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Shifting of Tectonic plates away from each other.

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Where does new crust comes from?

New crust is formed at mid-ocean ridges through a process called seafloor spreading. Magma rises to the surface, cools, and solidifies, creating new oceanic crust. This process continually adds new material to the ocean floor, expanding the Earth's crust.


What is the mechanism responisble for producing the new oceanic crust between 2 diverging plates?

The mechanism responsible for producing new oceanic crust between two diverging plates is seafloor spreading. Magma rises up from the mantle at mid-ocean ridges, solidifies upon reaching the seafloor, and forms new crust. As the plates move apart, this process continuously adds new material to the ocean floor.


Process that forms new seafloor?

The process that forms new seafloor is called seafloor spreading. It occurs at mid-ocean ridges where new oceanic crust is created through volcanic activity. As magma rises and solidifies, it adds to the seafloor, pushing older crust away from the ridge and creating a continuous process of crust formation.


How does the movement of the earth's crustal plates cause the formation of ocean basins?

The movement of earth's crustal plates causes divergent boundaries where plates move apart, allowing magma to rise from below and solidify to form new crust. This process creates mid-ocean ridges, which is where new oceanic crust is formed. Over time, as more crust is added, the ocean basin widens and gets deeper.


What is the major source of oceanic salinity?

The major source of oceanic salinity is the dissolution of ions from rocks on land that are carried into the ocean by rivers. This process adds various salts to seawater, contributing to its overall salinity. Additionally, hydrothermal vents on the ocean floor can also introduce elements and minerals that affect salinity.

Related Questions

The process of continually adds new crust to the ocean floor along both sides of the mid-ocean ridge.?

sea floor spreading


What process adds new crust to the ocean floor?

Volcanic eruptions are one process that adds new material to crust. Lava from the volcanoes eventually cool, forming new land. Sea floor spreading also adds new material to the crust.


What is a good sentence for sea floor spreading?

Sea floor spreading mean the process by which molten material adds new oceanic crust to the ocean floor


The process by which molten material adds new oceanic crust to the ocean floor?

DA ANSWER ISseafloor spreadingThe_process_by_which_molten_material_adds_new_oceanic_crust_to_the_ocean_floor_is_calledThe_process_by_which_molten_material_adds_new_oceanic_crust_to_the_ocean_floor_is_called


What is the process that continually adds new material to the ocean floor is called?

sea-floor spreading


What is the process that adds new material to the ocean floor?

Sedimentation.


The process that continualy adds new material to the ocean floor is called?

sea floor spreading


Each cycle of spreading and intrusion of magma during seafloor spreading results in?

the formation of new oceanic crust. Magma rises to the surface at mid-ocean ridges, solidifies upon contact with seawater, and creates new crust as it spreads horizontally away from the ridge axis. This process continually adds new crust to the ocean floor as tectonic plates move apart.


Where does new crust comes from?

New crust is formed at mid-ocean ridges through a process called seafloor spreading. Magma rises to the surface, cools, and solidifies, creating new oceanic crust. This process continually adds new material to the ocean floor, expanding the Earth's crust.


The process that continually adds new material to ocean floor is?

sedimentation


What is the proces that continually adds new material to the ocean floor?

Sea-floor Spreading through a mid ocean ridge.


What is the mechanism responisble for producing the new oceanic crust between 2 diverging plates?

The mechanism responsible for producing new oceanic crust between two diverging plates is seafloor spreading. Magma rises up from the mantle at mid-ocean ridges, solidifies upon reaching the seafloor, and forms new crust. As the plates move apart, this process continuously adds new material to the ocean floor.