The Mountains of the Moon

October 22, 2009 | Posted by maneerat

If you're new here, you may want to subscribe to my RSS feed. Thanks for visiting!

The lack of air is considered by many astronomers to furnish the explanation of the enormous number of “craters” which pit the moon’s surface. There are about a hundred thousand of these strange rings, and it is now believed by many that they are spots where very large meteorites, or even planetoids, splashed into the moon when its surface was still soft. Other astronomers think that they are the remains of gigantic bubbles which were raised in the moon’s “skin,” when the globe was still molten, by volcanic gases from below. A few astronomers think that they are, as is popularly supposed, the craters of extinct volcanoes. Our craters, on the earth, are generally deep cups, whereas these ring-formations on the moon are more like very shallow and broad saucers. Clavius, the largest of them, is 123 miles across the interior, yet its encircling rampart is not a mile high.

The mountains on the moon (Fig. 16) rise to a great height,[Pg 35] and are extraordinarily gaunt and rugged. They are like fountains of lava, rising in places to 26,000 and 27,000 feet. The lunar Apennines have three thousand steep and weird peaks. Our terrestrial mountains are continually worn down by frost acting on moisture and by ice and water, but there are none of these agencies operating on the moon. Its mountains are comparatively “everlasting hills.”

The moon is interesting to us precisely because it is a dead world. It seems to show how the earth, or any cooling metal globe, will evolve in the remote future. We do not know if there was ever life on the moon, but in any case it cannot have proceeded far in development. At the most we can imagine some strange lowly forms of vegetation lingering here and there in pools of heavy gas, expanding during the blaze of the sun’s long day, and frozen rigid during the long night.

METEORS AND COMETS

We may conclude our survey of the solar system with a word about “shooting stars,” or meteors, and comets. There are few now who do not know that the streak of fire which suddenly lights the sky overhead at night means that a piece of stone or iron has entered our atmosphere from outer space, and has been burned up by friction. It was travelling at, perhaps, twenty or thirty miles a second. At seventy or eighty miles above our heads it began to glow, as at that height the air is thick enough to offer serious friction and raise it to a white heat. By the time the meteor reached about twenty miles or so from the earth’s surface it was entirely dissipated, as a rule in fiery vapour.

Millions of Meteorites

It is estimated that between ten and a hundred million meteorites enter our atmosphere and are cremated, every day.[Pg 36] Most of them weigh only an ounce or two, and are invisible. Some of them weigh a ton or more, but even against these large masses the air acts as a kind of “torpedo-net.” They generally burst into fragments and fall without doing damage.

It is clear that “empty space” is, at least within the limits of our solar system, full of these things. They swarm like fishes in the seas. Like the fishes, moreover, they may be either solitary or gregarious. The solitary bit of cosmic rubbish is the meteorite, which we have just examined. A “social” group of meteorites is the essential part of a comet. The nucleus, or bright central part, of the head of a comet (Fig. 19) consists of a swarm, sometimes thousands of miles wide, of these pieces of iron or stone. This swarm has come under the sun’s gravitational influence, and is forced to travel round it. From some dark region of space it has moved slowly into our system. It is not then a comet, for it has no tail. But as the crowded meteors approach the sun, the speed increases. They give off fine vapour-like matter and the fierce flood of light from the sun sweeps this vapour out in an ever-lengthening tail. Whatever way the comet is travelling, the tail always points away from the sun.

A Great Comet

The vapoury tail often grows to an enormous length as the comet approaches the sun. The great comet of 1843 had a tail two hundred million miles long. It is, however, composed of the thinnest vapours imaginable. Twice during the nineteenth century the earth passed through the tail of a comet, and nothing was felt. The vapours of the tail are, in fact, so attenuated that we can hardly imagine them to be white-hot. They may be lit by some electrical force. However that may be, the comet dashes round the sun, often at three or four hundred miles a second, then may pass gradually out of our system once more. It may be a thousand years, or it may be fifty years, before[Pg 37] the monarch of the system will summon it again to make its fiery journey round his throne.

Photo: Harvard College Observatory.

FIG. 21.—TYPICAL SPECTRA

Six main types of stellar spectra. Notice the lines they have in common, showing what elements are met with in different types of stars. Each of these spectra corresponds to a different set of physical and chemical conditions.

Photo: Mount Wilson Observatory.

FIG. 22.—A NEBULAR REGION SOUTH OF ZETA ORIONIS

Showing a great projection of “dark matter” cutting off the light from behind.

Photo: Astrophysical Observatory, Victoria, British Columbia.

FIG. 23.—STAR CLUSTER IN HERCULES

A wonderful cluster of stars. It has been estimated that the distance of this cluster is such that it would take light more than 100,000 years to reach us.

Categories: THE OUTLINE OF SCIENCE | Tags: Apennines, Astronomers, Blaze, Bubbles, Craters On The Earth, Everlasting Hills, Fountains, Hundred Thousand, Lava, Life On The Moon, Meteorites, Meteors And Comets, Mountains Of The Moon, Mountains On The Moon, Planetoids, Rampart, Shooting Stars, Solar System, Vegetation, Volcanic Gases | No Comments »