There are several lines of evidence that suggest the interior of the Earth is hot. Here are two key pieces of evidence:
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Geothermal Gradient: The geothermal gradient is the rate at which temperature increases with depth below the Earth's surface. Typically, the temperature rises by about 25 to 30 degrees Celsius for every kilometer of depth in the crust. In some regions, this gradient can be even higher, indicating that the deeper you go, the hotter it gets. This consistent increase in temperature supports the idea that the Earth's interior is considerably hot.
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Volcanic Activity: The presence of volcanic activity provides clear evidence of the heat within the Earth's interior. When magma, which is molten rock, rises from deep within the Earth to the surface, it indicates that there are high temperatures prevalent in the mantle and the lower crust. The occurrence of geothermal features such as hot springs and geysers further underscores the heat emanating from beneath the Earth's surface.
Together, these pieces of evidence support the conclusion that the Earth's interior is indeed hot.