There are 3 energy sources for earth; solar, accretion/diffusion, and radioactive decay.
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There are 3 energy sources for earth; solar, accretion/diffusion, and radioactive decay. Accretion/diffusion was an important energy source in the early Earth, but it doesn't release almost any energy anymore. The reason the planet core stays warm is primarily due to radioactive decay now.
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There are 3 energy sources for earth; solar, accretion/diffusion, and radioactive decay. Accretion/diffusion was an important energy source in the early Earth, but it doesn't release almost any energy anymore. The reason the planet core stays warm is primarily due to radioactive decay now.
you forgot tidal power (from the moon)
also geothermal is about 20% heat from when the earth formed and about 80% continuous decay of radioactive materials. (This means that the planet's core cools down so slowly that it's still hot inside from when it formed) https://en.wikipedia.org/wiki/Geothermal_energy#Resources
Outside of the seasonal variations, the geothermal gradient of temperatures through the crust is 25–30 °C (77–86 °F) per km of depth in most of the world. The conductive heat flux averages 0.1 MW/km2. These values are much higher near tectonic plate boundaries where the crust is thinner. They may be further augmented by combinations of fluid circulation, either through magma conduits, hot springs, hydrothermal circulation.
That means 0.1 W/m² of heat on the surface of earth comes from the inside of earth, meanwhile the solar irradiation constant is 1361 W/m², while actually only about 200 W/m² reach the surface on average if you account for day-night-cycles (30% efficiency) and weather patterns (clouds reflect light, 50% efficiency). So geothermal makes about 0.05% of the energy that reaches the surface of earth.
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