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When spreading molten material rises from the mantle in the sea-floor and erupts, it can create sea mounts, which are underwater mountains. If enough material is ejected, the mounts will break through the surface of the water to create islands.

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Q: In seafloor spreading molten material rises from the mantle and erupts?
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What does magma have to do with seafloor spreading?

Magma plays a key role in seafloor spreading as it rises from the mantle through the mid-ocean ridges, creating new oceanic crust. This process involves the formation of new crust as magma cools and solidifies along the spreading center, pushing the existing seafloor apart.


Where does molten material that rises from the mantle erupt?

Molten material that rises from the mantle erupts through openings in the Earth's crust called volcanoes. These volcanic eruptions release lava, ash, and gases onto the Earth's surface.


What process forms new seafloor?

New seafloor is formed through a process called seafloor spreading, which occurs at mid-ocean ridges. Magma rises from the mantle and solidifies to create new crust as tectonic plates move apart. This continuous process results in the creation of new seafloor and plays a key role in plate tectonics.


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.


What are facts about seafloor spreading?

Seafloor spreading is the process where new oceanic crust is formed through volcanic activity along mid-ocean ridges. It occurs due to the upwelling of magma from the mantle, creating new crust that pushes the existing seafloor apart. The age of the oceanic crust gets progressively older as you move away from the mid-ocean ridge, demonstrating the continual growth of the seafloor.

Related questions

In sea-floor spreading molten material rises from the mantle and erupts .?

When spreading molten material rises from the mantle in the sea-floor and erupts, it can create sea mounts, which are underwater mountains. If enough material is ejected, the mounts will break through the surface of the water to create islands.


When solid mantle rock rises during seafloor spreading magma is produced as a result of decompression melting?

Yes, during seafloor spreading, when solid mantle rock rises due to plate tectonic forces, it experiences reduced pressure which leads to decompression melting. This process produces magma that eventually erupts onto the seafloor, creating new oceanic crust.


What is the process that makes old oceanic crust go into the mantle?

makes up the bottom of the world's oceans is Magma from the underlying mantle erupts at the edges, then cools and solidifies to form new ocean crust.plate a process called seafloor spreading and back into the.


What layer produces the magma that cause seafloor spreading and volcanoes?

the upper mantle


What was the primary force that causes the seafloor to spread and continents to drift?

The primary force driving seafloor spreading and continental drift is mantle convection. Heat from Earth's core causes the mantle to circulate, creating convection currents that move tectonic plates, leading to the spreading of the seafloor and movement of continents.


What is a constructive force caused by the convection in the mantle?

A constructive force caused by convection in the mantle is seafloor spreading. As hot mantle material rises and spreads out at mid-ocean ridges, it creates new oceanic crust, which pushes the older crust aside. This process helps in the formation of new oceanic crust and contributes to the widening of the seafloor.


What kinds of ocean currents might cause seafloor spreading?

Oceanic currents themselves do not directly cause seafloor spreading. Seafloor spreading is primarily driven by tectonic forces, specifically the movement of tectonic plates away from each other at mid-ocean ridges. This movement leads to the upwelling of magma from the mantle, creating new oceanic crust at the spreading center. Ocean currents can affect the distribution of heat and nutrients in the ocean, but they do not play a direct role in the process of seafloor spreading.


What does magma have to do with seafloor spreading?

Magma plays a key role in seafloor spreading as it rises from the mantle through the mid-ocean ridges, creating new oceanic crust. This process involves the formation of new crust as magma cools and solidifies along the spreading center, pushing the existing seafloor apart.


What is the driving force for seafloor spreading?

The driving force for seafloor spreading is the movement of tectonic plates. As magma rises from the mantle to the surface at mid-ocean ridges, it creates new oceanic crust which pushes the existing plates apart, causing seafloor spreading. This process is part of the larger theory of plate tectonics.


In sea-floor spreading what happens to the old oceanic crust as new molten material rises from the mantle?

In sea-floor spreading, the old oceanic crust is pushed away from the mid-ocean ridge as new molten material rises from the mantle. As the new material solidifies, it forms new oceanic crust, leading to the spreading of the seafloor and the continuous creation of new crust. The older oceanic crust eventually gets subducted back into the mantle at tectonic plate boundaries.


Where does molten material that rises from the mantle erupt?

Molten material that rises from the mantle erupts through openings in the Earth's crust called volcanoes. These volcanic eruptions release lava, ash, and gases onto the Earth's surface.


Is there evidence that seafloor-spreading?

Yes, there is evidence supporting seafloor spreading, including magnetic striping patterns on the ocean floor, the age progression of seafloor away from mid-ocean ridges, and the presence of hydrothermal vents along mid-ocean ridges that release magma from the Earth's mantle.