Varies obviously, but the average geothermal gradient in the Earth's continental crust is 25 degrees Centigrade/kilometre
continental crust
Geothermal energy is from heated water within the earth's crust.
it has been washed into the oceans as the continental crust has eroded.
The increase in temperature with depth in the Earth is known as the geothermal gradient. It typically averages about 25 to 30 degrees Celsius per kilometer of depth in the crust, although this can vary based on geological conditions. The geothermal gradient is important for understanding heat flow, geological processes, and the potential for geothermal energy resources.
it can be used for power, like geothermal
continental crust
Geothermal energy is from heated water within the earth's crust.
The geothermal gradient in the Earth's oceanic crust is around 25-30°C per kilometer depth. This means that the temperature increases by about 25-30 degrees Celsius for every kilometer of depth below the seafloor in oceanic crust.
people dont use geothermal it is in the earths crust so people dont use geothermal
The term for the increase in temperature with depth in the Earth is called geothermal gradient. This gradient is typically around 25-30°C per kilometer in the Earth's crust.
continental crust
Water
geothermal starts at the outer edge of the earth's crust and gets hotter the deeper you go. The gradual increase in the temperature as the depth increases is called the geothermal gradient. As you proceed through the crust the gradient is gradual. When you break through the upper mantle the temps then rise almost exponentially.
The average geothermal gradient is around 25 to 30 degrees Celsius per kilometer of depth in the Earth's crust. This means that the temperature increases by this amount for every kilometer you descend into the Earth.
The continental crust is about 25 to 70 kilometers thick. The average is about 50 kilometers.
rejuvenated
well, to be technical the earths crust is really on the inner outside