isostatic equilibrium
The balance between the lithosphere and asthenosphere is described by isostasy, which refers to the gravitational equilibrium between the Earth's crust (lithosphere) and the underlying mantle (asthenosphere). The lithosphere, being more rigid and less dense, floats on the semi-fluid asthenosphere, which allows it to adjust in response to changes in surface load, such as erosion or glaciation. This dynamic balance ensures that the lithosphere remains buoyant, maintaining stability in the Earth's topography over geological timescales.
The force responsible for the Earth's crust and lithosphere floating on the mantle is isostasy. Isostasy is a balancing act between the buoyant force of the lithosphere on the denser, more fluid asthenosphere below it. This balance helps maintain the equilibrium of the Earth's crust.
Hydrosphere - water Lithosphere - land So far, that's all I can say.
There is only a slight difference between crust and lithosphere. The difference is that the lithosphere is part of the Earth that encompasses.
lithosphere
Isostasy is the balance between the buoyant force of the lithosphere floating on the denser underlying mantle and the gravitational force pulling the lithosphere downwards.
Isostasy is the balance between the buoyant force of the mantle pushing up on the lithosphere and the gravitational force pulling the lithosphere downward. This balance helps maintain the equilibrium of the Earth's crust.
Isostasy. It refers to the equilibrium between the weight of Earth's lithosphere (which includes the continents) and the buoyant force exerted by the asthenosphere below, which causes the lithosphere to float.
a balance achieved between two desirable but incompatible features; a compromise
In any market, equilibrium is achieved when the level of demand is equal to level of supply. This means that there is a perfect balance between the two variables.
The process of plate tectonics drives the creation and destruction of lithosphere. As new lithosphere is formed at mid-ocean ridges through seafloor spreading, older lithosphere is consumed at subduction zones, creating a balance between formation and destruction over time. This equilibrium maintains a relatively constant amount of lithosphere on Earth.
I'll give it a shot The way I read this is that when darkness is made light strength is given by the light and the balance between light and dark is achieved. This is what life strives for is that balance.
It would be referred to as equilibrium. It has never, nor will it ever, be completely achieved.
The force responsible for the Earth's crust and lithosphere floating on the mantle is isostasy. Isostasy is a balancing act between the buoyant force of the lithosphere on the denser, more fluid asthenosphere below it. This balance helps maintain the equilibrium of the Earth's crust.
The lithosphere, (The "gooey" part of the mantel that is between the crust) Is moved by convection currents.
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.
Isostasy involves the balance between the downward force of gravity acting on the lithosphere and the buoyant force exerted by the asthenosphere below. This balance determines the level of the Earth's crust in response to variations in crustal thickness and density.