The outer layer of the lithosphere is called the crust. It is divided into two types: continental crust, which forms the landmasses, and oceanic crust, which forms the ocean floors.
The layer above the lithosphere is the Earth's crust, which is divided into the continental crust and the oceanic crust.
lithosphere
Isostasy is the flotational balance achieved between rocks of the crust lithosphere and deeper mantle. This balance is maintained as lighter rocks of the crust "float" on the denser rocks of the mantle below.
There is only a slight difference between crust and lithosphere. The difference is that the lithosphere is part of the Earth that encompasses.
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, (The "gooey" part of the mantel that is between the crust) Is moved by convection currents.
The boundary between the crust and the lithosphere is known as the MohoroviΔiΔ 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 lithosphere is generally thinner under oceanic crust compared to continental crust. Oceanic lithosphere is typically around 5-10 kilometers thick, while continental lithosphere can be up to 200 kilometers thick. This difference is due to variations in temperature and composition between the two types of crust.
the lithosphere and the crust of the earth are the same lithosphere is another word for crust so the thickest is both of them.
The outer layer of the lithosphere is called the crust. It is divided into two types: continental crust, which forms the landmasses, and oceanic crust, which forms the ocean floors.
Yes, the crust of the Earth is part of the lithosphere
The layer above the lithosphere is the Earth's crust, which is divided into the continental crust and the oceanic crust.
The uppermost mantle and the crust makes the lithosphere.
Not exactly. The lithosphere is the crust and the top of the mantle (down to the asthenosphere).
The lithosphere is thicker than the Earth's crust. The lithosphere includes the crust and the upper part of the mantle, typically ranging in thickness from about 100 to 200 kilometers beneath the oceanic crust and up to 250 kilometers beneath continental crust.
The lithosphere and the crust are both parts of the Earth's outermost layer, but the lithosphere includes the crust and the uppermost part of the mantle. The crust is the solid, outermost layer of the Earth's surface, while the lithosphere is defined by its rigid behavior and consists of the crust and a portion of the upper mantle.