It is an area where new crust is constantly being created.
In the 1950's a research team that was mapping the ocean floor discovered strange features around the Mid-Atlantic Ridge that indicated the ridge was seismologically active. Further mapping indicated that all of Earth's oceans had similar ridge systems, supporting the theory of plate tectonics the spreading of the sea floor
The mid ocean ridge support it becuase your find similar sample of rock type on opposite side of the ridge which has thesame age. Mid-Oceanic ridge are where new sea floors are created which is usually called a divergent boundary. As these places move apart they push the other plates to collide and slide pass each other. That is why it is a cycle
No, the crust is very thin under the oceanic ridge system, making deep focus earthquakes impossible there as the crust does not have the required depth for such earthquakes.
The creation of oceanic crust at the mid-ocean ridges is part of the all encompassing theory of plate tectonics. The mid-ocean ridge is a volcanic feature caused by the spreading apart of oceanic plates as part of plate tectonics. The sea floor at the ridges are uplifted by rising magma. The rising magma is part of a process of heat transfer from the interior of the Earth to the surface known as a convection current. As the rising magma cools, it forms new crust which becomes part of the ridge.
Ridge push is a gravitation force that causes a plate to move away from the crest of an ocean ridge, and into a subduction zone.
The mid-atlantic ridge is a good example
plate tectonics.
plate tectonics.
In the 1950's a research team that was mapping the ocean floor discovered strange features around the Mid-Atlantic Ridge that indicated the ridge was seismologically active. Further mapping indicated that all of Earth's oceans had similar ridge systems, supporting the theory of plate tectonics the spreading of the sea floor
The mid ocean ridge support it becuase your find similar sample of rock type on opposite side of the ridge which has thesame age. Mid-Oceanic ridge are where new sea floors are created which is usually called a divergent boundary. As these places move apart they push the other plates to collide and slide pass each other. That is why it is a cycle
Iceland is a volcanic island on the midatlantic ridge, separating the North American Plate to the west from the European Plate to the east.
No, the crust is very thin under the oceanic ridge system, making deep focus earthquakes impossible there as the crust does not have the required depth for such earthquakes.
Plate tectonics.
the ages of the rocks become increasingly older in samples obtained farther from the ridge and the younger had just come out the ridge.
An ocean ridge is and underwater mountain range which is formed in the same way as an above water mountain range, by plate tectonics.
Plate TECTONICS
Yes. New ocean crust is being formed at the mid ocean ridges (MORs) resulting in the older crust being pushed farther away, moving the plates towards a subduction zone. MORs divide 2 plates.