Temperature increases as you go deeper inside Earth, with the highest temperatures ocurring in the core.
The temperature of Earth's crust is much lower than the temperature of Earth's interior. The temperature of Earth's crust generally ranges from about 0°C to 30°C, while the temperature of Earth's interior can reach thousands of degrees Celsius in the mantle and core. The higher temperatures in the interior are due to the heat generated by radioactive decay and leftover heat from Earth's formation.
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The constant interaction between rocks and external forces like weathering, erosion, and tectonic activity can change the Earth's surface. However, the fundamental composition and structure of rocks themselves cannot be changed by external forces other than extreme conditions like high pressure and temperature in the Earth's interior.
Scientists study Earth's interior to better understand the planet's composition, structure, and dynamics. This helps in predicting natural disasters like earthquakes and volcanic eruptions, as well as in understanding processes like plate tectonics and magnetic field generation. Studying the Earth's interior also provides insights into the planet's history and evolution.
it depends on the deepth
As you go deeper and deeper the layers will start to get hotter and thicker.
it depends on the deepth
it depends on the deepth
Depth, temperature and pressure barrier.
radioactive decay
The earths interior is cold
temperature increases with depth
The temperature of Earth's crust is much lower than the temperature of Earth's interior. The temperature of Earth's crust generally ranges from about 0°C to 30°C, while the temperature of Earth's interior can reach thousands of degrees Celsius in the mantle and core. The higher temperatures in the interior are due to the heat generated by radioactive decay and leftover heat from Earth's formation.
highest near equator
A body wave is a seismic wave that travels through Earths interior.
outer core; Earth Science Reference Tables page 10