From the Earth to the Moon by Verne, Jules

particular facts; Barbicane and Nicholl always serious, Michel

Ardan always enthusiastic. The projectile, its situation,

its direction, incidents which might happen, the precautions

necessitated by their fall on to the moon, were inexhaustible

matters of conjecture.

As they were breakfasting, a question of Michel’s, relating to

the projectile, provoked rather a curious answer from Barbicane,

which is worth repeating. Michel, supposing it to be roughly

stopped, while still under its formidable initial speed, wished

to know what the consequences of the stoppage would have been.

“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 space.”

“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 Uranus 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 masses 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

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