Oceanic Trench or Deep Sea Channel, it is a narrow, long and having a sharp inclination depression in the lowermost deep-sea in which happen the extreme oceanic depths. They normally form in places where once the structure of the earth's crust plate <span>is forced below the edge of</span> another. While Abbysal plain is a beneath the surface of the water plain on the deep ocean floor, typically found at depths approximately 3,000 meters and 6,000 meters. It is in a horizontal position largely between in a mid-ocean ridge and a foot of a continental rise. Almost 50% of the Earth’s surface was sheltered by Abbysal Plains. They are the smoothest and flattest and not so discovered areas on Earth.
A substantial rise in sea level along a coast during a severe storm is called a storm surge
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What is storm surge?</h3>
- A coastal flood or tsunami-like event of rising water known as a storm surge, storm flood, tidal surge, or storm tide is frequently linked to low-pressure weather systems like cyclones.
- It excludes waves and is calculated as the increase in water level above the typical tidal level.
- The high-speed wind pushing water towards the coast over a long fetch is the primary meteorological component causing a storm surge.
- The shallowness and orientation of the water body in the storm's path, the timing of tides, and the storm's impact on atmospheric pressure are other variables that affect how severe a storm surge will be. There is evidence to suggest that storm surge danger may be rising due to climate change.
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