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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.
thinner and denser
I believe this would be the oceanic crust
it show 8km is oceanic crust and 40km is continental crust
The temperature increases. The average geothermal gradient is 25C/Km
Varies obviously, but the average geothermal gradient in the Earth's continental crust is 25 degrees Centigrade/kilometre
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.
oceanic crust
thinner and denser
Oceanic crust is more dense.
because the oceanic crust lithospher descend into the mantle at the subduction zone .it will be taken to increasing higher temperature as it get deeper
Oceanic
Oceanic crust, new oceanic crust is produced by seafloor spreading.
The oceanic plate is made of denser (and thinner) rock than the continental crust, so the oceanic plate gets subducted (pushed underneath) where it descends and gets melted by geothermal heat.
people dont use geothermal it is in the earths crust so people dont use geothermal
Geothermal energy is from heated water within the earth's crust.
one and a half miles thick