New oceanic lithosphere is constantly being produced at mid-ocean ridges and is recycled back to the mantle at subduction zones.
The Lithosphere has 3 layers. The first one being the Crust, the second layer is called the Mantle and third is known as the Core.
The difference between the core and the lithosphere is the core is on the top of the lithosphere and the lithosphere is on the bottom of the core
lithosphere.
division of lithosphere
The crust and the upper mantle are a geological part of the earth called the lithosphere. There are 2 parts of the lithosphere: the oceanic lithosphere, which is made up of land underneath water, and the continental lithosphere, which is the the part made of just land. The lithosphere lies on top of the asthenosphere. The lithosphere is made up of tectonic plates, which are pieces of land floating on the lithosphere.
New lithosphere is constantly being produced at the oceanic ridges. Lithosphere is consumed at the subduction zones. A balance is maintained because older, denser proportions of oceanic lithosphere descend into the mantle at a rate equal to seafloor production.
85 percent of fossil fuel is being consumed today
Petroleum oil from the lithosphere of the earth is being consumed at a significantly faster rate than it is being produced. From that standpoint, NO, it is NOT sustainable. On the other hand, a number of processes have been developed to produce the same mixture of molecules from sustainable sources (e.g. biodiesel) so oil in general CAN be sustainable if we do not rely strictly on drilling to produce it.
The planet is ripped to shreds and completely vaporizes before being sucked in, it has no surface when it is being consumed.
The Lithosphere has 3 layers. The first one being the Crust, the second layer is called the Mantle and third is known as the Core.
enzymes are never consumed in a chemical reaction, therefore the answer to your question is that enzymes that affect the speed of a chemical reaction without being consumed are indeed called enzymes.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
The uppermost mantle and the crust makes the lithosphere.
The difference between the core and the lithosphere is the core is on the top of the lithosphere and the lithosphere is on the bottom of the core
The lithosphere is composed of the crust and uppermost hard, brittle mantle.
lithosphere.
division of lithosphere