lithosphere or geosphere
Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins.
oceanic lithosphere sinks at subduction zones but not at mid ocean ridges because at subduction zones the oceanic lithosphere is subducted, or sinks, under another plate. Oceanic Lithosphere sinks at subduction zones which are usually at convergent boundaries, but at mid-ocean ridges the plates are actually separating not coming together
The oceanic lithosphere slides downhill due to the gradual cooling and densification of the lithosphere as it moves away from the mid-ocean ridges. This increase in density causes the lithosphere to sink into the underlying asthenosphere due to gravity.
New oceanic lithosphere forms as a result of seafloor spreading at mid-ocean ridges. Magma rises from the mantle, solidifies at the mid-ocean ridge, and creates new oceanic crust. This process leads to the continuous expansion of the ocean floor.
No, the lithosphere doesn't include the ocean floor because it is a layer of the atmosphere. (outer space)
lithosphere or geosphere
Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins.
Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins.
Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins.
oceanic lithosphere sinks at subduction zones but not at mid ocean ridges because at subduction zones the oceanic lithosphere is subducted, or sinks, under another plate. Oceanic Lithosphere sinks at subduction zones which are usually at convergent boundaries, but at mid-ocean ridges the plates are actually separating not coming together
No, the continents and ocean basins are located on the lithosphere, which is the rigid outer layer of the Earth. The asthenosphere is a semi-fluid layer beneath the lithosphere.
oceanic lithosphere sinks at subduction zones but not at mid ocean ridges because at subduction zones the oceanic lithosphere is subducted, or sinks, under another plate. Oceanic Lithosphere sinks at subduction zones which are usually at convergent boundaries, but at mid-ocean ridges the plates are actually separating not coming together
As the oceanic lithosphere moves away from a mid-ocean ridge, it cools and thickens. This process causes the ocean floor to become older and denser, resulting in its gradual subsidence. The farther it gets from the ridge, the deeper the ocean floor becomes due to the increased thickness and weight of the lithosphere.
Oceanic. Most of the Pacific plate is under the Pacific Ocean.
The oceanic lithosphere slides downhill due to the gradual cooling and densification of the lithosphere as it moves away from the mid-ocean ridges. This increase in density causes the lithosphere to sink into the underlying asthenosphere due to gravity.
ocean,sea,ponds,rivers and swamps.