"... the Moon, whose orb
The Tuscan artist views through optic glass
At evening from the top of Fesolé,
Or in Valdarno, to descry new lands,
Rivers or mountains in her spotty globe."—Paradise Lost.
The moon is probably the most interesting of all telescopic
objects. This arises from its comparative nearness
to the earth. A telescope magnifying 1,000 diameters
brings the moon within an apparent distance of
less than 240 miles. If telescopes are ever made with
a magnifying power of 10,000 diameters, then, provided
that atmospheric difficulties can be overcome, we shall
see the moon as if it were only about twenty miles off, and
a sensitive astronomer might be imagined to feel a little
hesitation about gazing so closely at the moon—as if he
were peering into a neighbor world's window.
But a great telescope and a high magnifying power are
not required to interest the amateur astronomer in the
study of the moon. Our three-inch telescope is amply
sufficient to furnish us with entertainment for many an
evening while the moon is running through its phases,
and we shall find delight in frequently changing the magnifying
power as we watch the lunar landscapes, because
every change will present them in a different aspect.
It should be remembered that a telescope, unless a terrestrial
eyepiece or prism is employed, reverses such an
object as the moon top for bottom. Accordingly, if the
moon is on or near the meridian when the observations
are made, we shall see the north polar region at the
bottom and the south polar region at the top. In other
words, the face of the moon as presented in the telescope
will be upside down, north and south interchanging places
as compared with their positions in a geographical map.
But east and west remain unaltered in position, as compared
with such a map—i. e., the eastern hemisphere of
the moon is seen on the right and the western hemisphere
on the left. It is the moon's western edge that catches
the first sunlight when "new moon" begins, and, as the
phase increases, passing into "first quarter" and from
that to "full moon," the illumination sweeps across the
disk from west to east.
Lunar Chart No. 1, Northwest Quarter.
The narrow sickle of the new moon, hanging above the
sunset, is a charming telescopic sight. Use a low power,
and observe the contrast between the bright, smooth
round of the sunward edge, which has almost the polish
of a golden rim, and the irregular and delicately shaded
inner curve, where the adjacent mountains and plains
picturesquely reflect or subdue the sunshine. While the
crescent grows broader new objects are continually coming
into view as the sun rises upon them, until at length
one of the most conspicuous and remarkable of the lunar
"seas," the Mare Crisium, or Sea of Crises, lies fully displayed
amid its encircling peaks, precipices, and craters.
The Mare Crisium is all in the sunlight between the third
and fourth day after "new moon." It is about 350 by 280
miles in extent, and if ever filled with water must have
been a very deep sea, since its arid bed lies at a great but
not precisely ascertained depth below the general level
of the moon. There are a few small craters on the floor of
the Mare Crisium, the largest bearing the name of Picard,
and its borders are rugged with mountains. On the
southwestern side is a lofty promontory, 11,000 feet in
height, called Cape Agarum. At the middle of the eastern
side a kind of bay opens deep in the mountains, whose
range here becomes very narrow. Southeast of this bay
lies a conspicuous bright point, the crater mountain Proclus,
on which the sun has fully risen in the fourth day of
the moon, and which reflects the light with extraordinary
liveliness. Adjoining Proclus on the east and south is a
curious, lozenge-shaped flat, broken with short, low ridges,
and possessing a most peculiar light-brown tint, easily distinguished
from the general color tone of the lunar landscapes.
It would be interesting to know what was passing
in the mind of the old astronomer who named this singular
region Palus Somnii. It is not the only spot on the moon
which has been called a "marsh," and to which an unexplained
connection with dreams has been ascribed.
Nearly on the same meridian with Proclus, at a distance
of about a hundred miles northward, lies a fine example of
a ring mountain, rather more than forty miles in diameter,
and with peak-tipped walls which in some places are
13,000 feet in height, as measured from the floor within.
This is Macrobius. There is an inconspicuous central
mountain in the ring.
North of the Mare Crisium, and northwest of Macrobius,
we find a much larger mountain ring, oblong in
shape and nearly eighty miles in its greatest diameter.
It is named Cleomenes. The highest point on its wall is
about 10,000 feet above the interior. Near the northeast
corner of the wall yawns a huge and very deep crater,
Tralles, while at the northern end is another oblong
crater mountain called Burckhardt.
From Cleomenes northward to the pole, or to the
northern extremity of the crescent, if our observations
are made during new moon, the ground appears broken
with an immense number of ridges, craters, and mountain
rings, among which we may telescopically wander at will.
