the lithosphere is the Earth's crust and the very top of the mantle together
Isostasy theory is a geological concept that posits that Earth's lithosphere is in gravitational equilibrium, with lighter elements floating on top of heavier materials in the mantle. This theory explains how the lithosphere adjusts vertically to maintain balance when weight is added or removed, such as from the melting of ice sheets.
The lithosphere is the rigid outermost layer of Earth, consisting of the crust and upper portion of the mantle. It is divided into several large tectonic plates that float on the semi-fluid asthenosphere beneath.
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.
No, oceanic lithosphere contains more mafic rocks compared to continental lithosphere. Oceanic lithosphere is mainly composed of basalt, which is a mafic rock, whereas continental lithosphere is composed of a variety of rock types, including granitic rocks which are more felsic in composition.
Oceanic lithosphere is denser and cooler than continental lithosphere, making it more prone to subduction. As oceanic lithosphere descends into the mantle at subduction zones, it creates a trench and can trigger volcanic activity. Continental lithosphere, being less dense and thicker, tends to be buoyant and is typically too buoyant to be subducted.
the lithosphere.
The lithosphere is the outermost layer of Earth and includes the crust and part of the upper mantle. It is rigid and divided into tectonic plates that interact and move over the semi-fluid asthenosphere below.
a piece of lithosphere that becomes part of a larger landmass when tectonic plats collide at a convergent boundary
The upper layer of the earth's mantle, below the lithosphere, in which there is relatively low resistance to plastic flow and convection is thought to occur.
The uppermost mantle and the crust makes the lithosphere.
Isostasy theory is a geological concept that posits that Earth's lithosphere is in gravitational equilibrium, with lighter elements floating on top of heavier materials in the mantle. This theory explains how the lithosphere adjusts vertically to maintain balance when weight is added or removed, such as from the melting of ice sheets.
The lithosphere is composed of the crust and uppermost hard, brittle mantle.
The lithosphere is the rigid outermost layer of Earth, consisting of the crust and upper portion of the mantle. It is divided into several large tectonic plates that float on the semi-fluid asthenosphere beneath.
Lithosphere (apex)
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.
Oceanic lithosphere is dense enough to be forced down into the mantle. Continental lithosphere is not.
whats an antonyms for lithosphere