The boundary between the crust and the lithosphere is known as the Mohorovičić discontinuity or Moho. It is typically located at an average depth of about 5 to 10 kilometers beneath the ocean floor and 20 to 90 kilometers beneath the continents. The Moho marks the transition from the less dense crust to the denser upper mantle.
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 discontinuity separates the Earth's crust from the underlying mantle. This boundary is located between the crust and the uppermost part of the mantle known as the lithosphere.
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 lithosphere-asthenosphere boundary is located below the Moho discontinuity. The lithosphere is the rigid outer layer of the Earth, which includes the crust and the uppermost part of the mantle. The asthenosphere is a semi-fluid layer beneath the lithosphere where the rock is more ductile and capable of flow.
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 discontinuity separates the Earth's crust from the underlying mantle. This boundary is located between the crust and the uppermost part of the mantle known as the lithosphere.
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
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 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.
The upper mantle and the lower mantle.
The boundary between the crust and the mantle is called the Mohorovičić discontinuity, or the Moho for short. This is where seismic waves change in velocity, indicating the transition between the Earth's crust and mantle.
The lithosphere, (The "gooey" part of the mantel that is between the crust) Is moved by convection currents.