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.
isostatic equilibrium
isostatic is also known as isometric stretching and it is used to help increase flexibility by elongating your muscles
H. V. Atkinson has written: 'Hot isostatic processing' -- subject(s): Isostatic pressing
isostatic is also known as isometric stretching and it is used to help increase flexibility by elongating your muscles
Gravity
As these isostatic adjustment occur, areas of the crust are bent up and down. This bending cause rock in that area to deform.
Gravity
they happen because of isostatic adjustment
Gravity.
Yes.
Isostasy refers to the balance between the Earth's lithosphere (outermost layer) and asthenosphere (plastic layer below). When the lithosphere undergoes stress, such as due to tectonic forces, it can become imbalanced and adjust to achieve equilibrium. During this adjustment process, known as isostatic readjustment, earthquakes can occur as the rocks rupture and release built-up energy. Hence, isostasy can be a contributing factor to the occurrence of earthquakes.