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The sidereal messenger of Galileo Galilei

Galileo Galilei · 1610 (composed as a short astronomical pamphlet; observations and initial report from early 1610) primary

passage 11 of 48 · (11/47)

↪ you wandered here via “lunar craters crust collapse” — the connecting lines are tinted below

in brief
Galileo describes a large, perfectly round lunar cavity in the Moon’s middle, explaining how its light-and-shadow behavior proves the Moon’s bright region is rugged and uneven.

[8] Specimens of frosted or crackled Venetian glass are to be seen in the Slade Collection, British Museum, and fully justify Galileo’s comparison.

[Sidenote: Description of a lunar crater, perhaps Tycho.][9]

[9] Webb, Celestial Objects for Common Telescopes, p. 104, suggests this identification.

There is one other point which I must on no account forget, which I have noticed and rather wondered at. It is this:—The middle of the Moon, as it seems, is occupied by a certain cavity larger than all the rest, and in shape perfectly round. I have looked at this depression near both the first and third quarters, and I have represented it as well as I can in the second illustration already given. It produces the same appearance as to effects of light and shade as a tract like Bohemia would produce on the Earth, if it were shut in on all sides by very lofty mountains arranged on the circumference of a perfect circle; for the tract in the Moon is walled in with peaks of such enormous height that the furthest side adjacent to the dark portion of the Moon is seen bathed in sunlight before the boundary between light and shade reaches half-way across the circular space. But according to the characteristic property of the rest of the spots, the shaded portion of this too faces the Sun, and the bright part is towards the dark side of the Moon, which for the third time I advise to be carefully noticed as a most solid proof of the ruggednesses and unevennesses spread over the whole of the bright region of the Moon. Of these spots, moreover, the darkest are always those which are near to the boundary-line between the light and the shadow, but those further off appear both smaller in size and less decidedly dark; so that at length, when the Moon at opposition becomes full, the darkness of the cavities differs from the brightness of the prominences with a subdued and very slight difference.

[Sidenote: Reasons for believing that there is a difference of constitution in various parts of the Moon’s surface.]

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topics: experiment, observation, and evidence · perception and the senses · the earth and its formation

The sidereal messenger of Galileo Galilei · Galileo Galilei · 1610