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
JULIUS CAESAR.--A large incomplete formation of irregular shape. The wall
on the E. is much terraced, and forms a flat "S" curve. The summit ridge
is especially bright, and has a conspicuous little crater upon it. On
the W. is a number of narrow longitudinal valleys trending from N. to S.,
included by a wide valley which constitutes the boundary on this side.
The border on the S. consists of a number of low rounded banks, those
immediately E. of Sosigenes being traversed by several shallow valleys,
which look as if they had been shaped by alluvial action. There is a
brilliant little hill at the end of one of these valleys, a few miles E.
of Sosigenes. The floor of Julius Caesar is uneven in tone, becoming
gradually duskier from S. to N., the northern end ranking among the
darkest areas on the lunar surface. There are at least three large
circular swellings in the interior. A long low mound, with two or three
depressions upon it, bounds the wide valley on the E. side.
GODIN.--A square-shaped ring-plain, 28 miles in diameter, with rounded
corners. The bright rampart is everywhere lofty, except on the S., is
much terraced, and includes a central mountain. On the S. a curious
trumpet-shaped valley, extending some distance towards the S.W., and
bounded by bright walls, is a noteworthy feature at sunrise. There are
other longitudinal valleys with associated ridges on this side of the
formation, all running in the same direction. There is a large bright
crater outside the border on the N.E., and, between it and the wall,
another, smaller, which is readily seen under a high sun.
AGRIPPA.--A ring-plain 28 miles in diameter on the N. of the last, with a
terraced border rising to a height of between 7000 and 8000 feet above
the floor, which contains a large bright central mountain and two craters
on the S. The shape of this formation deviates very considerably from
circularity, the N. wall, on which stands a small crater, being almost
lineal. On the W., at a distance of a few miles, runs the prominent
mountain range, extending northwards nearly up to the E. flank of Julius
Caesar, which bounds the E. side of the great Ariadaeus plain. Between
this rocky barrier and Agrippa is a very noteworthy enclosure containing
much minute detail and a long straight ridge resembling a cleft. A few
miles N. of Agrippa stands a small crater; at a point W. of which the
Hyginus cleft originates.
SILBERSCHLAG.--A very brilliant crater, 8 or 9 miles in diameter,
connected with the great mountain range just referred to. The Ariadaeus
cleft cuts through the range a few miles N. of it. This neighbourhood at
sunrise presents a grand spectacle. With high powers under good
atmospheric conditions, the plain E. of the mountains is seen to be
traversed by a number of shallow winding valleys, trending towards
Agrippa, and separated by low rounded hills which have all the appearance
of having been moulded by the action of water.
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