- The Earth formed billions of years ago. : āĻĒā§āĻĨāĻŋā§ąā§ āĻā§āĻāĻŋ āĻā§āĻāĻŋ āĻŦāĻā§° āĻāĻāϤ⧠āĻāĻ āύ āĻšā§āĻāĻŋāϞāĨ¤
- A large amount of heat was trapped during its formation. : āĻāĻ āύ āĻšā§ā§ąāĻžā§° āϏāĻŽāϝāĻŧāϤ āĻŦāĻšā§āϤ āϤāĻžāĻĒ āĻāĻŋāϤ⧰āϤ āϧ⧰āĻŋ āĻĨāĻžāĻāĻŋāϞāĨ¤
- Heavy elements sank toward the center of the Earth's core. : āĻāĻžā§°ā§ āĻāĻĒāĻžāĻĻāĻžāύāϏāĻŽā§āĻš āĻĒā§āĻĨāĻŋā§ąā§ā§° āĻā§āύā§āĻĻā§ā§°ā§° āĻĢāĻžāϞ⧠āύāĻžāĻŽāĻŋ āĻ’āϞāĨ¤
- This sinking created more heat due to strong pressure. : āĻāĻ āύāĻžāĻŽāĻžā§° āĻĢāϞāϤ āĻ
āϧāĻŋāĻ āĻāĻžāĻĒā§° āĻŦāĻžāĻŦā§ āĻā§°ā§ āϤāĻžāĻĒ āĻā§āĻĒāύā§āύ āĻšāϞāĨ¤
- Radioactive elements release energy inside Earth. : āĻāĻŋāϤ⧰āϤ āĻĨāĻāĻž āϤā§āĻāϏā§āĻā§ā§°āĻŋāϝāĻŧ āĻāĻĒāĻžāĻĻāĻžāύāĻŦā§ā§°ā§ āĻļāĻā§āϤāĻŋ āĻŽā§āĻāϞāĻŋ āĻā§°ā§āĨ¤
- This energy keeps the core extremely hot. : āĻāĻ āĻļāĻā§āϤāĻŋā§° āĻŦāĻžāĻŦā§ āĻĒā§āĻĨāĻŋā§ąā§ā§° āĻā§āύā§āĻĻā§ā§° āϏāĻĻāĻžāϝāĻŧ āĻŦāĻšā§āϤ āĻā§°āĻŽ āĻĨāĻžāĻā§āĨ¤

Key Point: Earth’s core remains hot because of heat trapped during formation and energy released by radioactive elements.
āĻĒā§āĻĨāĻŋā§ąā§ā§° āĻāĻ āύāĻāĻžāϞā§āύ āϤāĻžāĻĒ āĻā§°ā§ āϤā§āĻāϏā§āĻā§ā§°āĻŋāϝāĻŧ āĻāĻĒāĻžāĻĻāĻžāύ⧰ āĻĒā§°āĻž āĻŽā§āĻā§āϤ āĻļāĻā§āϤāĻŋā§° āĻŦāĻžāĻŦā§ āĻĒā§āĻĨāĻŋā§ąā§ā§° āĻā§āύā§āĻĻā§ā§° āĻŦāĻšā§āϤ āĻā§°āĻŽ āĻĨāĻžāĻā§āĨ¤