The Worlds of Robert A. Heinlein

equations until I’ve dreamed about them.” He turned to Lentz. “Do you

agree, Doctor?”

Lentz nodded slowly. “I believe so . . . Yes, I think I may say so.”

Harrington should have been pleased; he wasn’t. “I had hoped you could tell

me I was wrong,” he said, almost petulantly, “but I’m afraid there is no

further doubt about it. Dr. Destry included an assumption valid in molar

physics, but for which we have absolutely no assurance in atomic physics. I

suppose you realize what this means to you, Dr. King?”

King’s voice was dry whisper. “Yes,” he said, “yes — It means that if that

bomb out there ever blows up, we must assume that it will go up all at

once, rather than the way Destry predicted — and God help the human race!”

Captain Harrington cleared his throat to break the silence that followed.

“Superintendent,” he said, “I would not have ventured to call had it been

simply a matter of disagreement as to interpretation of theoretical

predictions — ”

“You have something more to go on?”

“Yes and no. Probably you gentlemen think of the Naval Observatory as being

exclusively preoccupied with ephemerides and tide tables. In a way you

would be right — but we still have some time to devote to research as long

as it doesn’t cut into the appropriation. My special interest has always

been lunar theory.

“I don’t mean lunar ballistics,” he continued. “I mean the much more

interesting problem of its origin and history, the problem the younger

Darwin struggled with, as well as my illustrious predecessor, Captain

T.J.J. See. I think that it is obvious that any theory of lunar origin and

history must take into account the surface features of the Moon —

especially the mountains, the craters, that mark its face so prominently.”

He paused momentarily, and Superintendent King put in: “Just a minute,

Captain — I may be stupid, or perhaps I missed something, but — is there a

connection between what we were discussing before and lunar theory?”

“Bear with me for a few moments, Dr. King,” Harrington apologized. “There

is a connection — at least, I’m afraid there is a connection — but I would

rather present my points in their proper order before making my

conclusions.” They granted him an alert silence; he went on:

“Although we are in the habit of referring to the craters of the Moon, we

know they are not volcanic craters. Superficially, they follow none of the

rules of terrestrial volcanoes in appearance or distribution, but when

Rutter came out in 1952 with his monograph on the dynamics of vulcanology,

he proved rather conclusively that the lunar craters could not be caused by

anything that we know as volcanic action.

“That left the bombardment theory as the simplest hypothesis. It looks

good, on the face of it, and a few minutes spent throwing pebbles into a

patch of mud will convince anyone that the lunar craters could have been

formed by falling meteors.

“But there are difficulties. If the Moon was struck so repeatedly, why not

the Earth? It hardly seems necessary to mention that the Earth’s atmosphere

would be no protection against masses big enough to form craters like

Endymion or Plato. And if they fell after the Moon was a dead world while

the Earth was still young enough to change its face and erase the marks of

bombardment, why did the meteors avoid so nearly completely the great dry

basins we call lunar seas?

“I want to cut this short; you’ll find the data and the mathematical

investigations from the data here in my notes. There is one other major

objection to the meteor-bombardment theory: the great rays that spread from

Tycho across almost the entire surface of the Moon. It makes the Moon look

like a crystal ball that had been struck with a hammer, and impact from

outside seems evident, but there are difficulties. The striking mass, our

hypothetical meteor, must be small enough to have formed the crater of

Tycho, but it must have the mass and speed to crack an entire planet.

“Work it out for yourself — you must either postulate a chunk out of the

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