It is an area where new crust is constantly being created.
The crustal movement of the plates in the earth are not completely understood by scientist and considered a phenomenon. It is an accepted theory that the strength of the water in contrast to the weakness of the land make the movement of the plates.
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 sinking of mid-ocean ridges into ocean trenches does not directly prove the Continental Drift theory. However, it supports the theory by providing evidence of plate tectonics and the movement of tectonic plates. The theory of plate tectonics explains how continents move and interact with each other over time.
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 absence of deep focus earthquakes along the oceanic ridge system is not inconsistent with the theory of plate tectonics. Deep focus earthquakes typically occur in subduction zones, where one tectonic plate is sinking beneath another. Oceanic ridges are areas where new oceanic crust is formed and plates are moving apart, which does not typically generate deep focus earthquakes.
plate tectonics.
plate tectonics.
Yes, the fact that ocean crust is older the farther away it is from an ocean ridge supports the theory of plate tectonics. This is because new oceanic crust is formed at ocean ridges through the process of seafloor spreading, where molten rock rises and solidifies, pushing older crust away from the ridge. By observing the age of oceanic crust, scientists can trace the movement of tectonic plates and support the theory of plate tectonics.
Harry Hammond Hess is famous for his contributions to the theory of plate tectonics. He proposed the idea of seafloor spreading, which suggested that new oceanic crust is formed at mid-ocean ridges and then gradually moves away from the ridge. This theory provided key evidence in support of the broader concept of plate tectonics.
Knowledge of undersea features such as the Midatlantic Ridge gradually grew during the 19th century as accurate hydrographic surveys were made across the world. The ridge is many thousands of miles long, so parts of it would have been discovered at different dates years apart.
Iceland is a volcanic island on the midatlantic ridge, separating the North American Plate to the west from the European Plate to the east.
The crustal movement of the plates in the earth are not completely understood by scientist and considered a phenomenon. It is an accepted theory that the strength of the water in contrast to the weakness of the land make the movement of the plates.
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
Yes, Harry Hess proposed the theory of seafloor spreading and the existence of mid-ocean ridges during the 1960s. His work significantly contributed to the development of the theory of plate tectonics.
Marie Tharp's contribution to plate tectonics was the creation of the first scientific map of the ocean floor that revealed the existence of a mid-ocean ridge and deep-sea trenches. Her mapping work provided critical evidence in support of the theory of continental drift and 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.
Plate tectonics.