The crust is part of the lithosphere, so there is no boundary between them. There is a boundary between the crust and the other part of the lithosphere which is the uppermost mantle. It is called the Mohorovicic Discontinuity or the 'Moho' for short.
The boundary between continental crust and oceanic crust occurs at the base of the lithosphere. This boundary is known as the Mohorovičić discontinuity, or Moho. It separates the less dense continental crust from the more dense oceanic crust below.
You would draw the line at the base of the lithosphere, which is the boundary between the lithosphere and the asthenosphere. This boundary is located around 100-200 kilometers below the Earth's surface and marks the point where the rigid lithosphere transitions to the more ductile asthenosphere.
I would draw the line at the base of the lithosphere, which is known as the lithosphere-asthenosphere boundary. This boundary separates the rigid lithosphere from the more plastic asthenosphere below it.
The Moho separates the crust and the mantle.
The lithosphere is part of the Earth's crust and uppermost mantle; it includes the crust itself. So, the distance to the lithosphere is essentially the same as the thickness of the crust, which varies from about 5 to 75 kilometers (3 to 46 miles) beneath the oceans and continents.
The boundary between the asthenosphere and the lithosphere is normally below the Moho (which marks the boundary between the crust and the mantle). The exception to this is below mid-ocean ridges where the moho and the lithosphere / asthenosphere boundary are at the same depth.
The boundary between continental crust and oceanic crust occurs at the base of the lithosphere. This boundary is known as the Mohorovičić discontinuity, or Moho. It separates the less dense continental crust from the more dense oceanic crust below.
You would draw the line at the base of the lithosphere, which is the boundary between the lithosphere and the asthenosphere. This boundary is located around 100-200 kilometers below the Earth's surface and marks the point where the rigid lithosphere transitions to the more ductile asthenosphere.
I would draw the line at the base of the lithosphere, which is known as the lithosphere-asthenosphere boundary. This boundary separates the rigid lithosphere from the more plastic asthenosphere below it.
The Moho separates the crust and the mantle.
The lithosphere is part of the Earth's crust and uppermost mantle; it includes the crust itself. So, the distance to the lithosphere is essentially the same as the thickness of the crust, which varies from about 5 to 75 kilometers (3 to 46 miles) beneath the oceans and continents.
Divergent
The crust is the outermost layer of the Earth, while the lithosphere is a combination of the crust and uppermost part of the mantle. The lithosphere includes the crust and behaves as a rigid outer shell that is divided into tectonic plates.
A diverging boundary results in the separation of tectonic plates, leading to the creation of new crust through seafloor spreading. Magma rises to fill the gap between the plates, solidifies, and becomes part of the oceanic crust. This process contributes to the continuous renewal and expansion of the Earth's lithosphere.
The upper mantle and the lower mantle.
The lithosphere, (The "gooey" part of the mantel that is between the crust) Is moved by convection currents.
This is known as the Mohorovičić discontinuity. This is often shortened to Moho. It was one of the first 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.