Table of Contents
- 1 What is the process by which new oceanic crust is added?
- 2 What happens to the oceanic crust as new molten materials rises from the mantle?
- 3 What rises up through the mantle and pushes apart the oceanic plates at the mid-ocean ridge?
- 4 What is the cycle in which heated material rises and cooler material sinks?
- 5 Where does the molten material rise from during sea floor spreading?
- 6 What does molten material that rises from the mantle erupt?
- 7 What happens to the plates and the mantle at convergent plate boundaries?
- 8 What is formed on the oceanic side when oceanic and continental crust collide?
What is the process by which new oceanic crust is added?
New oceanic crust is formed at mid-ocean ridges. This happens through the process of seafloor spreading. Seafloor spreading is the process by which new oceanic lithosphere forms at mid-ocean ridges. As tectonic plates move away from each other, magma rises from Earth’s interior.
What happens to the oceanic crust as new molten materials rises from the mantle?
What happens to old oceanic crust as new molten material rises from the mantle? The molten material spreads out, pushing older rock to both sides of the ridge. It sinks down due to density. The Earth’s ocean floors move like conveyor belts, carrying the continents along with them, as they move.
Whats the process when the ocean floor sinks into the mantle?
Subduction is the process by which the ocean floor sinks beneath a deep-ocean trench and back into the mantle.
What rises up through the mantle and pushes apart the oceanic plates at the mid-ocean ridge?
A mid-ocean ridge or mid-oceanic ridge is an underwater mountain range, formed by plate tectonics. This uplifting of the ocean floor occurs when convection currents rise in the mantle beneath the oceanic crust and create magma where two tectonic plates meet at a divergent boundary.
What is the cycle in which heated material rises and cooler material sinks?
convection cell
The cooler, denser water sinks, and the warmer water rises to the surface to create a cycle called a convection cell.
What happens when molten material rises?
At a mid-ocean ridge, molten material rises from the mantle and erupts. The molten material then spreads out, pushing older rock to both sides of the ridge. As the molten material cools, it forms a strip of solid rock in the center of the ridge.
Where does the molten material rise from during sea floor spreading?
What is the process of sea-floor spreading? At the mid-ocean ridge, molten material rises from the asthenosphere/mantle and erupts. The molten material then spreads out, pushing older rock to both sides of the ridge.
What does molten material that rises from the mantle erupt?
A ridge forms along a crack in the oceanic crust. At a mid-ocean ridge, molten material rises from the mantle and erupts. The molten material then spreads out, pushing older rock to both sides of the ridge. As the molten material cools, it forms a strip of solid rock in the center of the ridge.
How does seafloor spreading add material to the ocean floor?
Seafloor spreading occurs at divergent plate boundaries. As tectonic plates slowly move away from each other, heat from the mantle’s convection currents makes the crust more plastic and less dense. The less-dense material rises, often forming a mountain or elevated area of the seafloor.
What happens to the plates and the mantle at convergent plate boundaries?
At convergent plate boundaries, oceanic crust is often forced down into the mantle where it begins to melt. Magma rises into and through the other plate, solidifying into granite, the rock that makes up the continents. Thus, at convergent boundaries, continental crust is created and oceanic crust is destroyed.
What is formed on the oceanic side when oceanic and continental crust collide?
Trench is formed on the oceanic side when oceanic and continental crust collide. Explanation: At the subduction boundary, a deep ocean trench forms.
When convection occurs warmer material rises and cooler material sinks?
Notice how all three are affected by heat and gravity. Convection In the process of convection, hot material from deep within the Earth rises while cooler material near the surface sinks. When the warmer material cools, it becomes denser and begins to sink back down.