Oceanic Ridges, when the plates separate magma leaks out through the surface and creates a small ridge or mountain. Repetition of this causes the ridge to get larger and larger as time progresses.
Oceanic plates are sections of the Earth's lithosphere that form the bedrock beneath the world's oceans. These plates are typically denser and younger than continental plates, and they are constantly moving due to the process of plate tectonics. Subduction zones are often found at the boundaries where oceanic plates meet continental plates.
Mid-ocean ridges form at diverging oceanic plates. As the plates move apart, magma rises to fill the space, creating new oceanic crust. This process results in the formation of underwater mountain ranges along the divergent boundary.
The categories are a continental and a continental plate colliding, continental and oceanic plates colliding, and oceanic and oceanic plates colliding. The two continental plates form mountains. The continental and oceanic plated colliding cause subduction zones and volcanoes. Oceanic and oceanic plates colliding form a trench.
Subduction zones are formed when oceanic plates slide beneath continental plates. The process leads to the oceanic plate being forced into the Earth's mantle. This can result in the formation of deep oceanic trenches and volcanic activity at the surface.
A deep ocean trench is likely to form where two oceanic plates push together in a convergent boundary. This is because one of the plates subducts beneath the other, creating a deep trench.
When two oceanic plates diverge, they create a mid-ocean ridge. As the plates move apart, magma from the mantle rises to fill the gap, solidifying to form new oceanic crust. This process can lead to the formation of underwater volcanic activity and features such as rift valleys along the ridge. Over time, this contributes to the growth of the ocean floor.
subduction zones
They form in areas of the Earth in which continental or oceanic plates are pulling apart.
Volcanoes form from the exposure of lava in the Earth's mantle. B Actually this is wrong, it forms a mid oceanic ridge. Do some more research next time. C. Actually it forms a Mid-Ocean Trench both of you do better reserch next time.
the oceanic plates are denser than continental plates, therefore, when oceanic plates and continental plates converge, the oceanic will go under the continental plates. But when two oceanic converge either both will rise to form moutains, or both will sink and cause a trench.
yes it does
convergent boudary
Mid-ocean ridges form where tectonic plates diverge, or move apart. This process allows magma from the mantle to rise to the surface, creating new oceanic crust as it cools and solidifies. The continuous movement of the plates at these ridges contributes to seafloor spreading and the dynamic nature of the Earth's lithosphere.
Oceanic plates are sections of the Earth's lithosphere that form the bedrock beneath the world's oceans. These plates are typically denser and younger than continental plates, and they are constantly moving due to the process of plate tectonics. Subduction zones are often found at the boundaries where oceanic plates meet continental plates.
Oceanic plates form the 'floors' of the worlds oceans.
Mid-ocean ridges form at diverging oceanic plates. As the plates move apart, magma rises to fill the space, creating new oceanic crust. This process results in the formation of underwater mountain ranges along the divergent boundary.
They form volcanic mountains by heating magma that breaks through the crust. On the oceanic plates, these crustal hot spots can form chains of volcanic islands such as the Hawaiian Islands.