The Moon: A Popular TreatiseServiss, Garrett Putman
Science
The Moon: A Popular Treatise
Serviss, Garrett Putman
Moon
Accordingly, after a few minutes, I presented to her these two diagrams,
remarking that it should be borne in mind that the two sketches were not
made on the same relative scale. “I was compelled,” I said, “to change
the true proportions in the section of the lunar volcano, for if I had
drawn them as they are in fact, the width of the basin would have been
enormous in proportion to its depth. You will recall that I told you
that such rings as Albategnius and Maurolycus are a hundred miles and
even more in diameter, while their depth does not exceed two or three
miles. It results from this necessary falsification of proportions in
the sketch that the terrestrial volcano, although so widely different in
form, appears comparable in magnitude with the lunar one. But the fact
is that you could take a dozen of the largest volcanic mountains on the
earth and throw them into one of the great lunar rings without filling
it.”
“I am the more astonished by what you say,” remarked my friend, “because
you have already told me that the moon is so much smaller than the
earth. How does it happen, then, that her volcanoes are so much larger?
I should think that in a little world all things would be small in
proportion.”
“It is quite natural to think so,” I replied, “until you reflect upon
the consequences of the smaller force of gravitation on a small world. I
told you last evening that gravitation on the moon, is only one sixth as
powerful as it is on the earth, and you will recall that one consequence
which I pointed out was that you would weigh only twenty pounds if you
were on the moon. Since the same reasoning applies to all objects in the
lunar world, it is clear that a similar force exerted there would be
able to produce enormously greater effects, as for instance in the
formation of vast hollows or depressions, by violent explosions, the
products of which would be thrown to immense distances. Some
selenographers, which is a term applied to those who study the features
of the lunar world, have suggested that in this cause alone is to be
found the explanation of the giant lunar ring mountains. At some remote
period of the past, according to them, the volcanic forces of the moon
reached a maximum of activity and energy. The lava, cinders, ashes, and
other products of ejection, were hurled to a height of scores of miles,
and when this fell back at a great distance from the centers of eruption
these were piled up in huge rings, fifty, eighty, or a hundred miles in
diameter, while the surface of the moon within the rings sank in
consequence of the withdrawal of the material thus ejected. To account
for the existence of the central mountains so often found in the middle
of the rings, it has been suggested that at a much later period, when
the volcanic energy had become comparatively insignificant, as a result
of the cooling of the interior of the moon, less violent explosions, not
greater than many that have occurred on the earth, took place, and by
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