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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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∙ 14y ago
Isostatic changes refer to adjustments in the Earth's crust in response to changes in surface loads, such as the melting of ice caps or the deposition of sediments. These adjustments involve the uplifting or sinking of land masses to achieve equilibrium between the weight of the surface mass and the buoyancy of the underlying mantle.
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What is a prefix for pert?
A prefix for "pert" is "im-," which changes the meaning to "impertinent."
What prefix will change the meaning of text to an underlying meaning?
The prefix "sub-" changes the meaning of "text" to represent an underlying meaning, as in subtext, which refers to the underlying or implied message in written or spoken communication.
What is the prefix for the word tolerant?
The prefix for the word "tolerant" is "in-" which changes the meaning to "intolerant."
Adding the prefix over- to the word priced changes the meaning of the word to?
Adding the prefix "over-" to the word "priced" changes the meaning of the word to "priced higher than usual or beyond reasonable value".
What is a word or phrase that limits or changes the meaning of another word or phrase?
A modifier is a word or phrase that limits or changes the meaning of another word or phrase. It can include adjectives, adverbs, modal verbs, or phrases like "in addition to" or "on the other hand".
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.
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 force controls the isostatic adjustment of Earth?
Gravity
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 has the author H V Atkinson written?
H. V. Atkinson has written: 'Hot isostatic processing' -- subject(s): Isostatic pressing
Isostatic stretching refers to?
isostatic is also known as isometric stretching and it is used to help increase flexibility by elongating your muscles
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.
What continental motion is caused by isostasy?
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.
What force works against isostatic adjustment?
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.
