The sidereal messenger of Galileo Galilei : $b and a part of the preface to Kepler's Dioptrics containing the original account of Galileo's astronomical discoveries — John Shaqi
The sidereal messenger of Galileo Galilei : $b and a part of the preface to Kepler's Dioptrics containing the original account of Galileo's astronomical discoveriesGalilei, Galileo
History
The sidereal messenger of Galileo Galilei : $b and a part of the preface to Kepler's Dioptrics containing the original account of Galileo's astronomical discoveries
Galilei, Galileo
Astronomy -- Early works to 1800; Jupiter (Planet) -- Satellites
I think that it has been sufficiently made clear, from the explanation
of phenomena which have been given, that the brighter part of the
Moon’s surface is dotted everywhere with protuberances and cavities;
it only remains for me to speak about their size, and to show that the
ruggednesses of the Earth’s surface are far smaller than those of the
Moon’s; smaller, I mean, absolutely, so to say, and not only smaller
in proportion to the size of the orbs on which they are. And this is
plainly shown thus:—As I often observed in various positions of the
Moon with reference to the Sun, that some summits within the portion
of the Moon in shadow appeared illumined, although at some distance
from the boundary of the light (the terminator), by comparing their
distance with the complete diameter of the Moon, I learnt that it
sometimes exceeded the one-twentieth (1/20th) part of the diameter.
Suppose the distance to be exactly 1/20th part of the diameter, and
let the diagram represent the Moon’s orb, of which C A F is a great
circle, E its centre, and C F a diameter, which consequently bears
to the diameter of the Earth the ratio 2:7; and since the diameter
of the Earth, according to the most exact observations, contains
7000 Italian miles, C F will be 2000, and C E 1000, and the 1/20th
part of the whole, C F, 100 miles. Also let C F be a diameter of the
great circle which divides the bright part of the Moon from the dark
part (for, owing to the very great distance of the Sun from the Moon
this circle does not differ sensibly from a great one), and let the
distance of A from the point C be 1/20th part of that diameter; let
the radius E A be drawn, and let it be produced to cut the tangent
line G C D, which represents the ray that illumines the summit, in
the point D. Then the arc C A or the straight line C D will be 100 of
such units, as C E contains 1000. The sum of the squares of D C, C E is
therefore 1,010,000, and the square of D E is equal to this; therefore
the whole E D will be more than 1004; and A D will be more than 4 of
such units, as C E contained 1000. Therefore the height of A D in the
Moon, which represents a summit reaching up to the Sun’s ray, G C D,
and separated from the extremity C by the distance C D, is more than
4 Italian miles; but in the Earth there are no mountains which reach
to the perpendicular height even of one mile. We are therefore left to
conclude that it is clear that the prominences of the Moon are loftier
than those of the Earth.
[Sidenote: The faint illumination of the Moon’s disc about new-moon
explained to be due to earth-light.]
Public-domain text, read in full here on John Shaqi.
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