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As the Earth orbits around the Sun, its axis
remains tilted at 2342° from the orbital path
throughout. This means that as the Earth
revolves, the northern hemisphere faces the Sun
for one part of the year and tilts away from the
Sun for the other part of the year. It also means
that different locations on the Earth face the
TSun at various times of the year. This constant
inclination of the Earth on its axis, combined
with the revolution of the Earth, causes the
th
different seasons.
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