They can occur anywhere between the Earth's surface; about 700 kilometers<span> below the surface.</span>
The heat that remains inside the Earth from its creation and radioactive decay are its main heat sources.
The deep earth receives heat from three main sources: (1) heat left over from the planet's formation and accretion, (2) frictional heating brought on by denser core material sinking to the planet's centre, and (3) heat from radioactive element decay.
The energy produced when unstable atoms decay is known as radioactivity, and it is a substantial contributor to the Earth's heat. The main source are the radioactive isotopes of uranium-235 (235U), uranium-238 (238U), potassium-40 (40K), and thorium-232 (232Th) in the Earth's mantle.
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Answer:
To put it simply, Bangladesh is half an hour ahead of India because the sun rises half an hour earlier in Bangladesh than it does in the Indian standard time zone (IST). If IST were situated in Assam, both India and Bangladesh would have the same time.
Explanation:
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