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Seafloor spreading occurs when two tectonic plates move further away from each at mid-ocean ridges. In these ridges new crust is formed through volcanic activity and thus expanding the seafloor.

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What is least likely to result from seafloor spreading?

bananas :~P


What did the magnetic strips prove in seafloor spreading?

They proved that the seafloor was spreading.


How to Diagram the process of seafloor spreading?

A diagram that shows how seafloor spreading works.


Seafloor spreading begins when?

Seafloor spreading is triggered by a rift in a continental land mass.


Which force is responsible for seafloor spreading?

Gravity in the oceanic crust is responsible for seafloor spreading.


Which observation was not instrumenntal in formulating the hypothesis of seafloor spreading?

The observation of the alternating magnetic stripes on the seafloor was instrumental in formulating the hypothesis of seafloor spreading.


What does seafloor spreading have to do with the theory of continental drift?

Seafloor Spreading helped move the Continents to their current location.


How many centimeters does the seafloor move a year?

The movement of the seafloor can vary depending on the location, but on average it moves at a rate of a few centimeters per year. This movement is a result of plate tectonics and the process of seafloor spreading.


What seafloor is the process by which new crust is created when seafloor moves apart and magma rises?

Seafloor Spreading


What is seafloor spreading and what forms as a result of seafloor spreading?

Seafloor spreading is the process by which new oceanic crust is formed at mid-ocean ridges as tectonic plates diverge and magma rises to the surface. This results in the creation of new ocean floor, leading to the expansion of ocean basins. As seafloor spreading occurs, features such as mid-ocean ridges, rift valleys, and volcanic islands can also form as a consequence. Additionally, this process contributes to the cycle of plate tectonics, influencing geological activity and the distribution of continents.


What phenomenon occurs as a result of seafloor spreading?

In 1960, seafloor spreading was hypothesized by Harry Hess of Princeton University. Seafloor spreading occurs at divergent boundaries and it is said to be the mechanism that operates along the oceanic ridge system to generate new seafloor. Thus, the result of seafloor spreading is the creation of new sea floor through the uplift of magma: magma raises from asthenosphere, new oceanic lithosphere moves from ridge, and it thickens, cools (becomes denser), and subsides.


How does magma help seafloor spreading?

Magma plays a crucial role in seafloor spreading as it rises from the mantle at mid-ocean ridges, where tectonic plates are diverging. When magma reaches the ocean floor, it cools and solidifies, forming new oceanic crust. This process not only creates new seafloor but also pushes older crust away from the ridge, facilitating the movement of tectonic plates. As a result, seafloor spreading continuously reshapes the ocean floor and contributes to geological activity.