One of the more remarkable of these objects, which may
be identified with the aid of Lunar Chart No. 1, is the vast
ringed plain near the edge of the disk, named Gauss. It
is more than a hundred and ten miles in diameter. Owing
to its situation, so far down the side of the lunar globe, it
is foreshortened into a long ellipse, although in reality it
is nearly a circle. A chain of mountains runs north and
south across the interior plain. Geminus, Berzelius, and
Messala are other rings well worth looking at. The remarkable
pair called Atlas and Hercules demand more
than passing attention. The former is fifty-five and the latter
forty-six miles in diameter. Each sinks 11,000 feet below
the summit of the loftiest peak on its encircling wall.
Both are full of interesting detail sufficient to occupy the
careful observer for many nights. The broad ring bearing
the name of Endymion is nearly eighty miles in diameter,
and has one peak 15,000 feet high. The interior plain is flat
and dark. Beyond Endymion on the edge of the disk is
part of a gloomy plain called the Mare Humboltianum.
After glancing at the crater-shaped mountains on the
western and southern border of the Mare Crisium, Alhazen,
Hansen, Condorcet, Firmicus, etc., we pass southward
into the area covered in Lunar Chart No. 2. The long
dark plain south of the Mare Crisium is the Mare Fecunditatis,
though why it should have been supposed to be particularly
fecund, or fertile, is by no means clear. On the
western border of this plain, about three hundred miles
from the southern end of the Mare Crisium, is the mountain
ring, or circumvallation, called Langrenus, about ninety
miles across and in places 10,000 feet high. There is a fine
central mountain with a number of peaks. Nearly a hundred
miles farther south, on the same meridian, lies an
equally extensive mountain ring named Vendelinus. The
broken and complicated appearance of its northern walls
will command the observer's attention. Another similar
step southward, and still on the same meridian brings us to
a yet finer mountain ring, slightly larger than the others,
and still more complicated in its walls, peaks, and terraces,
and in its surroundings of craters, gorges, and broken
ridges. This is Petavius. West of Petavius, on the very
edge of the disk, is a wonderful formation, a walled plain
named Humboldt, which is looked down upon at one point
near its eastern edge by a peak 16,000 feet in height.
About a hundred and forty miles south of Petavius is the
fourth great mountain ring lying on the same meridian.
Its name is Furnerius. Look particularly at the brilliantly
shining crater on the northeast slope of the outer wall of
Furnerius.
Lunar Chart No. 2, Southwest Quarter.
Suppose that our observations are now interrupted,
to be resumed when the moon, about "seven days old," is
in its first quarter. If we had time, it would be a most
interesting thing to watch the advance of the lunar sunrise
every night, for new beauties are displayed almost
from hour to hour; but, for the purposes of our description
it is necessary to curtail the observations. At first
quarter one half of the lunar hemisphere which faces the
earth is illuminated by the sun, and the line of sunrise
runs across some of the most wonderful regions of the
moon.
We begin, referring once more to Lunar Chart No. 1,
in the neighborhood of the north pole of the moon. Here
the line along which day and night meet is twisted and
broken, owing to the roughness of the lunar surface.
About fifteen degrees southwest of the pole lies a remarkable
square-cornered, mountain-bordered plain, about
forty miles in length, called Barrow. Very close to the
pole is a ring mountain, about twenty-five miles in diameter,
whose two loftiest peaks, 8,000 to 9,000 feet high,
according to Neison, must, from their situation, enjoy perpetual
day.
The long, narrow, dark plain, whose nearest edge is
about thirty degrees south of the pole, is the Mare Frigoris,
bordered on both sides by uplands and mountains. At its
southern edge we find the magnificent Aristoteles, a
mountain ring, sixty miles across, whose immense wall is
composed of terraces and ridges running up to lofty peaks,
which rise nearly 11,000 feet above the floor of the valley.
About a hundred miles south of Aristoteles is Eudoxus,
another fine mountain ring, forty miles in diameter,
and quite as deep as its northern neighbor. These two
make a most striking spectacle.
We are now in the neighborhood of the greatest mountain
chains on the moon, the lunar Alps lying to the
east and the lunar Caucasus to the south of Aristoteles
and Eudoxus, while still farther south, separated from the
Caucasus by a strait not more than a hundred miles
broad, begins the mighty range of the lunar Apennines.
We first turn the telescope on the Alps. As the line of
sunrise runs directly across their highest peaks, the effect
is startling. The greatest elevations are about 12,000
feet. The observer's eye is instantly caught by a great
valley, running like a furrow through the center of the
mountain mass, and about eighty or ninety miles in
length. The sealike expanse south and southeast of the
Alps is the Mare Imbrium, and it is along the coast of this
so-called sea that the Alps attain their greatest height.
The valley, or gorge, above mentioned, appears to cut
through the loftiest mountains and to reach the "coast,"
although it is so narrowed and broken among the greater
peaks that its southern portion is almost lost before it
actually reaches the Mare Imbrium. Opening wider again
as it enters the Mare, it forms a deep bay among precipitous
mountains.
