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High geothermal activity and high heat flow at shallow levels in the crust are most likely due to aqueous fluids.
Alternatively, the present-day geothermal gradient may be lower than that used in calculating the profile.
Water as hot as 380°C gushes out of geothermal springs along the spreading centers.
On Earth, microbes can derive energy from sources other than the sun, such as chemical and geothermal energy from hydrothermal vents.
The internal, or geothermal , heat from within the Earth is responsible for the fact that temperature increases with depth.
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