The music of the spheres : $b A nature lover's astronomyGrondal, Florence Armstrong
Science
The music of the spheres : $b A nature lover's astronomy
Grondal, Florence Armstrong
Astronomy
A crater only six miles in diameter may be easily seen in a small
telescope, although there are thousands less than a mile in diameter
which may be seen in a large telescope. Craters from 16 miles to 60
miles in diameter are common and a few even measure as much as 100 to
150 miles. These craters have deeply sunken floors and are usually
surrounded by gigantic mountain walls which rise like a fringe of rock
above the general level of the region outside. Near the center of many
of the craters with the largest brims, one and sometimes two or three
sharp-peaked mountains tower, casting a long, weird shadow over the
crater's floor. The surrounding brim is almost invariably higher than
the central mountain, yet many of these central mountains are a mile or
so high.
Probably the deepest of the moon's craters is _Theophilus_, on the edge
of the circular "sea" Mare Nectaris, and it is best seen while the moon
is still a slender crescent. The encircling walls of this crater rise
from 14,000 to 18,000 feet above its floor, the floor itself being
10,000 feet below the general level of the moon outside the wall. The
walls of this amazing cavity, in the main, slope gently to the outer
plain but rise very steeply from the depths of the inner floor which
measures 64 miles across. Three lofty cone-shaped mountains rest in the
center of this floor, their sharp, black shadows stretching to the left.
One of these mountains rises 6000 feet, yet its summit is some 4000 feet
lower than the level of the outside plain! Imagine standing on the rim
of Theophilus and watching the darkness flow into its huge bowl until
the mountain peaks in the center look like sunny isles in a dense, black
sea! This is a _real_ crater, for the word "crater" means "cup."
Most of the large craters on the moon, however, are not so "cup-like,"
but, to pursue the simile still farther, are more like platters and
saucers and individual butter plates, for their diameters range from
five times to more than fifty times their depth.
[Figure 164: THE LUNAR CRATER COPERNICUS, FIFTY MILES IN DIAMETER.
Photograph by Mount Wilson Observatory through the 100-inch
Hooker telescope.]
Chacornac mentions a walled-plain called _Schickard_, on the southeast
portion of the moon, which is 134 miles in breadth, and, although
encircled by a mountain wall which in one place is nearly 10,000 feet
high, a spectator centrally located on the floor of the crater would
think himself on a boundless desert, for this encircling wall, due to
the curvature of the surface of the moon, would lie entirely beneath his
horizon.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account