The Caucasus Mountains are not so lofty nor so precipitous
as the Alps, and consequently have less attraction
for the observer. They border the dark, oval plain of
the Mare Serenitatis on its northeastern side. The great
bay running out from the Mare toward the northwest, between
the Caucasus and the huge mountain ring of Posidonius,
bears the fanciful name of Lacus Somniorum. In
the old days when the moon was supposed to be inhabited,
those terrestrial godfathers, led by the astronomer Riccioli,
who were busy bestowing names upon the "seas" and
mountains of our patient satellite, may have pleased their
imagination by picturing this arm of the "Serene Sea" as
a peculiarly romantic sheet of water, amid whose magical
influences the lunar gentlefolk, drifting softly in their
silver galleons and barges, and enjoying the splendors of
"full earth" poured upon their delightful little world,
were accustomed to fall into charming reveries, as even
we hard-headed sons of Adam occasionally do when the
waters under the keel are calm and smooth and the balmy
air of a moonlit night invokes the twin spirits of poetry
and music.
Posidonius, the dominating feature of the shore line
here, is an extraordinary example of the many formations
on the moon which are so different from everything on
the earth that astronomers do not find it easy to bestow
upon them names that truly describe them. It may be
called a ring mountain or a ringed plain, for it is both.
Its diameter exceeds sixty miles, and the interior plain
lies about 2,000 feet below the outer surface of the lunar
ground. The mountain wall surrounding the ring is by
no means remarkable for elevation, its greatest height
not exceeding 6,000 feet, but, owing to the broad sweep of
the curved walls, the brightness of the plain they inclose,
and the picturesque irregularity of the silhouette of
shadow thrown upon the valley floor by the peaks encircling
it, the effect produced upon the observer is very
striking and attractive.
Having finished with Posidonius and glanced across
the broken region of the Taurus Mountains toward the
west, we turn next to consider the Mare Serenitatis. This
broad gray plain, which, with a slight magnifying power,
certainly looks enough like a sea to justify the first telescopists
in thinking that it might contain water, is about
430 by 425 miles in extent, its area being 125,000 square
miles. Running directly through its middle, nearly in a
north and south line, is a light streak, which even a good
opera glass shows. This streak is the largest and most
wonderful of the many similar rays which extend on all
sides from the great crater, or ring, of Tycho in the southern
hemisphere. The ray in question is more than 2,000
miles long, and, like its shorter congeners, it turns aside
for nothing; neither "sea," nor peak, nor mountain range,
nor crater ring, nor gorge, nor cañon, is able to divert it
from its course. It ascends all heights and drops into
all depths with perfect indifference, but its continuity is
not broken. When the sun does not illuminate it at a
proper angle, however, the mysterious ray vanishes. Is
it a metallic vein, or is it volcanic lava or ash? Was the
globe of the moon once split open along this line?
The Mare Serenitatis is encircled by mountain ranges to
a greater extent than any of the other lunar "seas." On
its eastern side the Caucasus and the Apennines shut it in,
except for a strait a hundred miles broad, by means of
which it is connected with the Mare Imbrium. On the
south the range of the Hæmus Mountains borders it, on
the north and northwest the Caucasus and the Taurus
Mountains confine it, while on the west, where again it
connects itself by a narrow strait with another "sea,"
the Mare Tranquilitatis, it encounters the massive uplift
of Mount Argæus. Not far from the eastern strait is
found the remarkable little crater named Linné, not conspicuous
on the gray floor of the Mare, yet easily enough
found, and very interesting because a considerable change
of form seems to have come over this crater some time
near the middle of the nineteenth century. In referring
to it as a crater it must not be forgotten that it does
not form an opening in the top of a mountain. In fact,
the so-called craters on the moon, generally speaking, are
simply cavities in the lunar surface, whose bottoms lie
deep below the general level, instead of being elevated on
the summit of mountains, and inclosed in a conical peak.
In regard to the alleged change in Linné, it has been suggested,
not that a volcanic eruption brought it about, but
that a downfall of steep walls, or of an unsupported rocky
floor, was the cause. The possibility of such an occurrence,
it must be admitted, adds to the interest of the observer
who regularly studies the moon with a telescope.
Just on the southern border of the Mare, the beautiful
ring Menelaus lies in the center of the chain of the Hæmus
Mountains. The ring is about twenty miles across, and
its central peak is composed of some highly reflecting
material, so that it shines very bright. The streak or
ray from Tycho which crosses the Mare Serenitatis passes
through the walls of Menelaus, and perhaps the central
peak is composed of the same substance that forms the ray.
