The seasons are caused by the tilt of the Earth's axis of rotation relative to its orbit around the sun. During the summer and winter solstices, the sun's rays hit the Earth most directly at the Tropics of Cancer and Capricorn, respectively, causing the longest and shortest days of the year in the northern and southern hemispheres. Twice a year during the equinoxes, day and night are approximately equal lengths everywhere on Earth as the sun's rays hit the equator most directly.