In geology, geothermal refers to heat sources within the planet. Strictly speaking, geo-thermal necessarily refers to the Earth but the concept may be applied to other planets.
The planet's internal heat was originally generated during its accretion, due to gravitational binding energy, and since then additional heat has continued to be generated by the radioactive decay of elements such as uranium, thorium, and potassium. The heat flow from the interior to the surface is only 1/20,000 as great as the energy received from the Sun.
Temperature within the Earth increases with increasing depth. Highly viscous or partially molten rock at temperatures between 1,200 and 2,200°F (650 to 1,200°C) is postulated to exist everywhere beneath the Earth's surface at depths of 50 to 60 miles (80 to 100 kilometers), and the temperature at the Earth's center, nearly 4,000 miles (6,400 kilometers) deep, is estimated to be 5650 ± 600 kelvins [http://www.carnegieinstitution.org/news_010905.html.
Geothermal heat at the surface is highly concentrated where magma is close to the surface. This primarily occurs in volcanic and hotspot areas and at spreading ridge areas.
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