The moon : $b a full description and map of its principal physical featuresElger, Thomas Gwyn
Science
The moon : $b a full description and map of its principal physical features
Elger, Thomas Gwyn
Moon
COPERNICUS.--This is without question the grandest object, not only on
the second Quadrant, but on the whole visible superficies of the moon. It
undoubtedly owes its supremacy partly to its comparative isolation on the
surface of a vast plain, where there are no neighbouring formations to
vie with it in size and magnificence, but partly also to its favourable
position, which is such, that, though not central, is sufficiently
removed from the limb to allow all its manifold details to be critically
examined without much foreshortening. There are some other formations,
Langrenus and Petavius, for example, which, if they were equally well
situated, would probably be fully as striking; but, as we see it
Copernicus is _par excellence_ the monarch of the lunar ring-mountains.
Schmidt remarks that this incomparable object combines nearly all the
characteristics of the other ring-plains, and that careful study directed
to its unequalled beauties and magnificent form is of much more value
than that devoted to a hundred other objects of the same class. It is
fully 56 miles in diameter, and, though generally described as nearly
circular, exhibits very distinctly under high powers a polygonal outline,
approximating very closely to an equilateral hexagon. There are, however,
two sections of the crest of the border on the N.E. which are inflected
slightly towards the centre, a peculiarity already noticed in the case of
Eratosthenes. The walls, tolerably uniform in height, are surmounted by a
great number of peaks, one of which on the W., according to Neison,
stands 11,000 feet above the floor, and a second on the opposite side is
nearly as high. Both the inner and outer slopes of this gigantic rampart
are very broad, each being fully 10 miles in width. The outer slope,
especially on the E., is a fine object at sunrise, when its rugged
surface, traversed by deep gullies, is seen to the best advantage. The
terraces and other features on the bright inner declivities on this side
may be well observed when the sun's altitude is about 6 deg. Schmidt,
whose measures differ from those of Neison, estimates the height of the
wall on the E. to be 12,000 feet, and states that the interior slopes
vary from 60 deg. to 50 deg. above, to from 10 deg. to 2 deg. at the
base. The first inclination of 50 deg., and in some cases of 60 deg., is
confined to the loftiest steep crests and to the flanks of the terraces.
There are apparently five bright little mountains on the floor, the most
easterly being rather the largest, and a great number of minute hillocks
on the S.E. quarter. S.W. of the centre is a little crater, and on the
same side of the interior a curious hook-shaped ridge, projecting from
the foot of the wall, and extending nearly halfway across the floor. The
region surrounding Copernicus is one of the most remarkable on the moon,
being everywhere traversed by low ridges, enclosing irregular areas,
Public-domain text, read in full here on John Shaqi.
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