Solstices are caused by Earth's tilt, affecting the amount of sunlight each hemisphere receives and leading to distinct seasons.
Solstices occur when the Earth's tilt causes one hemisphere to be tipped towards the Sun, leading to longer periods of daylight and more direct sunlight, resulting in warmer temperatures during summer solstice and cooler temperatures during winter solstice. These events influence the amount of sunlight received in each hemisphere, with the Northern Hemisphere experiencing summer when tilted towards the Sun, and the Southern Hemisphere experiencing summer when tilted away. This phenomenon demonstrates the impact of Earth's axial tilt on the changing of seasons around the globe.
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