Something more than a hundred miles east-southeast
from Menelaus, in the midst of the dark Mare Vaporum, is
another brilliant ring mountain which catches the eye,
Manilius. It exceeds Menelaus in brightness as well as
in size, its diameter being about twenty-five miles. There
is something singular underlying the dark lunar surface
here, for not only is Manilius extraordinarily brilliant in
contrast with the surrounding plain, but out of that plain,
about forty miles toward the east, projects a small mountain
which is also remarkable for its reflecting properties,
as if the gray ground were underlain by a stratum of some
material that flashes back the sunlight wherever it is exposed.
The crater mountain, Sulpicius Gallus, on the border
of the Mare, north of Manilius and east of Menelaus, is
another example of the strange shining quality of certain
formations on the moon.
Follow next the Hæmus range westward until the attention
falls upon the great ring mountain Plinius, more
than thirty miles across, and bearing an unusual resemblance
to a fortification. Mr. T. G. Elger, the celebrated
English selenographer, says of Plinius that, at sunrise,
"it reminds one of a great fortress or redoubt erected to
command the passage between the Mare Tranquilitatis and
the Mare Serenitatis." But, of course, the resemblance is
purely fanciful. Men, even though they dwelt in the
moon, would not build a rampart 6,000 feet high!
Mount Argæus, at the southwest corner of the Mare
Serenitatis, is a very wonderful object when the sun has
just risen upon it. This occurs five days after the new
moon.
Returning to the eastern extremity of the Mare, we
glance, in passing, at the precipitous Mount Hadley, which
rises more than 15,000 feet above the level of the Mare and
forms the northern point of the Apennine range. Passing
into the region of the Mare Imbrium, whose western end is
divided into the Palus Putredinis on the south and the
Palus Nebularum on the north, we notice three conspicuous
ring mountains, Cassini near the Alps, and Aristillus
and Autolycus, a beautiful pair, nearly opposite the
strait connecting the two Maria. Cassini is thirty-six
miles in diameter, Aristillus thirty-four, and Autolycus
twenty-three. The first named is shallow, only 4,000 feet
in depth from the highest point of its wall, while Aristillus
carries some peaks on its girdle 11,000 feet high. Autolycus,
like Cassini, is of no very great depth.
Westward from the middle of an imaginary line joining
Aristillus and Cassini is the much smaller crater Theætetus.
Outside the walls of this are a number of craterlets,
and a French astronomer, Charbonneaux, of the Meudon
Observatory, reported in December, 1900, that he had repeatedly
observed white clouds appearing and disappearing
over one of these small craters.
South of the Mare Vaporum are found some of the most
notable of those strange lunar features that are called
"clefts" or "rills." Two crater mountains, in particular,
are connected with them, Ariadæus at the eastern edge of
the Mare Tranquilitatis and Hyginus on the southern border
of the Mare Vaporum. These clefts appear to be broad
and deep chasms, like the cañons cut by terrestrial rivers,
but it can not be believed that the lunar cañons are the
work of rivers. They are rather cracks in the lunar crust,
although their bottoms are frequently visible. The principal
cleft from Ariadæus runs eastward and passes between
two neighboring craters, the southern of which is
named Silberschlag, and is noteworthy for its brightness.
The Hyginus cleft is broader and runs directly through
the crater ring of that name.
The observer will find much to interest him in the
great, irregular, and much-broken mountain ring called
Julius Cæsar, as well as in the ring mountains, Godin,
Agrippa, and Triesnecker. The last named, besides presenting
magnificent shadows when the sunlight falls
aslant upon it, is the center of a complicated system of
rills, some of which can be traced with our five-inch glass.
We next take up Lunar Chart No. 2, and pay a telescopic
visit to the southwestern quarter of the lunar
world. The Mare Tranquilitatis merges through straits
into two southern extensions, the Mare Fecunditatis and
the Mare Nectaris. The great ring mountains or ringed
plains, Langrenus, Vendelinus, Petavius, and Furnerius,
all lying significantly along the same lunar meridian, have
already been noticed. Their linear arrangement and isolated
position recall the row of huge volcanic peaks that
runs parallel with the shore of the Pacific Ocean in Oregon
and Washington—Mount Jefferson, Mount Hood, Mount
St. Helen's, Mount Tacoma—but these terrestrial volcanoes,
except in elevation, are mere pins' heads in the comparison.
In the eastern part of the Mare Fecunditatis lies a pair
of relatively small craters named Messier, which possess
particular interest because it has been suspected, though
not proved, that a change of form has occurred in one or
other of the pair. Mädler, in the first half of the nineteenth
century, represented the two craters as exactly
alike in all respects. In 1855 Webb discovered that they
are not alike in shape, and that the easternmost one is the
larger, and every observer easily sees that Webb's description
is correct. Messier is also remarkable for the light
streak, often said to resemble a comet's tail, which extends
from the larger crater eastward to the shore of the
Mare Fecunditatis.
