In the earth's structure, what is the name for the sharp boundary between the crust and the mantle?
The sharp boundary between the Earth's crust and the underlying mantle is called the "Mohorovičić discontinuity," often referred to as the "Moho" for short. This boundary represents a significant change in seismic wave velocities, indicating the transition from the relatively brittle and solid crust to the hotter and more ductile mantle beneath. The Moho is an important feature in understanding the Earth's internal structure and the division between its outermost layer and the layer below.