The moon is Earth's only natural satellite and is the fifth largest moon in the solar system. It has a significant impact on Earth's tides, and its phases have been studied and revered by humans for centuries.
The leading theory for the formation of the moon is the Giant Impact Hypothesis. This suggests that the moon was formed from the debris left over after a giant impact between Earth and a Mars-sized body early in the history of the solar system.
The moon's appearance changes over the course of a month, as it goes through its different phases: new moon, waxing crescent, first quarter, waxing gibbous, full moon, waning gibbous, third quarter, and waning crescent.
The moon's surface is covered in large, dark plains called maria, and is also home to numerous craters, mountains, and valleys. The lack of atmosphere and weather on the moon means that these surface features remain relatively unchanged over vast periods of time.
The moon's gravitational pull is responsible for the ocean tides on Earth. This gravitational interaction also causes the moon to become tidally locked, meaning the same face of the moon always faces towards Earth.
Humans first landed on the moon in 1969 during the Apollo 11 mission. Since then, several other missions have been sent to the moon to study its surface and geology.