isokinetic exercises: exercises with special machines that allow for the maximum resistance over the complete range of motion.
A prefix for "pert" is "im-," which changes the meaning to "impertinent."
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.
The prefix for the word "tolerant" is "in-" which changes the meaning to "intolerant."
A prefix for "common" is "un-". When added to "common," it changes the meaning to "uncommon," which indicates something that is not ordinary or usual. Prefixes are morphemes added to the beginning of a word to modify its meaning.
Adding the prefix "over-" to the word "priced" changes the meaning of the word to "priced higher than usual or beyond reasonable value".
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.
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.
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.
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.
An isostatic is something that pertains to or is characterized by isostasy. Isostasy is the equilibrium of the Earths crust.
isostatic is also known as isometric stretching and it is used to help increase flexibility by elongating your muscles
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.
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 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
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.