Goclenius and Guttemberg, on the highland between
the Mare Fecunditatis and the Mare Nectaris, are intersected
and surrounded by clefts, besides being remarkable for
their broken and irregular though lofty walls. Guttemberg
is forty-five miles and Goclenius twenty-eight miles
in diameter. The short mountain range just east of Guttemberg,
and bordering a part of the Mare Nectaris on the
west, is called the Pyrenees.
The Mare Nectaris, though offering in its appearance no
explanation of its toothsome name—perhaps it was regarded
as the drinking cup of the Olympian gods—is one
of the most singular of the dark lunar plains in its outlines.
At the south it ends in a vast semicircular bay,
sixty miles across, which is evidently a half-submerged
mountain ring. But submerged by what? Not water,
but perhaps a sea of lava which has now solidified and
forms the floor of the Mare Nectaris. The name of this singular
formation is Fracastorius. Elger has an interesting
remark about it.
"On the higher portion of the interior, near the center,"
he says, "is a curious object consisting apparently of
four light spots, arranged in a square, with a craterlet in
the middle, all of which undergo notable changes of aspect
under different phases."
Other writers also call attention to the fine markings,
minute craterlets, and apparently changeable spots on the
floor of Fracastorius.
We go now to the eastern side of the Mare Nectaris,
where we find one of the most stupendous formations in
the lunar world, the great mountain ring of Theophilus,
noticeably regular in outline and perfect in the completeness
of its lofty wall. The circular interior, which contains
in the center a group of mountains, one of whose
peaks is 6,000 feet high, sinks 10,000 feet below the general
level of the moon outside the wall! One of the peaks
on the western edge towers more than 18,000 feet above
the floor within, while several other peaks attain elevations
of 15,000 to 16,000 feet. The diameter of the immense
ring, from crest to crest of the wall, is sixty-four miles.
Theophilus is especially wonderful on the fifth and sixth
days of the moon, when the sun climbs its shining pinnacles
and slowly discloses the tremendous chasm that lies
within its circles of terrible precipices.
On the southeast Theophilus is connected by extensions
of its walls with a shattered ring of vast extent
called Cyrillus; and south from Cyrillus, and connected
with the same system of broken walls, lies the still larger
ring named Catharina, whose half-ruined walls and numerous
crater pits present a fascinating spectacle as the
shadows retreat before the sunrise advancing across
them. These three—Theophilus, Cyrillus, and Catharina—constitute
a scene of surpassing magnificence, a glimpse
of wonders in another world sufficient to satisfy the most
riotous imagination.
South of the Mare Nectaris the huge ring mountain of
Piccolomini attracts attention, its massive walls surrounding
a floor nearly sixty miles across, and rising
in some places to an altitude of nearly 15,000 feet. It
should be understood that wherever the height of the
mountain wall of such a ring is mentioned, the reference
level is that of the interior plain or floor. The
elevation, reckoned from the outer side, is always very
much less.
The entire region south and east of Theophilus and its
great neighbors is marvelously rough and broken. Approaching
the center of the moon, we find a system of
ringed plains even greater in area than any of those we
have yet seen. Hipparchus is nearly a hundred miles
long from north to south, and nearly ninety miles broad
from east to west. But its walls have been destroyed
to such an extent that, after all, it yields in grandeur to a
formation like Theophilus.
Albategnius is sixty-five miles across, with peaks from
10,000 to 15,000 feet in height. Sacrobosco is a confused
mass of broken and distorted walls. Aliacensis is remarkable
for having a peak on the eastern side of its wall
which is more than 16,000 feet high. Werner, forty-five
miles in diameter, is interesting because under its northeastern
wall Mädler, some seventy years ago, saw a light
spot of astonishing brightness, unmatched in that respect
by anything on the moon except the peak of Aristarchus,
which we shall see later. This spot seems afterward to
have lost brilliance, and the startling suggestion has been
made that its original brightness might have been due to
its then recent deposit from a little crater that lies in the
midst of it. Walter is of gigantic dimensions, about one
hundred miles in diameter. Unlike the majority of the
ringed plains, it departs widely from a circle. Stöfler is
yet larger than Walter; but most interesting of all these
gigantic formations is Maurolycus, whose diameter exceeds
one hundred and fifty miles, and which has walls
13,000 or 14,000 feet high. Yet, astonishing though it
may seem, this vast and complicated mass of mountain
walls, craters, and peaks, is virtually unseen at full moon,
owing to the perpendicularity of the sunlight, which prevents
the casting of shadows.
