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isokinetic exercises: exercises with special machines that allow for the maximum resistance over the complete range of motion.

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How do isostatic adjustments affect isostacy?

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.


What force controls the isostatic adjustment of Earth?

Gravity


Why isostatic rebound slows down over time?

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.


What triggers isostatic subsidence?

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.


What processes could cause isostatic adjustments of continents?

Isostatic adjustments of continents can be caused by the movement of tectonic plates, volcanic activity, erosion, and deposition of sediment. These processes can result in changes in the elevation and shape of continents over long periods of time as the Earth's crust responds to changes in the distribution of mass.


What is the definition of isostatic?

An isostatic is something that pertains to or is characterized by isostasy. Isostasy is the equilibrium of the Earths crust.


What is isostatic?

isostatic is also known as isometric stretching and it is used to help increase flexibility by elongating your muscles


What is an isostatic rebound?

Isostatic rebound, also known as isostatic adjustment or post-glacial rebound, refers to the process by which the Earth's crust rises after being depressed by the weight of glaciers or ice sheets. When these massive ice formations melt, the reduced pressure allows the crust to gradually adjust and rise back to its original elevation. This phenomenon can occur over thousands of years and is influenced by factors like the viscosity of the mantle and the rate of ice melt. Isostatic rebound is a key aspect of understanding geological and environmental changes following the last Ice Age.


What is isostatic recovery?

Isostatic recovery refers to the process by which the Earth's crust gradually adjusts and rebounds after being subjected to the weight of ice sheets or sediment. When these massive loads are removed, such as during glacial melting, the crust experiences a slow uplift as it seeks to reach a state of equilibrium. This phenomenon is a response to changes in pressure and can take thousands of years to fully manifest. Isostatic recovery is an important factor in understanding geological processes and the long-term evolution of landscapes.


Isostatic stretching refers to?

isostatic is also known as isometric stretching and it is used to help increase flexibility by elongating your muscles


What has the author H V Atkinson written?

H. V. Atkinson has written: 'Hot isostatic processing' -- subject(s): Isostatic pressing


How wounld a period of major erosion affect the isostatic adjustment of a mountain range?

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.