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The sometimes magnesium rich Mohorovi?i? discontinuity, which often is called simply 'Moho', separates the earth's crust and the cooler part of the planet's mantle.

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The sometimes magnesium rich Mohorovi?i? discontinuity, which often is called simply 'Moho', separates the earth's crust and the cooler part of the planet's mantle.

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A vertical asymptote can be, but need not be a discontinuity. In simple terms, the distinction depends whether the domain extends on only one side of the (no discontinuity) or both sides (infinite discontinuity).

For example, there is no discontinuity in f(x) = 1/x for x > 0

On the other hand, f(x) = 1/x for x ≠ 0 has an infinite discontinuity at x = 0.

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The zone of discontinuity in the density between mantle and core is known as gutenburg discontinuity.

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It is called the Mohorovičić discontinuity or the Moho for short.

It was one of the fist features of the Earth's interior that was discovered using seismic waves. In 1909, Andrija Mohorovicic discovered this boundary and it was named in his honor.

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The Discontinuity Guide was created in 1995.

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