We shall next suppose that another period of about
seven days has elapsed, the moon in the meantime reaching
its full phase. We refer for guidance to Lunar Chart
No. 3. The peculiarity of the northeastern quadrant
which immediately strikes the eye is the prevalence of the
broad plains called Maria, or "seas." The northern and
central parts are occupied by the Mare Imbrium, the "Sea
of Showers" or of "Rains," with its dark bay the Sinus
Æstuum, while the eastern half is covered by the vast
Oceanus Procellarum, the "Ocean of Storms" or of "Tempests."
Toward the north a conspicuous oval, remarkably dark
in hue, immediately attracts our attention. It is the celebrated
ringed plain of Plato, about sixty miles in diameter
and surrounded by a saw-edged rampart, some of whose
pinnacles are 6,000 or 7,000 feet high. Plato is a favorite
subject for study by selenographers because of the
changes of color which its broad, flat floor undergoes as
the sun rises upon it, and also because of the existence of
enigmatical spots and streaks whose visibility changes.
South of Plato, in the Mare Imbrium, rises a precipitous,
isolated peak called Pico, 8,000 feet in height. Its resemblance
in situation to the conical mountain Pico in the
Azores strikes the observer.
Eastward of Plato a line of highlands, separating the
Mare Imbrium from the Mare Frigoris, carries the eye to
the beautiful semicircular Sinus Iridum, or "Bay of Rainbows."
The northwestern extremity of this remarkable
bay is guarded by a steep and lofty promontory called
Cape Laplace, while the southeastern extremity also has
its towering guardian, Cape Heraclides. The latter is
interesting for showing, between nine and ten days after
full moon, a singularly perfect profile of a woman's face
looking out across the Mare Imbrium. The winding lines,
like submerged ridges, delicately marking the floor of the
Sinus Iridum and that of the Mare beyond, are beautiful
telescopic objects. The "bay" is about one hundred and
thirty-five miles long by eighty-four broad.
Lunar Chart No. 3, Northeast Quarter.
The Mare Imbrium, covering 340,000 square miles, is
sparingly dotted over with craters. All of the more conspicuous
of them are indicated in the chart. The smaller
ones, like Caroline Herschel, Helicon, Leverrier, Délisle,
etc., vary from eight to twelve miles in diameter. Lambert
is seventeen miles in diameter, and Euler nineteen,
while Timocharis is twenty-three miles broad and 7,000
feet deep below its walls, which rise only 3,000 feet above
the surface of the Mare.
Toward the eastern border of the sea, south of the Harbinger
Mountains, we find a most remarkable object, the
mountain ring, or crater plain, called Aristarchus. This
ring is not quite thirty miles in diameter, but there is
nothing on the moon that can compare with it in dazzling
brilliance. The central peak, 1,200 or 1,300 feet high,
gleams like a mountain of crusted snow, or as if it were
composed of a mass of fresh-broken white metal, or of compacted
crystals. Part of the inner slope of the east wall is
equally brilliant. In fact, so much light is poured out of
the circumvallation that the eye is partially blinded, and
unable distinctly to see the details of the interior. No
satisfactory explanation of the extraordinary reflecting
power of Aristarchus has ever been offered. Its neighbor
toward the east, Herodotus, is somewhat smaller and
not remarkably bright, but it derives great interest from
the fact that out of a breach in its northern wall issues
a vast cleft, or chasm, which winds away for nearly a
hundred miles across the floor of the Mare, making an
abrupt turn when it reaches the foot of the Harbinger
Mountains.
The comparatively small crater, Lichtenberg, near the
northeastern limb of the moon, is interesting because Mädler
used to see in its neighborhood a pale-red tint which
has not been noticed since his day.
Returning to the western side of the quadrant represented
in Lunar Chart No. 3, we see the broad and beautifully
regular ringed plain of Archimedes, fifty miles in
diameter and 4,000 feet deep.
A number of clefts extend between the mountainous
neighborhood of Archimedes and the feet of the gigantic
Apennine Mountains on the southwest. The little double
crater, Beer, between Archimedes and Timocharis, is very
bright.
The Apennines extend about four hundred and eighty
miles in a northwesterly and southeasterly direction.
One of their peaks near the southern end of the range,
Mount Huygens, is at least 18,000 feet high, and the black
silhouettes of their sharp-pointed shadows thrown upon
the smooth floor of the Mare Imbrium about the time of
first quarter present a spectacle as beautiful as it is
unique. The Apennines end at the southeast in the ring
mountain, Eratosthenes, thirty-eight miles across and
very deep, one of its encircling chain of peaks rising
16,000 feet above the floor, and about half that height
above the level of the Mare Imbrium. The shadows cast
by Eratosthenes at sunrise are magnificent.
