At the mid-ocean ridges, new ocean floor is continuously being created from rising magma originating from the Earth's mantle. The creation of the new oceanic crust pushes older crust away from the ridge in a conveyor belt fashion. This process is known as sea-floor spreading. The fracture can be seen beneath the ocean as a line of ridges that form as molten rock reaches the ocean bottom and solidifies. A narrow depressed area running along the center of the ridges, called a rift, is the region where volcanic activity is adding magma to the two diverging pieces of oceanic crust.
The Oceanic Crust close to the Mid Ocean Ridge is thinner than that Oceanic Crust far away from the ridge. This is due to tensional forces, as a result of crustal expansion and rock fracturing during the formation of the ridge.the oceanic crust is thinner
The interconnected oceanic ridge system is known for its volcanic activity and the creation of new oceanic crust through seafloor spreading.
A synonym for mid-ocean ridge is oceanic ridge. These underwater mountain ranges are formed by tectonic plates moving apart and are characterized by volcanic activity and the creation of new oceanic crust.
an oceanic ridge
Yes, new oceanic crust is formed at mid-ocean ridges through a process called seafloor spreading. Magma rises from the mantle through the ridge, cools and solidifies to form new crust. This process helps in constantly renewing the oceanic crust.
mid-oceanic ridge. its where the plates are shifting away from eachother.
Its oceanic crust
Trench
a ridge in the ocean
a ridge in the ocean
hit the books!!
Isochrons on the sea floor are located at the mid-ocean ridges. They represent the age of the oceanic crust and are created as new crust forms at the ridge axis and moves away from it over time. Older crust is farther from the ridge, while younger crust is closer to the ridge.
Plates on either side of the Mid-Atlantic Ridge are oceanic plates.
haha i really dont know
The Oceanic Crust close to the Mid Ocean Ridge is thinner than that Oceanic Crust far away from the ridge. This is due to tensional forces, as a result of crustal expansion and rock fracturing during the formation of the ridge.the oceanic crust is thinner
An equal amount of oceanic crust is being subducted at the convergent plate boundaries as is being created at the mid-oceanic ridge.
haha i really dont know