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.
It's often called a trench.
An Anticline is formed when the crust bends and curves upward.
The place where oceanic crust bends back into the mantle is called a subduction zone. This occurs when one tectonic plate is forced beneath another, often creating deep-sea trenches and volcanic activity. Subduction zones are common around the Pacific Ring of Fire.
At some points, the oceanic crust bends downward and forms a deep-ocean trench. Then the oceanic crust sinks back into the mantle through a process called subduction.
The force pushing upward on the continental crust is isostatic rebound, caused by the buoyancy of the less dense continental crust floating on the denser mantle. The downward force is from the weight of the overlying rock and sediments, as well as tectonic forces like subduction or compression.
It's often called a trench.
Syncline is a type of fold that is created when the crust bends and curves downward. It is a fold that is convex up and has its oldest beds at its core.
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This geological formation is called a syncline. It is a downward fold in the rock layers where the youngest layers are in the center and the oldest are on the outside.
When the Earth's crust bends but does not break, it is called flexural bending or flexure. This type of deformation can occur in response to tectonic forces, leading to the formation of features like folds, fault-related folds, and anticlines.
An upward fold in rock that forms an arch-like structure is called an anticline. It is a type of fold in the Earth's crust where the rock layers are bent upwards in a convex shape, with the oldest rocks located at the core of the fold.
An Anticline is formed when the crust bends and curves upward.
It is an exposed slice into the crust of the earth.
A downward bend in rocks is called a syncline. It is a type of fold where the rocks bend downward in the center, forming a U-shape. Synclines are commonly found in regions where the Earth's crust has been subjected to tectonic forces.
When a rock bends instead of breaking due to plate movement, it is called ductile deformation. This usually occurs under high pressure and temperature conditions deep within the Earth's crust.
A trench between two parallel faults in the earth's crust is called a graben. Grabens are formed by the downward movement of blocks of land between normal faults.
When a body of rock bends upward into an arch, it is called an anticline. It is a type of fold in the Earth's crust where the oldest rocks are found at the core of the arch. Anticlines are often associated with the accumulation of oil and gas deposits.