When the weight of an area of Earth's crust increases, the lithosphere tends to sink or subside due to the added pressure. This process is part of isostasy, where the lithosphere adjusts to changes in surface load. Conversely, if weight is removed, the lithosphere may rebound or uplift over time. This dynamic balance is essential for understanding geological processes such as mountain formation and erosion.
it is the lithosphere
When the weight of an area of Earth's crust increases, such as through sediment accumulation or glacial formation, the lithosphere can experience a process called subsidence, where it sinks deeper into the underlying asthenosphere. This occurs because the added weight causes the lithosphere to deform and sink due to isostatic adjustments. Conversely, if the weight is removed, such as through melting glaciers, the lithosphere can rebound and rise, a process known as isostatic rebound. This dynamic balance of forces is essential for understanding geological processes and landscape changes over time.
It is called the lithosphere.
I'm studying the earths layers and it's right after the lithosphere which is right underneath the crust I'm studying the earths layers and it's right after the lithosphere which is right underneath the crust I'm studying the earths layers and it's right after the lithosphere which is right underneath the crust
The Earth's crust and the uppermost part of the mantle together form the lithosphere. The lithosphere is a rigid outer layer of the Earth that is divided into tectonic plates which float on the semi-fluid asthenosphere beneath them.
the lithosphere and the crust of the earth are the same lithosphere is another word for crust so the thickest is both of them.
lithosphere.
The lithosphere crust
The lithosphere.
it is the lithosphere
When the weight of an area of Earth's crust increases, such as through sediment accumulation or glacial formation, the lithosphere can experience a process called subsidence, where it sinks deeper into the underlying asthenosphere. This occurs because the added weight causes the lithosphere to deform and sink due to isostatic adjustments. Conversely, if the weight is removed, such as through melting glaciers, the lithosphere can rebound and rise, a process known as isostatic rebound. This dynamic balance of forces is essential for understanding geological processes and landscape changes over time.
crust and upper mantle
The Lithosphere. (Earths Crust).
the mantle also known as the athenosphere the crust is also known as the lithosphere
The lithosphere is composed of the hard and brittle outer shell of the Earth consisting of the crust and the uppermost mantle.
Troposphere: nitrogen Lithosphere and hydrosphere: oxygen
how is the earths crust related to the lithosphere