Isostatic equilibrium is the balance between Earth's crust and the layer of mantle it floats on. The denser the crust is, the more it sinks into the mantle. Equilibrium is achieved when the crust floats at a certain level in the mantle.
Equilibrium can mean a state in which opposing forces or influences are balanced. Examples are, to trip and fall over is to lose your equilibrium. To stumble but recover is to regain your equilibrium.A market is in equilibrium when supply and demand are matched and prices stable.
The internal equilibrium is a balance condition between internal forces and the commulative integrated stresses.
That is the correct spelling of "dynamic equilibrium" (state of balanced gain and loss resulting in no net change).
The equilibrium price refers to the price point at which supply and demand are equal. This price can be found by applying the three basic properties of equilibrium.
Equilibrium ,
An isostatic is something that pertains to or is characterized by isostasy. Isostasy is the equilibrium of the Earths crust.
The force that works against isostatic adjustment is typically referred to as tectonic forces. These forces include compression, extension, and shear created by the movement of tectonic plates. These forces can cause the crust to deform and adjust, disrupting the isostatic equilibrium.
Isostatic adjustments refer to the process where Earth's lithosphere changes in response to the addition or removal of mass on its surface. This can lead to isostasy, which is the balancing of the lithosphere on the denser underlying mantle. Isostatic adjustments can cause the lithosphere to either rise or sink to achieve isostatic equilibrium.
Isostatic subsidence is triggered by changes in the weight or mass of the Earth's crust, such as the removal of a heavy load of ice or sediment. This removal causes the crust to slowly adjust to achieve equilibrium, leading to subsidence.
Gravity
Isostatic rebound slows down over time as the earth's crust reaches a state of isostatic equilibrium where it is balanced with the underlying mantle. As the crust continues to adjust to changes in mass distribution, the rate of rebound gradually decelerates until it eventually stabilizes.
The crust adjusts to gravity by settling into a state of isostatic equilibrium. This means that the crust will rise or sink to achieve balance between the forces of gravity pulling it down and the buoyant forces pushing it up. Isostatic adjustment can lead to phenomena like mountain building and subsidence over geologic time scales.
Isostatic adjustment will cause the crust beneath the volcanic mountain range to gradually sink due to the weight of the mountains. This sinking is a response to the added load of the mountains and helps to maintain equilibrium in the Earth's crust.
Isostasy can cause continental uplift or subsidence depending on changes in crustal thickness and density. When weight is added to the crust, such as by mountain building or erosion, the crust can adjust by uplifting or sinking to maintain gravitational equilibrium. This vertical movement of the crust due to isostasy is known as isostatic rebound or isostatic subsidence.
Isostatic adjustment is the process by which the Earth's crust responds to changes in surface loads by rising or sinking to achieve equilibrium. It involves vertical movement of the crust to balance the weight of material on the surface, such as ice sheets or mountain ranges, in order to maintain gravitational equilibrium.
A period of major erosion can lead to the removal of significant mass from a mountain range, causing it to rebound or rise due to isostatic adjustment. This adjustment occurs as the lithosphere beneath the mountain range readjusts to achieve equilibrium with the reduced load on top. Over time, the mountain range may experience changes in elevation and shape as a result of this isostatic adjustment process.
isostatic is also known as isometric stretching and it is used to help increase flexibility by elongating your muscles