And now we come to one of the supreme spectacles of
the moon, the immense ring or crater mountain Copernicus.
This is generally regarded as the grandest object
that the telescope reveals on the earth's satellite. It is
about fifty-six miles across, and its interior falls to a
depth of 8,000 feet below the Mare Imbrium. Its broad
wall, composed of circle within circle of ridges, terraces,
and precipices, rises on the east about 12,000 feet above
the floor. On the inner side the slopes are very steep, cliff
falling below cliff, until the bottom of the fearful abyss is
attained. To descend those precipices and reach the depressed
floor of Copernicus would be a memorable feat for
a mountaineer. In the center of the floor rises a complicated
mountain mass about 2,400 feet high. All around
Copernicus the surface of the moon is dotted with countless
little crater pits, and splashed with whitish streaks.
Northward lie the Carpathian Mountains, terminating on
the east in Tobias Mayer, a ring mountain more than
twenty miles across. The mountain ring Kepler, which is
also the center of a great system of whitish streaks and
splashes, is twenty-two miles in diameter, and notably
brilliant.
Finally, we turn to the southeastern quadrant of the
moon, represented in Lunar Chart No. 4. The broad,
dark expanse extending from the north is the Mare Nubium
on the west and the Oceanus Procellarum on the east. Toward
the southeast appears the notably dark, rounded
area of the Mare Humorum inclosed by highlands and
rings. We begin with the range of vast inclosures running
southward near the central meridian, and starting
with Ptolemæus, a walled plain one hundred and fifteen
miles in its greatest diameter and covering an area considerably
exceeding that of the State of Massachusetts.
Its neighbor toward the south, Alphonsus, is eighty-three
miles across. Next comes Arzachel, more than sixty-five
miles in diameter. Thebit, more than thirty miles across,
is very deep. East of Thebit lies the celebrated "lunar
railroad," a straight, isolated wall about five hundred feet
high and sixty-five miles long, dividing at its southern end
into a number of curious branches, forming the buttresses
of a low mountain. Purbach is sixty miles broad, and
south of that comes a wonderful region where the ring
mountains Hell, Ball, Lexell, and others, more or less
connected with walls, inclose an area even larger than
Ptolemæus, but which, not being so distinctly bordered as
some of the other inclosed plains, bears no distinctive
name.
Lunar Chart No. 4, Southeast Quarter.
The next conspicuous object toward the south ranks
with Copernicus among the grandest of all lunar phenomena—the
ring, or crater, Tycho. It is about fifty-four
miles in diameter and some points on its wall rise 17,000
feet above the interior. In the center is a bright mountain
peak 5,000 feet high. But wonderful as are the details
of its mountain ring, the chief attraction of Tycho is
its manifest relation to the mysterious bright rays heretofore
referred to, which extend far across the surface of
the moon in all directions, and of which it is the center.
The streaks about Copernicus are short and confused, constituting
rather a splash than a regular system of rays;
but those emanating from Tycho are very long, regular,
comparatively narrow, and form arcs of great circles which
stretch away for hundreds of miles, allowing no obstacle to
interrupt their course.
Southwest of Tycho lies the vast ringed plain of Maginus,
a hundred miles broad and very wonderful to look
upon, with its labyrinth of formations, when the sun
slopes across it, and yet, like Maurolycus, invisible under
a vertical illumination. "The full moon," to use Mädler's
picturesque expression, "knows no Maginus." Still
larger and yet more splendid is Clavius, which exceeds
one hundred and forty miles in diameter and covers 16,000
square miles of ground within its fringing walls, which
carry some of the loftiest peaks on the moon, several attaining
17,000 feet. The floor is deeply depressed, so that
an inhabitant of this singular inclosure, larger than Massachusetts,
Connecticut, and Rhode Island combined, would
dwell in land sunk two miles below the general level of
the world about him.
In the neighborhood of the south pole lies the large
walled plain of Newton, whose interior is the deepest
known depression on the moon. It is so deep that the sunshine
never touches the larger part of the floor of the
inner abyss, and a peak on its eastern wall rises 24,000
feet sheer above the tremendous pit. Other enormous
walled plains are Longomontanus, Wilhelm I, Schiller,
Bailly, and Schickard. The latter is one hundred and
thirty-four miles long and bordered by a ring varying from
4,000 to 9,000 feet in height. Wargentin, the oval close to
the moon's southeast limb, beyond Schickard, is a unique
formation in that, instead of its interior being sunk below
the general level, it is elevated above it. It has been
suggested that this peculiarity is due to the fact that the
floor of Wargentin was formed by inflation from below,
and that it has cooled and solidified in the shape of a
gigantic dome arched over an immense cavity beneath. A
dome of such dimensions, however, could not retain its
form unless partly supported from beneath.
