The ocean basins are the result of tectonic forces and processes. All of the ocean basins were formed from volcanic rock that was released from fissures located at the mid-oceanic ridges. The oldest rocks found in these basins are approximately 200 million years old. This is a lot younger than the oldest continental rocks which have ages greater than 4 billion years. The reason for this discrepancy is simple. Tectonic processes destroy old oceanic rocks! Oceanic rock is returned to the Earth's mantlewhen oceanic crust is subducted. Many of these subduction zones occur at the continental marginswhere oceanic crust meets continental crust. Subduction also creates the ocean's deep trenches.
The ocean basins are the result of tectonic forces and processes. All of the ocean basins were formed from volcanic rock that was released from fissures located at the mid-oceanic ridges. The oldest rocks found in these basins are approximately 200 million years old. This is a lot younger than the oldest continental rocks which have ages greater than 4 billion years. The reason for this discrepancy is simple. Tectonic processes destroy old oceanic rocks! Oceanic rock is returned to the Earth's mantlewhen oceanic crust is subducted. Many of these subduction zones occur at the continental marginswhere oceanic crust meets continental crust. Subduction also creates the ocean's deep trenches.
At the moment, a place in the Mariana Trench called the Challenger Deep, in the Pacific Ocean is the deepest part of any ocean.
The Pacific Ocean has the deepest trenches.
That it is a topgraphical and the features are a ocean floor.
Elongated troughs on the ocean floor are called oceanic trenches. These features are formed by the subduction of one tectonic plate beneath another, creating deep depressions in the seabed. Oceanic trenches are some of the deepest parts of the Earth's crust.
Challenger deep.
What causes ocean floor features to form
Isolated volcanic peaks on the ocean floor are known as seamounts. These undersea mountains are formed by volcanic activity and can be found scattered throughout the world's oceans.
The deepest known portion of the ocean floor is called the Challenger Deep, located in the Mariana Trench in the western Pacific Ocean. It reaches a depth of about 36,000 feet (10,972 meters).
The deepest parts of the ocean floor are caused by plate tectonic subduction and occur where the sea floor sinks back into the mantle in a subduction zone. These areas are called deep sea trenches and the Challenger Deep in the Mariana Trench in the Pacific is the deepest known point in Earth's oceans.
Plate tectonics and (river) erosion are responsible for the formation of ocean-floor features.
Plate tectonics and (river) erosion are responsible for the formation of ocean-floor features.
The Marianas trench .
The Marianas trench .