RE GELATION Meaning and
Definition
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Re gelation is a term that refers to the reformation or re-solidification of ice after it has melted and then refrozen. This phenomenon occurs when a block of ice, that had previously undergone partial melting, is subjected to pressure. Under such pressure, the ice melts at the point where the pressure is applied, but as soon as the pressure is released, the melted ice quickly refreezes. This process is known as re gelation.
Re gelation is often observed in environments where ice is subject to compressive forces. For example, it is commonly seen in glaciers, where the weight of the ice causes it to melt slightly underneath the surface due to pressure. As the pressure is released, the melted ice refreezes, leading to the reformation of the original ice structure. This process is crucial for the stability and movement of glaciers, as it enables them to retain their mass and continue their flow.
In addition to glaciers, re gelation also plays a significant role in other natural phenomena involving ice, such as the formation of ice dams and icicles. It is important to note that re gelation is a reversible process, as ice can melt and refreeze multiple times as the conditions change.
Common Misspellings for RE GELATION
- regelation
- regelatin
- regellation
- ee gelation
- de gelation
- fe gelation
- te gelation
- 5e gelation
- 4e gelation
- rw gelation
- rs gelation
- rd gelation
- rr gelation
- r4 gelation
- r3 gelation
- re helation
- re yelation
- re gwlation
- re gslation
- re gdlation
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