yes it is. because of the extream heat it makes the plates plastic like.
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.
Subduction occurs where the oceanic crust bends down towards the mantle at a subduction zone, typically at convergent plate boundaries where two tectonic plates collide. The denser oceanic plate is forced beneath the less dense continental plate, creating a deep trench and volcanic activity. This process contributes to the recycling of Earth's crust and the formation of mountain ranges and volcanic arcs.
These bends in rock formations caused by tectonic plate collision are known as fold mountains. These mountains form when rock layers are squeezed and pushed together, resulting in folds such as anticlines and synclines. Examples include the Himalayas and the Andes.
That is a description of a trench, which is formed at tectonic plate boundaries where one plate is forced beneath another through a process called subduction. Trenches are among the deepest parts of the ocean floor.
It's often called a trench.
The plastic-like part of the mantle is known as the asthenosphere. It is a semi-fluid layer located beneath the lithosphere, composed of partially molten rock material that allows for the movement of tectonic plates.
A long narrow and very deep canyon where the ocean floor bends down toward the mantle is called an ocean trench. This is caused by two plates pulling apart.
A long narrow and very deep canyon where the ocean floor bends down toward the mantle is called an ocean trench. This is caused by two plates pulling apart.
A long narrow and very deep canyon where the ocean floor bends down toward the mantle is called an ocean trench. This is caused by two plates pulling apart.
asthenosphere!
A portion of the upper mantle known as the asthenosphere.
Rocks in the mantle are subjected to high temperatures and pressures, which cause them to deform plastically over long periods of time. This plastic deformation allows rocks in the mantle to flow slowly, similar to the behavior of very viscous fluids. This process is known as mantle convection and plays a crucial role in the movement of tectonic plates on the Earth's surface.
Partially molten, plastic like, flowing layer located below the solid part of Earth's mantle is the Asthenosphere. The asthenosphere is mechanically weak and ductiley deforming region of the upper mantle.
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.
deep ocean trench.
Subduction occurs where the oceanic crust bends down towards the mantle at a subduction zone, typically at convergent plate boundaries where two tectonic plates collide. The denser oceanic plate is forced beneath the less dense continental plate, creating a deep trench and volcanic activity. This process contributes to the recycling of Earth's crust and the formation of mountain ranges and volcanic arcs.
Convex when it bends outwards, concave when it bends inwards