to the north,
       the reverse position to that which they occupy when they study
       a terrestrial map. As they turn their backs to the north, the
       east is on their left, and the west to their right. To observers
       in the southern hemisphere (Patagonia for example), the moon's
       west would be quite to their left, and the east to their right,
       as the south is behind them. Such is the reason of the apparent
       reversing of these two cardinal points, and we must bear it in mind
       in order to be able to follow President Barbicane's observations.
       With the help of Boeer and Moedler's _Mappa Selenographica_,
       the travelers were able at once to recognize that portion
       of the disc enclosed within the field of their glasses.
       "What are we looking at, at this moment?" asked Michel.
       "At the northern part of the `Sea of Clouds,'" answered Barbicane.
       "We are too far off to recognize its nature. Are these plains
       composed of arid sand, as the first astronomer maintained?
       Or are they nothing but immense forests, according to M. Warren
       de la Rue's opinion, who gives the moon an atmosphere, though
       a very low and a very dense one? That we shall know by and by.
       We must affirm nothing until we are in a position to do so."
       This "Sea of Clouds" is rather doubtfully marked out upon the maps.
       It is supposed that these vast plains are strewn with blocks of
       lava from the neighboring volcanoes on its right, Ptolemy,
       Purbach, Arzachel. But the projectile was advancing, and sensibly
       nearing it. Soon there appeared the heights which bound this sea
       at this northern limit. Before them rose a mountain radiant with
       beauty, the top of which seemed lost in an eruption of solar rays.
       "That is--?" asked Michel.
       "Copernicus," replied Barbicane.
       "Let us see Copernicus."
       This mount, situated in 9@ north latitude and 20@ east
       longitude, rose to a height of 10,600 feet above the surface of
       the moon. It is quite visible from the earth; and astronomers
       can study it with ease, particularly during the phase between
       the last quarter and the new moon, because then the shadows are
       thrown lengthways from east to west, allowing them to measure
       the heights.
       This Copernicus forms the most important of the radiating
       system, situated in the southern hemisphere, according to Tycho
       Brahe. It rises isolated like a gigantic lighthouse on that
       portion of the "Sea of Clouds," which is bounded by the "Sea of
       Tempests," thus lighting by its splendid rays two oceans at
       a time. It was a sight without an equal, those long luminous
       trains, so dazzling in the full moon, and which, passing the
       boundary chain on the north, extends to the "Sea of Rains."
       At one o'clock of the terrestrial morning, the projectile,
       like a balloon borne into space, overlooked the top of this
       superb mount. Barbicane could recognize perfectly its
       chief features. Copernicus is comprised in the series of
       ringed mountains of the first order, in the division of
       great circles. Like Kepler and Aristarchus, which overlook
       the "Ocean of Tempests," sometimes it appeared like a brilliant
       point through the cloudy light, and was taken for a volcano
       in activity. But it is only an extinct one-- like all on that
       side of the moon. Its circumference showed a diameter of about
       twenty-two leagues. The glasses discovered traces of
       stratification produced by successive eruptions, and the
       neighborhood was strewn with volcanic remains which still choked
       some of the craters.
       "There exist," said Barbicane, "several kinds of circles on the
       surface of the moon, and it is easy to see that Copernicus
       belongs to the radiating class. If we were nearer, we should
       see the cones bristling on the inside, which in former times
       were so many fiery mouths. A curious arrangement, and one
       without an exception on the lunar disc, is that the interior
       surface of these circles is the reverse of the exterior, and
       contrary to the form taken by terrestrial craters. It follows,
       then, that the general curve of the bottom of these circles
       gives a sphere of a smaller diameter than that of the moon."
       "And why this peculiar disposition?" asked Nicholl.
       "We do not know," replied Barbicane.
       "What splendid radiation!" said Michel. "One could hardly see
       a finer spectacle, I think."
       "What would you say, then," replied Barbicane, "if chance should
       bear us toward the southern hemisphere?"
       "Well, I should say that it was still more beautiful," retorted
       Michel Ardan.
       At this moment the projectile hung perpendicularly over the circle.
       The circumference of Copernicus formed almost a perfect circle,
       and its steep escarpments were clearly defined. They could even
       distinguish a second ringed enclosure. Around spread a grayish
       plain, of a wild aspect, on which every relief was marked in yellow.
       At the bottom of the circle, as if enclosed in a jewel case,
       sparkled for one instant two or three eruptive cones, like enormous
       dazzling gems. Toward the north the escarpments were lowered by a
       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.
       Content of Chapter XII - Orographic Details [Jules Verne's novel: A trip around the Moon]
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