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The Earth's Moon



The Earth's Moon
Click on image for full size (37K JPEG)
Image courtesy of NASA.
The Earth may only have one Moon, but it's a big one! The Earth's Moon is the fifth largest in the whole solar system. But it is still smaller than the Earth, so objects weigh less on the Moon than they do here. That's why the astronauts could enjoy bouncing around on the lunar surface.

Even though the Moon has no liquid water, it does have special "seas" and "land" on its surface. There are also many interesting features such as craters, mountain ranges, and lava plains. The interior of the Moon is made up of different layers of rock, some solid and some molten like lava. By studying the Moon's surface and interior, geologists can learn about the Moon's geological history and its formation.

The footprints left behind by the Apollo astronauts will last for many thousands of years because there is no wind on the Moon. The Moon has no atmosphere, so there is no weather to erase the footprints. On the Earth, the atmosphere acts as a blanket, keeping the warmth of the Sun in even at night. Because there is no atmosphere on the Moon, the temperatures there are very hot during the day (100 ° C) and very cold at night (-173 ° C).

The Moon doesn't produce its own light, but looks bright because it reflects light from the Sun. Think of the Sun as a light bulb, and the Moon as a mirror, reflecting light from the light bulb. The lunar phase changes as the Moon orbits the Earth and different portions of its surface are illuminated by the Sun.

Frequently Asked Questions about the Moon

Information on lunar eclipses

Table of recent and future lunar eclipses

Full Moon Names

An Article about the Findings from the Apollo Program1978

Lunar Links

Moon Image Archive

The Earth's Moon



The Earth's Moon
Click on image for full size (37K JPEG)
Image courtesy of NASA.
The Earth's one natural satellite, the Moon, is more than one quarter the size of Earth itself (3,474 km diameter). Because of its smaller size, the Moon's gravity is one-sixth of the Earth's gravity, as we saw demonstrated by the giant leaps of the Apollo astronauts.

While there are only two basic types of regions on the Moon's surface, there are many interesting surface features such as craters, mountain ranges, rilles, and lava plains. The structure of the Moon's interior is more difficult to study. The Moon's top layer is a rocky solid, perhaps 800 km thick. Beneath this layer is a partially molten zone. Although it is not known for certain, many lunar geologists believe the Moon may have a small iron core, even though the Moon has no magnetic field. By studying the Moon's surface and interior, geologists can learn about the Moon's geological history and its formation.

The footprints left by Apollo astronauts will last for centuries because there is no wind on the Moon. The Moon does not possess any atmosphere, so there is no weather as we are used to on Earth. Because there is no atmosphere to trap heat, the temperatures on the Moon are extreme, ranging from 100° C at noon to -173° C at night.

The Moon doesn't produce its own light, but looks bright because it reflects light from the Sun. Think of the Sun as a light bulb, and the Moon as a mirror, reflecting light from the light bulb. The lunar phase changes as the Moon orbits the Earth and different portions of its surface are illuminated by the Sun.

Frequently Asked Questions about the Moon

Information on lunar eclipses

Table of recent and future lunar eclipses

The Many Names for the Full Moon

An Article about the Findings from the Apollo Program1978

Lunar Links

Moon Image Archive

The Earth's Moon



The Earth's Moon
Click on image for full size (37K JPEG)
Image courtesy of NASA.
The Earth's one natural satellite, the Moon, is more than one quarter the size of Earth itself (3,474 km diameter), making the Earth-Moon system virtually a double-planet. Because of its smaller size, the Moon's gravity is one-sixth of the Earth's gravity, as we saw demonstrated by the gigantic leaps of the Apollo astronauts.

While there are only two basic types of regions on the Moon's surface, there are many interesting surface features such as craters, mountain ranges, rilles, and lava plains. The structure of the Moon's interior is more difficult to study. The Moon's crust, the top layer, is a rocky solid. Below the crust is the mantle which consists of a denser rock. Together, the crust and mantle form the Moon's lithosphere, which is very thick (perhaps 800 km) compared to the Earth's lithosphere. Beneath the lithosphere is a partially molten zone. Although it is not known for certain, many lunar geologists believe the Moon may have a small iron core, even though the Moon has no measurable magnetic field. By studying the Moon's surface and interior, geologists can learn about the Moon's geological history and its formation.

The footprints left by Apollo astronauts will last for centuries because there is no wind on the Moon. The Moon does not possess any atmosphere, so there is no weather as we are used to on Earth. Because there is no atmosphere to trap heat, the temperatures on the Moon vary dramatically over the course of a day, from 100° C at noon to -173° C at night.

The Moon doesn't produce its own light, but looks bright because it reflects light from the Sun. Think of the Sun as a light bulb, and the Moon as a mirror, reflecting light from the light bulb. The lunar phase changes as the Moon orbits the Earth and different portions of its surface are illuminated by the Sun.

Frequently Asked Questions about the Moon

Information on lunar eclipses

Table of recent and future lunar eclipses

Nicknames for the Full Moon

An Article about the Findings from the Apollo Program1978

Lunar Links

Moon Image Archive


Last modified October 19, 2005 by Randy Russell.
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