Press the block down and let go. apex
Earth's crust- apex (:
press the block down and let go
because elasticity of clay is very small, so when reaction of wall acts on the clay, clay cannot withheld the force and it deforms
(Potential) energy is directly proportional to the release height.
bounce and rebound against each other with a velocity dependent on the temperature.
To strike or thump, so as to rebound, or to make a sudden noise; a knock loudly., To leap or spring suddenly or unceremoniously; to bound; as, she bounced into the room., To boast; to talk big; to bluster., To drive against anything suddenly and violently; to bump; to thump., To cause to bound or rebound; sometimes, to toss., To eject violently, as from a room; to discharge unceremoniously, as from employment., To bully; to scold., A sudden leap or bound; a rebound., A heavy, sudden, and often noisy, blow or thump., An explosion, or the noise of one., Bluster; brag; untruthful boasting; audacious exaggeration; an impudent lie; a bouncer., A dogfish of Europe (Scyllium catulus)., With a sudden leap; suddenly.
Assuming the ball doesn't rebound: The energy is dissipated. That means it is spread out, as unusable forms of energy; most of it will heat the ball and the ground.
Post-glacial rebound (sometimes called continental rebound, glacial isostasy, glacial isostatic adjustment) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period, through a process known as isostasy.
it is called rebound.
Isostasy
Isostatic rebound.
The crust will rebound. (uplift will occur)
I am here because i googled this same question, but i think i have a hypothesis of my own, which would be that yes it should stop eventually. There are vast areas of the Earth that have no area of isostatic activity - check out the wikipedia on post glacial rebound and there is a map that shows regions. I would imagine that this since this is an energy state issue , balancing with gravity, that the system would tend to settle as soon as possible. If we look at varying geologic areas effected by isostatic rebound it seems like they occur, in then remain static. iso static , a series of teeter-totter weights and balances, on the surface of the crust.
Isostatic rebound. love ya Geography Questions.
isostatic rebound
The removal of the load causes something known as glacial isostatic rebound. The weight of the glacier causes the earth's lithosphere to deform (it squashes it). When the glacier retreats and the load is removed, the earth's lithosphere springs back to its original shape.
They are experiencing isostatic rebound, a rise in elevation due to the release of downward pressure from the exited ice.
Isostatic rebound. apex
There would be an immediate lift in the continental rock elevation, because of the weight of ice removed, and then a very slow and gradual continued rise. This is called isostatic rebound.