This means that different parts of the Earth receive varying amounts of sunlight at different times of the year, resulting in the seasons. When the Northern Hemisphere is tilted towards the Sun, it receives more direct sunlight and experiences summer, while the Southern Hemisphere tilts away from the Sun and experiences winter. Six months later, the situation reverses, and the Southern Hemisphere experiences summer while the Northern Hemisphere experiences winter.
It's important to note that while the Earth's tilt remains constant, the Earth's orbit around the Sun is not perfectly circular. Instead, it is slightly elliptical, meaning that the distance between the Earth and the Sun varies throughout the year. However, this variation in distance does not significantly affect the Earth's seasons or its overall tilt.