What is the Mohorovicic discontinuity and where is it found?
The Mohorovicic Discontinuity or "Moho" is the boundary between the cryst and the mantle. It lies on average 30-50 km below the surface on cobtinents, but 5-10 km under the oceans.
Here is a map showing the crustal depth down to the Moho: https://tutor.hix.ai
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The Moho, also called the Mohorovičić discontinuity, is the line that separates the Earth's crust from the underlying mantle. It is located below the surface of the Earth, usually between 5 and 70 kilometers (3 and 43 miles) below the continents and between 5 and 10 kilometers (3 and 6 miles) below the ocean floors.
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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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