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Q: In seafloor spreading where is old crust located?
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Explain the relationship between trenches and seafloor spreading?

1. New sea-floor is created by the upwelling of magma at mid-ocean spreading centers; old ocean floor is destroyed by subduction at deep sea trenches. 2. The area is a subduction zone. Magma from underground comes up and destroys that crust. That crust is then recycled and the magma cools and hardens. That creates new land, that creates the trenches. Seafloor spreading is in the ocean and happens with convection currents. That is the relationship between. 3. As new seafloor is formed at mid-ocean ridges, the old seafloor is pushed down into trenches at subduction zones.


What is the mechanism for seafloor spreading?

Molten lava leaks out along the seams between tectonic plates in the earth's crust, at the sea bottom. Because the water is cold, the lava hardens quickly into rock, causing the sea floor to spread in both directions.


What happens to the old oceanic crust as new molten material rises from the mantle?

The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.


How does new seafloor form at mid-ocean ridges?

Slow motion


What made the scientists believe that the sea floor is spreading?

1. What made scientist believe that the seafloor was spreading? Samples of the deep ocean floor show that basaltic oceanic crust and overlying sediment become progressively younger as the mid-ocean ridge is approached, and the sediment cover is thinner near the ridge. Also, the rock making up the ocean floor is considerably younger than the continents, with no samples found over 200 million years old, as contrasted with maximum ages of over 3 billion years for the continental rocks. This confirms that older ocean crust has been reabsorbed in ocean trench systems. by; Vontamayosa find me on Facebook

Related questions

How does the movement of the old and the new crust move in seafloor spreading?

well when the sea moves so does the crust.


Explain the relationship between trenches and seafloor spreading?

1. New sea-floor is created by the upwelling of magma at mid-ocean spreading centers; old ocean floor is destroyed by subduction at deep sea trenches. 2. The area is a subduction zone. Magma from underground comes up and destroys that crust. That crust is then recycled and the magma cools and hardens. That creates new land, that creates the trenches. Seafloor spreading is in the ocean and happens with convection currents. That is the relationship between. 3. As new seafloor is formed at mid-ocean ridges, the old seafloor is pushed down into trenches at subduction zones.


Why is Earth not getting larger if the seafloor is spreading?

Subduction and folding.The seafloor ,may be "spreading" in the center but that doesn't necessarily mean it's getting bigger; at the edges it may be slipping underneath a continental plate (subduction) or piling up on itself to form mountains (folding).


What happens along a divergent boundary between two oceanic plates?

A rift valley, volcano, earthquake, trench.


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 is the mechanism for seafloor spreading?

Molten lava leaks out along the seams between tectonic plates in the earth's crust, at the sea bottom. Because the water is cold, the lava hardens quickly into rock, causing the sea floor to spread in both directions.


What is the evidence for sea-floor spreading?

at the mid-ocean ridge, molten material rises up from the mantel and spreads out, pushing the older rocks to both sides of the ridge.


When new crust is made what happens to the old crust?

When new crust is made, like at a spreading center, old crust must be destroyed, like at a subduction zone, where it is brought back into the inner earth and melted and recycled through.


What is the age of the oldest seafloor?

The oldest seafloor is estimated to be around 200 million years old. New oceanic crust is continuously formed at mid-ocean ridges, so the seafloor is constantly being recycled.


Why doesn't our planet get larger from sea floor spreading?

As new oceanic crust forms at mid-ocean ridges, old oceanic crust is destroyed at subduction zones.


What happens to old oceanic crust as molten materials rises from the mantle?

The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.


What happens to old oceanic crust as new molten material from the mantle?

The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.