From the Earth to the Moon Part 33

"But," said Barbicane, "I do not see how it could have been stopped."

"But let us suppose so," said Michel.

"It is an impossible supposition," said the practical Barbicane; "unless that impulsive force had failed; but even then its speed would diminish by degrees, and it would not have stopped suddenly."

"Admit that it had struck a body in s.p.a.ce."

"What body?"

"Why that enormous meteor which we met."

"Then," said Nicholl, "the projectile would have been broken into a thousand pieces, and we with it."

"More than that," replied Barbicane; "we should have been burned to death."

"Burned?" exclaimed Michel, "by Jove! I am sorry it did not happen, `just to see.'"

"And you would have seen," replied Barbicane. "It is known now that heat is only a modification of motion. When water is warmed-- that is to say, when heat is added to it--its particles are set in motion."

"Well," said michel, "that is an ingenious theory!"

"And a true one, my worthy friend; for it explains every phenomenon of caloric. Heat is but the motion of atoms, a simple oscillation of the particles of a body. When they apply the brake to a train, the train comes to a stop; but what becomes of the motion which it had previously possessed? It is transformed into heat, and the brake becomes hot. Why do they grease the axles of the wheels? To prevent their heating, because this heat would be generated by the motion which is thus lost by transformation."

"Yes, I understand," replied Michel, "perfectly. For example, when I have run a long time, when I am swimming, when I am perspiring in large drops, why am I obliged to stop?

Simply because my motion is changed into heat."

Barbicane could not help smiling at Michel's reply; then, returning to his theory, said:

"Thus, in case of a shock, it would have been with our projectile as with a ball which falls in a burning state after having struck the metal plate; it is its motion which is turned into heat. Consequently I affirm that, if our projectile had struck the meteor, its speed thus suddenly checked would have raised a heat great enough to turn it into vapor instantaneously."

"Then," asked Nicholl, "what would happen if the earth's motion were to stop suddenly?"

"Her temperature would be raised to such a pitch," said Barbicane, "that she would be at once reduced to vapor."

"Well," said Michel, "that is a way of ending the earth which will greatly simplify things."

"And if the earth fell upon the sun?" asked Nicholl.

"According to calculation," replied Barbicane, "the fall would develop a heat equal to that produced by 16,000 globes of coal, each equal in bulk to our terrestrial globe."

"Good additional heat for the sun," replied Michel Ardan, "of which the inhabitants of Ura.n.u.s or Neptune would doubtless not complain; they must be perished with cold on their planets."

"Thus, my friends," said Barbicane, "all motion suddenly stopped produces heat. And this theory allows us to infer that the heat of the solar disc is fed by a hail of meteors falling incessantly on its surface. They have even calculated----"

"Oh, dear!" murmured Michel, "the figures are coming."

"They have even calculated," continued the imperturbable Barbicane, "that the shock of each meteor on the sun ought to produce a heat equal to that of 4,000 ma.s.ses of coal of an equal bulk."

"And what is the solar heat?" asked Michel.

"It is equal to that produced by the combustion of a stratum of coal surrounding the sun to a depth of forty-seven miles."

"And that heat----"

"Would be able to boil two billions nine hundred millions of cubic myriameters [2] of water."

[2] The myriameter is equal to rather more than 10,936 cubic yards English.

"And it does not roast us!" exclaimed Michel.

"No," replied Barbicane, "because the terrestrial atmosphere absorbs four-tenths of the solar heat; besides, the quant.i.ty of heat intercepted by the earth is but a billionth part of the entire radiation."

"I see that all is for the best," said Michel, "and that this atmosphere is a useful invention; for it not only allows us to breathe, but it prevents us from roasting."

"Yes!" said Nicholl, "unfortunately, it will not be the same in the moon."

"Bah!" said Michel, always hopeful. "If there are inhabitants, they must breathe. If there are no longer any, they must have left enough oxygen for three people, if only at the bottom of ravines, where its own weight will cause it to acc.u.mulate, and we will not climb the mountains; that is all." And Michel, rising, went to look at the lunar disc, which shone with intolerable brilliancy.

"By Jove!" said he, "it must be hot up there!"

"Without considering," replied Nicholl, "that the day lasts 360 hours!"

"And to compensate that," said Barbicane, "the nights have the same length; and as heat is restored by radiation, their temperature can only be that of the planetary s.p.a.ce."

"A pretty country, that!" exclaimed Michel. "Never mind!

I wish I was there! Ah! my dear comrades, it will be rather curious to have the earth for our moon, to see it rise on the horizon, to recognize the shape of its continents, and to say to oneself, `There is America, there is Europe;' then to follow it when it is about to lose itself in the sun's rays! By the bye, Barbicane, have the Selenites eclipses?"

"Yes, eclipses of the sun," replied Barbicane, "when the centers of the three orbs are on a line, the earth being in the middle.

But they are only partial, during which the earth, cast like a screen upon the solar disc, allows the greater portion to be seen."

"And why," asked Nicholl, "is there no total eclipse? Does not the cone of the shadow cast by the earth extend beyond the moon?"

"Yes, if we do not take into consideration the refraction produced by the terrestrial atmosphere. No, if we take that refraction into consideration. Thus let be the horizontal parallel, and _p_ the apparent semidiameter----"

"Oh!" said Michel. "Do speak plainly, you man of algebra!"

"Very well, replied Barbicane; "in popular language the mean distance from the moon to the earth being sixty terrestrial radii, the length of the cone of the shadow, on account of refraction, is reduced to less than forty-two radii.

The result is that when there are eclipses, the moon finds itself beyond the cone of pure shadow, and that the sun sends her its rays, not only from its edges, but also from its center."

"Then," said Michel, in a merry tone, "why are there eclipses, when there ought not to be any?"

"Simply because the solar rays are weakened by this refraction, and the atmosphere through which they pa.s.s extinguished the greater part of them!"

"That reason satisfies me," replied Michel. "Besides we shall see when we get there. Now, tell me, Barbicane, do you believe that the moon is an old comet?"

"There's an idea!"

"Yes," replied Michel, with an amiable swagger, "I have a few ideas of that sort."