The Earth has two main motions that affect its seasons: rotation, which causes day and night, and revolution around the Sun. The tilt of the Earth's axis of rotation combined with its revolution cause the seasons by changing which hemisphere receives more direct sunlight throughout the year. The solstices mark the summer and winter beginning in each hemisphere when the Sun is at its maximum northern and southern declinations, while the equinoxes occur when day and night are equal in length as the Sun crosses the celestial equator.