How does temperature change as depth increases within the earth?
As you head toward the center of the Earth, temperatures increase exponentially.
The Earth’s core is a sphere of molten nickel and iron. Now just think about how hot it has to be to melt iron, let alone for the iron to remain melted. The center of the Earth is almost as hot as the surface of the sun as new studies show, a blistering 10800 degrees Fahrenheit, approximately 5982 degrees Celsius.
As you move further and further away from the core, the crust cools to much colder temperatures all the way up to the surface.
The Earth gets hotter as you move towards to center.
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As depth increases within the Earth, temperature generally increases. This phenomenon is known as the geothermal gradient. The Earth's interior is heated primarily by the decay of radioactive isotopes and residual heat from its formation. As you move deeper into the Earth, the heat from these sources becomes more concentrated, causing temperatures to rise. On average, the geothermal gradient is about 25-30 degrees Celsius per kilometer of depth. However, local variations in geology and tectonic activity can lead to deviations from this average gradient.
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When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
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