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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.


Describe how molten rock can form new oceanic crust?

Some of the molten rock overflows onto the ocean floor in tremendous eruptions. material from the mantle canwell up, forming a ridge and new oceanic 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


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

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


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.


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.


What three of the 4 layers of this crust are igneous material?

The layers of Earth's crust that consist mostly of igneous material are the uppermost layer, the oceanic crust, and the lowermost layer, the lower continental crust and lithospheric mantle. These layers are primarily composed of igneous rocks formed from the cooling and solidification of molten rock.


Does molten material erupt inside the central valley of mid-ocean ridges?

Yes, molten material does erupt inside the central valley of mid-ocean ridges. This molten material comes from the Earth's mantle and rises to the surface through the cracks in the oceanic crust, creating new crust as it solidifies.


How do you explain the process of the seafloor spreading?

The seafloor spreading definition is the geologic process that occurs at the boundary between 2 plates where molten material within the earth pushes its way up, causing the plates to move away from each other. At these divergent boundaries molten material cools and hardens, creating new oceanic crust or seafloor


The process that permits new ocean crust to form as molten rock from the mantle wells up between two oceanic plates that have moved away from each other?

This process is called seafloor spreading. It occurs at mid-ocean ridges, where two oceanic plates diverge, allowing molten rock from the mantle to rise and solidify as new crust. As the plates move apart, the newly formed crust pushes older crust away from the ridge, leading to the formation of a continuous oceanic crust.


What happens when oceanic crust sinks?

When oceanic crust sinks into the mantle at a subduction zone, it melts due to the high temperature and pressure. The molten rock then rises to the surface, forming volcanoes on the overriding plate. This process helps to recycle material back into the mantle and plays a crucial role in plate tectonics.


What happens when oceanic crust and continental crust collide?

Subduction occurs on continental boundaries because oceanic sub floor is denser and heavier than the lighter more buoyant crust. The oceanic crust slides under the continental crust areas usually on a plate boundary. This is in a recycle style mode that constantly is remaking the ocean floor. The oldest rocks on the ocean bottom are a drop in the geologic time bucket, compared to the rock ages on land.