Learn more about sea floor spreading and how it works with this demo.
Seafloor spreading explained.
Seafloor spreading is a constant geologic phenomenon and a primary driver of continental drift.
Seafloor spreading happens at the bottom of an ocean as tectonic plates move apart.
The process begins when the crust is heated from beneath by upwelling in the mantle sometimes called a mantle plume.
Seafloor spreading helps to explain continental drift in the theory of plate tectonics.
These age data also allow the rate of seafloor spreading to be determined and they show that rates.
This idea played a pivotal role in the development of the theory of plate tectonics which revolutionized geologic thought during the last quarter of the 20th century.
The mid ocean ridge is the region where new oceanic crust is created.
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Convection currents carry heat from the lower mantle and core to the lithosphere.
The seafloor moves and carries continents with it.
The motivating force for seafloor spreading ridges is tectonic plate slab pull at subduction zones rather than magma pressure although there is typically.
Its discovery provided a mechanism for continental drift that alfred wegener could not explain.
The formation of the new crust is due to the rising of the molten material magma from the mantle by convection current.
The motivating force for seafloor spreading ridges is tectonic plate pull rather than magma pressure although there is typically significant magma activity at spreading ridges.
Seafloor spreading theory that oceanic crust forms along submarine mountain zones and spreads out laterally away from them.
This video goes over the process of sea floor spreading and the evidence that supports this theory.
Seafloor spreading and other tectonic activity processes are the result of mantle convection.
Seafloor spreading is a part of plate tectonics.
The oceanic crust is composed of rocks that move away from the ridge as new crust is being formed.
The process of sea floor spreading.
At ridges in the middle of oceans new oceanic crust is created.
Mantle convection is the slow churning motion of earth s mantle.
Convection currents also recycle lithospheric materials back to the mantle.