Seasons are the four main divisions of the year - spring, summer, autumn (fall), and winter - that are characterized by specific weather patterns and daylight hours. The changing of the seasons is caused by the tilt of the Earth's axis as it orbits the sun.
The Earth's axis is tilted at an angle of approximately 23.5 degrees. This tilt causes different parts of the Earth to receive varying amounts of sunlight at different times of the year. When a particular hemisphere is tilted toward the sun, it experiences summer, while the opposite hemisphere experiences winter. As the Earth continues its orbit, the tilt causes the seasons to change.
Each season brings specific changes in weather, temperature, and daylight hours. For example, summer is generally characterized by longer days, warmer temperatures, and more direct sunlight, while winter has shorter days, colder temperatures, and less direct sunlight. Spring and autumn fall in between, with mild temperatures and changing daylight hours.