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High temperatures inside the Earth form magma, which is molten rock beneath the Earth's surface. As the magma rises towards the surface, it can lead to volcanic eruptions and the formation of new land features like mountains, volcanoes, and oceanic ridges.
High temperatures inside the Earth can lead to the formation of molten rock, known as magma. This molten rock can rise to the surface and form volcanic activity, such as volcanic eruptions and lava flows. It can also form igneous rocks when it cools and solidifies.
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Deep in the Earth is where minerals form. This causes high pressure and temperatures.
Different temperatures inside the Earth lead to the formation of various structures, such as magma chambers where molten rock accumulates, as well as crystal growth in minerals under high temperatures and pressures. Additionally, temperature variations can cause thermal expansion and contraction, leading to the formation of fractures and faults within the Earth's crust.
The Earth is hot inside because of the heat left over from its formation over 4.5 billion years ago, as well as heat produced by radioactive decay of elements in the Earth's core. This heat is trapped and unable to escape, leading to high temperatures deep within the Earth.
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Earth's outer core is in liquid form because of the high temperatures and pressures deep within the planet. The intense heat from the Earth's core keeps the outer core in a molten state, allowing it to flow like a liquid.
Rocks inside earth are constantly melting and solidifying, when rocks are heated to high temperatures between (6250C and 1200OC),it melts into magma.