The transition between the Earth's crust and mantle is known as the Mohorovicic discontinuity, often known as the Moho discontinuity or the Moho.
As you are surely aware, the earth's crust and mantle are separated by the Mohorovicic Discontinuity. It would be constructed of many elements, including oxygen, iron, sodium, silicon, and aluminum. Rocks that make up the Earth's crust and mantle would contain these elements.
The line between the crust and mantle is known as the Mohorovicic Discontinuity or Moho. This barrier is situated at a depth of the Earth's surface of about 2891 kilometers. The discontinuity in seismic wave velocities at that depth allows for the observation of the boundary.
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