The continents and ocean floor are unstable because the plates of the lithosphere move. When the plate move, they cause the continents and ocean floor to move.
Basalt is the iron-rich volcanic rock that makes up much of the ocean floor. It forms from the cooling and solidification of magma that erupts through underwater volcanic activity, such as mid-ocean ridges. Basalt is a key component of Earth's oceanic crust.
Basalt
No. The newest ocean floor is at the mid-ocean ridge.
The floor of the ocean is called the seabed or ocean floor. It is made up of different features such as abyssal plains, trenches, ridges, and volcanoes.
You can't have a continent rise from land, but you can have land rise from the continental shelf, which may be under water, and that is called an island.
Continental Shelf.
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Molten meaterial
This occurs in a subduction zone.
As the sea floor spreads, the old ocean floor gets pushed out, which makes the plates move.
Slope
Continental Slope
Islands in an ocean don't belong to any continent. If they were part of a continent they wouldn't be islands would they? The African Continent is the continent nearest the Canary Islands, but the islands are the result of volcanic activity on the ocean floor.
basalt
An ocean to continent boundary is where the oceanic crust meets the continental crust. This typically occurs at a continental shelf, which is the gently sloping transition between the continent and the ocean floor. This boundary is marked by significant differences in physical and geological characteristics between the two crust types.
A sharp drop from a continent to an ocean basin is called a continental slope. This feature marks the boundary between the continental shelf and the deep ocean floor.
The transition zone between an ocean basin floor and a continent is known as the continental shelf. It is the submerged part of a continent that extends from the shoreline to the continental slope. The continental shelf is characterized by relatively shallow waters and is an area of high biological productivity.