Hainzel is interesting from its curious outline; Cichus
for the huge yawning crater on its eastern wall; Capuanus
for a brilliant shining crater also on its eastern wall;
and Mercator for possessing bright craters on both its
east and its west walls. Vitello has a bright central
mountain and gains conspicuousness from its position at
the edge of the dark Mare Humorum. Agatharchides is
the broken remnant of a great ring mountain. Gassendi,
an extremely beautiful object, is about fifty-five miles
across. It is encircled with broken walls, craters and
bright points, and altogether presents a very splendid
appearance about the eleventh day of the moon's age.
Letronne is a half-submerged ring, at the southern end
of the Oceanus Procellarum, which recalls Fracastorius in
the western lunar hemisphere. It lies, however, ten degrees
nearer the equator than Fracastorius. Billy is a
mountain ring whose interior seems to have been submerged
by the dark substance of the Oceanus Procellarum,
although its walls have remained intact. Mersenius is a
very conspicuous ring, forty miles in diameter, east of the
Mare Humorum. Vieta, fifty miles across, is also a fine
object. Grimaldi, a huge dusky oval, is nearly one hundred
and fifty miles in its greatest length. The ring mountain
Landsberg, on the equator, and near the center of
the visible eastern hemisphere, is worth watching because
Elger noticed changes of color in its interior in 1888.
Bullialdus, in the midst of the Mare Nubium, is a very
conspicuous and beautiful ring mountain about thirty-eight
miles in diameter, with walls 8,000 feet high above
the interior.
Those who wish to see the lunar mountains in all their
varying aspects will not content themselves with views
obtained during the advance of the sunlight from west to
east, between "new moon" and "full moon," but will continue
their observations during the retreat of the sunlight
from east to west, after the full phase is passed.
It is evident that the hemisphere of the moon which is
forever turned away from the earth is quite as marvelous
in its features as the part that we see. It will be noticed
that the entire circle of the moon's limb, with insignificant
interruptions, is mountainous. Possibly the invisible side
of our satellite contains yet grander peaks and crater
mountains than any that our telescopes can reach. This
probability is increased by the fact that the loftiest
known mountain on the moon is never seen except in silhouette.
It is a member of a great chain that breaks the
lunar limb west of the south pole, and that is called the
Leibnitz Mountains. The particular peak referred to is
said by some authorities to exceed 30,000 feet in height.
Other great ranges seen only in profile are the Dörfel
Mountains on the limb behind the ring plain Bailly, the
Cordilleras, east of Eichstadt, and the D'Alembert Mountains
beyond Grimaldi. The profile of these great mountains
is particularly fine when they are seen during an
eclipse of the sun. Then, with the disk of the sun for a
background, they stand out with startling distinctness.
When the sun is covered with spots it becomes a most
interesting object for telescopic study. Every amateur's
telescope should be provided with apparatus for viewing
the sun. A dark shade glass is not sufficient and not safe.
What is known as a solar prism, consisting of two solid
prisms of glass, cemented together in a brass box which
carries a short tube for the eyepiece, and reflecting an image
of the sun from their plane of junction—while the
major remnant of light and heat passes directly through
them and escapes from an opening provided for the purpose—serves
very well. Better and more costly is an apparatus
called a helioscope, constructed on the principle
of polarization and provided with prisms and reflectors
which enable the observer, by proper adjustment, to govern
very exactly and delicately the amount of light that
passes into the eyepiece.
Furnished with an apparatus of this description we
can employ either a three-, four-, or five-inch glass upon the
sun with much satisfaction. For the amateur's purposes
the sun is only specially interesting when it is spotted.
The first years of the twentieth century will behold a
gradual growth in the number and size of the solar spots
as those years happen to coincide with the increasing
phase of the sun-spot period. Large sun spots and groups
of spots often present an immense amount of detail which
tasks the skill of the draughtsman to represent it. But a
little practice will enable one to produce very good representations
of sun spots, as well as of the whitish patches
called faculæ by which they are frequently surrounded.
For the simple purpose of exhibiting the spotted face
of the sun without much magnifying power, a telescope
may be used to project the solar image on a white sheet or
screen. If the experiment is tried in a room, a little ingenuity
will enable the observer to arrange a curtain covering
the window used, in such a way as to exclude all
the light except that which comes through the telescope.
Then, by placing a sheet of paper or a drawing board before
the eyepiece and focusing the image of the sun upon
it, very good results may be obtained.
If one has a permanent mounting and a driving clock,
a small spectroscope may be attached, for solar observations,
even to a telescope of only four or five inches aperture,
and with its aid most interesting views may be obtained
of the wonderful red hydrogen flames that frequently
appear at the edge of the solar disk.