The boundary between the crust and the mantle is called the Mohorovicic discontinuity. It is also called simply the Moho and it is the abrupt divide between faster and slower speeds where the mantle starts.
The boundary between the Earth's core and mantle is rather unimaginatively titled the Core-Mantle Boundary (CMB). The very base of the mantle (bottom 200 km) is sometimes considered a transition zone between core and mantle that is known as the D'' (D double prime) layer. The top of this layer is marked by a strong seismic discontinuity known as the Gutenberg discontinuity.
The upper boundary of the the mantle that separates the mantle from the crust is commonly referred to as the Moho (or to give it it's full title, the Mohorovičić discontinuity) named after the Croatian seismologist who discovered it.
It's called "Moho" for short, the Mohorovicic discontinuity.
Upper mantle
hotspots
Crust Mantle Outer Core Inner Core
It is called the lithosphere.
peninsala
The name of the element magnesium was derived from Magnesia which is a Greek district in Thessaly. This metallic element is one of the most abundant elements on Earth and makes up a huge portion of its mantle.
toponym.
This is known as the Asthenospehere.
The metosphere is the name of the mantle
The mantle
hotspots
hotspots
The lithosphere.
crust athenisphere mantle outer core innercore
The lithosphere.
Crust Mantle Outer Core Inner Core
The mantle
It is called the lithosphere.