The Earth experiences four distinct seasons—spring, summer, autumn, and winter—due to its axial tilt and orbit around the Sun. As the Earth revolves around the Sun, different parts of the planet receive varying amounts of sunlight. The tilt of the Earth's axis causes different regions to be inclined toward or away from the Sun at different times of the year, resulting in the changing seasons. During spring, temperatures rise, and plants start to bloom. Summer brings warmth and longer daylight hours. Autumn is marked by cooling temperatures and the vibrant colors of falling leaves. Winter is characterized by colder temperatures and, in some regions, snowfall. The cycle of seasons influences various aspects of life on Earth, from wildlife behavior to agricultural activities.
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