Plates move away from mid-ocean ridges due to the process of seafloor spreading, which occurs as magma rises from the mantle at the ridge, creating new oceanic crust. As this new crust forms, it pushes the older crust away from the ridge, causing tectonic plates to diverge. This movement is driven by convection currents in the mantle, which create forces that pull the plates apart. Additionally, the cooling and sinking of the oceanic lithosphere further contribute to the movement of plates away from the ridges.
mid-ocean ridges and volcanoes
Depends on the type of plate boundary, at a mid-ocean ridge the plates move away from eachother. Ridges can also occur as a result of plate collision where the top layer of lithosphere is scraped off the subducted slab, this is called an accretionary prism.
At divergent plate boundaries, plates move away from each other due to the upwelling of magma from the mantle. This process creates new oceanic crust as the plates separate. As the plates move apart, they create features such as mid-ocean ridges and rift valleys.
friction - convection currents in the mantle drag the plates away from the hot rising zone below the ridgegravity - gravity pulls down on the cold dense plate being subducted under the continent, dragging the plate away from the ridge
mid-ocean ridges and volcanoes
Plates move away from mid-ocean ridges due to the process of seafloor spreading, which occurs as magma rises from the mantle at the ridge, creating new oceanic crust. As this new crust forms, it pushes the older crust away from the ridge, causing tectonic plates to diverge. This movement is driven by convection currents in the mantle, which create forces that pull the plates apart. Additionally, the cooling and sinking of the oceanic lithosphere further contribute to the movement of plates away from the ridges.
Depends on the type of plate boundary, at a mid-ocean ridge the plates move away from eachother. Ridges can also occur as a result of plate collision where the top layer of lithosphere is scraped off the subducted slab, this is called an accretionary prism.
At divergent plate boundaries, plates move away from each other due to the upwelling of magma from the mantle. This process creates new oceanic crust as the plates separate. As the plates move apart, they create features such as mid-ocean ridges and rift valleys.
When two plates move away from each other it makes a falt line or a riffed. -bekahcboo
friction - convection currents in the mantle drag the plates away from the hot rising zone below the ridgegravity - gravity pulls down on the cold dense plate being subducted under the continent, dragging the plate away from the ridge
As Earth's plates move away from each other at divergent boundaries, new crust is created as magma rises to the surface and solidifies. This process can result in the formation of features such as mid-ocean ridges and rift valleys.
Mid Ocean ridges separate the plates and create new seafloor. Places where plates converge and disappear into the abyss are called trenches. The Marianas Trench is the deepest trench in the world.
Seafloor spreading occurs when two tectonic plates move further away from each at mid-ocean ridges. In these ridges new crust is formed through volcanic activity and thus expanding the seafloor.
Yes, ocean ridges are divergent plate boundaries where tectonic plates move away from each other. As the plates separate, molten rock rises from the mantle and solidifies to form new oceanic crust, creating the underwater mountain range characteristic of ocean ridges.
divergent
when the earths plates move we either have earthquakes, tsunamis, and we get ridges and trenches.