The moon is Earth's only natural satellite and is the fifth largest moon in the solar system. It has a significant influence on the Earth's tides and has been the subject of scientific study and exploration for centuries.
The most widely accepted theory for the formation of the moon is the giant impact hypothesis. This theory suggests that the moon was formed from debris left over after a collision between Earth and a Mars-sized body early in the history of the solar system.
The moon's surface is covered in craters, plains, and mountains. It is composed of rocky material, with a relatively thin and patchy atmosphere consisting of various gases.
The moon goes through different phases as it orbits the Earth. These phases include new moon, first quarter, full moon, and last quarter. The changing appearance of the moon is due to the relative positions of the Earth, moon, and sun.
The moon's gravitational pull is responsible for the ocean tides on Earth. This pull is also the reason behind the phenomenon of tidal locking, which has resulted in the moon always showing the same face to the Earth.
The moon has been the target of numerous space missions, both manned and unmanned. The Apollo missions in the late 1960s and early 1970s were the first to land humans on the moon. Since then, various robotic missions have continued to study the moon's surface and its composition.