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∙ 8y agorift valley
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∙ 8y agoThe Earth's crust is thinner than the ocean floor because the oceanic crust is formed at mid-ocean ridges where heat from the mantle creates new crust through volcanic activity. This process creates younger, hotter, and thinner crust in the ocean compared to the older and thicker continental crust.
The ocean floor is located on the Earth's outermost layer called the crust. It is part of the crust that is covered by water, forming the ocean basins.
Oceanic crust, formed mostly of mafic rocks, or sima, is found on the ocean floor.
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
Movement of the ocean crust
A submarine canyon is a deep, steep-sided valley cut into the seabed of the continental slope, often formed by underwater currents. It can be a conduit for sediment transport from the shelf to the deep ocean.
The Earth's crust is thinner than the ocean floor because the oceanic crust is formed at mid-ocean ridges where heat from the mantle creates new crust through volcanic activity. This process creates younger, hotter, and thinner crust in the ocean compared to the older and thicker continental crust.
The ocean floor is located on the Earth's outermost layer called the crust. It is part of the crust that is covered by water, forming the ocean basins.
The ocean floor is mainly composed of basaltic crust known as oceanic crust. This crust is thinner and denser than continental crust and is formed through volcanic activity at mid-ocean ridges.
Oceanic crust, formed mostly of mafic rocks, or sima, is found on the ocean floor.
The Mariana Trench.
Ocean Crust.
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trench
The portion of Earth's crust that lies beneath the ocean floor is called oceanic crust. It is thinner and denser than continental crust, primarily composed of basaltic rocks, and formed at mid-ocean ridges through volcanic activity.
Approximately 60% of the ocean floor is made up of oceanic crust. Oceanic crust is typically thinner and denser than continental crust, and it forms at mid-ocean ridges through volcanic activity.
sea floor