Iceberg.
The continental margin consists of the continental shelf, continental slope, and continental rise. One feature that is not part of the continental margin is the abyssal plain, which lies deeper in the ocean and beyond the continental rise. The abyssal plain represents the flat, deep-sea floor that extends across the ocean basins, while the continental margin is specifically associated with the transition from land to ocean.
The part of the ocean floor nearest the continents is called the continental shelf. It is a gently sloping, submerged platform that extends from the shoreline to the continental slope. The continental shelf is important for marine life as it provides a shallow and productive area for various organisms to thrive.
A.Rift zoneC Near the continental marginB.Abyssal plainB Very flat part of ocean floorC.Ocean trenchA Site of seafloor spreadingD.SeamountD Underwater volcano
Icebergs.The icebergs that break off do so because the glacier of which they are a part flows toward the sea, like a river, only much slower.When a fracture or a vulnerable sheer exists in the glacier, and the glacier tongue drifts far enough into open water, and the sea currents or waves exert enough pressure on the tongue, the tongue splits off from the glacier and becomes an iceberg.
Icebergs were once part of a glacier. To better understand an iceburg, one must know what a glacier is made from. When the temperature is low enough that the sun doesn't melt snow, the snow then accumulates on top of itself, compressing and eventually hardening to become a glacier. The edges of the huge glaciers have ice shelves where the glacier itself meets the ocean and parts of the glacier float. These can break off to form icebergs when the waves from the ocean erosion on the thinner stretches of the ice shelf.
The continental shelf
The part of the ocean that steeply drops off is called the continental shelf.
The continental shelf is the shallow part of the ocean.
The continental margin consists of the continental shelf, continental slope, and continental rise. One feature that is not part of the continental margin is the abyssal plain, which lies deeper in the ocean and beyond the continental rise. The abyssal plain represents the flat, deep-sea floor that extends across the ocean basins, while the continental margin is specifically associated with the transition from land to ocean.
Continental Shelf.
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False, continental shelves are part of the Coastal Plain
No the shelf is among the shallowest parts of the ocean.
The bit between the mid ocean ridge and the continental rise.
The bottom of the ocean is part of a tectonic plate or continental shelf, or can be on the breach line between two shelves.
TheNeritic Zone
Clown fish live on the continental shelf part of the ocean zone.