<u>As the Earth revolves around the Sun, and as the Earth rotates on its axis</u>, <u><em>which is tilted 23.5 degrees</em></u>, <u>the sunlight reaches the planet in different degrees, and that is why we have different seasons around the world.</u>
<u>The solstice is when the sun is at its highest or lowest point in the hemisphere, and from that day, the days of sunlight are longer or shorter</u>,<em><u> in the winter and summer solstices.
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<u>The autumn and spring equinoxes are the days when the axis of the Earth is as straight as possible and the sun's rays fall on the equator</u>. <em><u>While in one hemisphere it is spring, in the other it will be autumn.</u></em>