Earth's Faithful
Companion

The Moon is Earth's only natural satellite and the fifth largest satellite in the Solar System. It is the largest natural satellite relative to its planet in the Solar System. The Moon has been a source of fascination for humanity throughout history, influencing our calendars, cultures, and inspiring countless stories and myths.

The Moon formed approximately 4.5 billion years ago, not long after Earth. The most widely accepted explanation is that the Moon formed from the debris left over after a giant impact between Earth and a Mars-sized body called Theia.

Phases of the Moon

New Moon

New Moon

When the Moon is between Earth and the Sun, the side facing Earth is not illuminated.

Waxing Crescent

Waxing Crescent

As the Moon moves away from the Sun, a small crescent becomes visible.

First Quarter

First Quarter

Half of the visible side of the Moon is illuminated.

Waxing Gibbous

Waxing Gibbous

More than half of the visible side is illuminated, approaching full moon.

Full Moon

Full Moon

The entire visible side of the Moon is illuminated.

Waning Gibbous

Waning Gibbous

The illuminated portion starts to decrease.

Last Quarter

Last Quarter

Half of the visible side is illuminated, opposite to first quarter.

Waning Crescent

Waning Crescent

A small crescent remains visible before returning to new moon.

Key Facts

Distance from Earth

384,400 km (average)

Orbital Period

27.3 days

Diameter

3,474 km

Surface Gravity

1.62 m/s² (0.1654 g)

Temperature Range

-173°C to 127°C

Age

4.5 billion years

Notable Features

Maria (Seas)

Large, dark plains formed by ancient volcanic eruptions

Craters

Impact craters formed by meteoroids and asteroids

Highlands

Light-colored, heavily cratered regions

Rilles

Long, narrow depressions resembling channels

Human Exploration

1959

Luna 2

First spacecraft to reach the Moon's surface

1969

Apollo 11

"That's one small step for man, one giant leap for mankind"

1972

Apollo 17

Last human mission to the Moon

2019

Chang'e 4

First landing on the far side of the Moon

Future

Artemis Program

NASA's plan to return humans to the Moon

Influence on Earth

Tides

The Moon's gravity pulls on Earth's oceans, causing high and low tides

Stabilization

Helps stabilize Earth's axial tilt, preventing extreme seasonal variations

Calendars

Lunar cycles have influenced calendar systems throughout human history

Lunar Resources

Lunar Terrain

Lunar Terrain Map

The lunar surface features mountains, valleys, and vast plains called maria. The near side (facing Earth) has more maria, while the far side is heavily cratered.

Highest Point: 10.8 km (Mons Huygens)
Deepest Crater: 9.1 km (South Pole-Aitken Basin)

Lunar Panorama

Lunar Surface Panorama
View in Full Screen

Apollo 11 mission panorama showing Buzz Aldrin on the lunar surface, July 20, 1969.

Did You Know?

The Moon and Earth

The Earth-Moon system is unique in our solar system. The Moon is exceptionally large relative to its parent planet, making it more of a binary system than a typical planet-satellite relationship. Together, they orbit around a common barycenter (center of mass) which lies about 4,671 km from Earth's center.

The Moon is gradually moving away from Earth at a rate of approximately 3.8 cm per year due to tidal interactions. Eventually, in the very distant future, the Moon will appear smaller in our sky and total solar eclipses will no longer be possible.