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To fill the gap of separating plates.
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What is the role of the mid ocean ridge in the movement of lithosphere plates?
To fill the gap of separating plates.
What is the role of the mid-ocean ridge in the movement of lithosphere plates?
To fill the gap of separating plates.
What is the role of mid ocean ridge in the movement of the lithosphere plates?
To fill the gap of separating plates.
How are ridge and slab pull related to convection in Earths mantle?
they are related because they all have to do with the oceanic lithosphere.The convection causes the lithosphere to move sideways and away from the midocean ridges.The ridge push makes the oceanic lithosphere slide downhill under the force of gravity. The slab pull:the old lithosphere is denser than asthenosphere so, the edge of the tectonic plates that contains oceanic lithosphere sinks and plls the rest of the tectonic plate.
How are ridge push and and slab pull related to convection in earths mantle?
they are related because they all have to do with the oceanic lithosphere.The convection causes the lithosphere to move sideways and away from the midocean ridges.The ridge push makes the oceanic lithosphere slide downhill under the force of gravity. The slab pull:the old lithosphere is denser than asthenosphere so, the edge of the tectonic plates that contains oceanic lithosphere sinks and plls the rest of the tectonic plate.
What is the role of the mid ocean ridge in the movement lithosphere plates?
The mid-ocean ridge is where new oceanic crust is formed as tectonic plates pull apart. This process, known as seafloor spreading, allows magma to rise from the mantle, solidify, and create new oceanic crust. As the crust forms at the mid-ocean ridge, it pushes older crust away, driving the movement of lithospheric plates.
What forces causes the plates to move?
The movement of tectonic plates is primarily driven by the heat and flow of mantle convection beneath the Earth's lithosphere. This convection creates currents that drag the plates along, causing them to move. Additional factors, such as ridge push and slab pull, also contribute to plate motion.
Which two tectonic plates are separated by the midocean ridge?
The mid ocean ridge separates many plates, not just two. In the Atlantic Ocean it separates the Eurasian and African plates from the North American Plate and the African Plate from the South American Plate. In the Indian Ocean it separates the African Plate from the Antarctic, Australian, Indian Plates and the Australian Plate from the Antarctic Plate. In the Red Sea it separates the African Plate from the Arabian Plate. In the Pacific Ocean it separates the Pacific Plate from the Antarctic, Nazca, Cocos, and Juan de Fuca Plates and the Nazca Plate from the Cocos and Antarctic Plates.
The movement of the ocean floor on either side of a midocean ridge is best known as?
it is known as sea floor spreading. this is when the oceanic plates diverge or move apart which causes the magma from the mantle to rise forming new sea floor.
What is the role of the mid ocean ridge in the movement of lithospheric plates?
The mid-ocean ridge is where tectonic plates diverge, allowing magma from the mantle to rise up and create new crust. As the magma cools and solidifies, it forms new oceanic lithosphere, which pushes the existing plates apart and drives the movement of the lithospheric plates. This process is known as seafloor spreading and is a key mechanism of plate tectonics.
What does the mid oceanic ridge do in the movement of the plates?
The mid-oceanic ridge is a divergent tectonic plate boundary where new oceanic crust is formed as magma rises from the mantle. As tectonic plates move apart, the ridge facilitates the continuous creation of new material, pushing older crust away from the ridge. This process drives seafloor spreading, contributing to the movement of tectonic plates and influencing geological activities like earthquakes and volcanic eruptions. Overall, the mid-oceanic ridge plays a crucial role in the dynamic cycling of Earth's lithosphere.
What causes the movement of the lisospheric plates?
The movement of lithospheric plates is primarily driven by the heat from the Earth's interior, which creates convection currents in the mantle. These currents cause the semi-fluid asthenosphere beneath the rigid lithosphere to slowly flow, pushing the tectonic plates in various directions. Additional factors, such as slab pull and ridge push, also contribute to the movement by exerting forces at plate boundaries. Together, these mechanisms lead to the dynamic behavior of the Earth's lithosphere.
