Some move away from each other and create massive trenches normally in the sea bed, for example the Mariana Trench - 10,998 m.
When plates move farther and farther apart, this is known as seafloor spreading. It occurs at mid-ocean ridges where new oceanic crust is formed as plates diverge. This process is driven by convection currents in the Earth's mantle.
Oceanic ridges are caused by the divergent movement of tectonic plates. As the plates move apart, magma rises from the Earth's mantle to fill the gap, creating new oceanic crust. This process is known as seafloor spreading.
The process that pushes tectonic plates apart is called seafloor spreading. Magma rises from the mantle through divergent boundaries, creating new oceanic crust. As the new crust forms, it pushes the existing plates away from each other, causing them to move.
No, oceanic plates move faster than continental plates. This is due to the density of the oceanic plates (basalt is denser). For example, the fastest moving plates are the Pacific plate, Cocos plate, and Nazca plate. All oceanic.
valconoes!
You are a mid-ocean ridge that forms when tectonic plates move apart and new oceanic crust is created through volcanic activity. This process is known as seafloor spreading, and it results in the formation of new oceanic crust at the mid-ocean ridge.
A long, linear crack that forms as two tectonic plates move apart is called a mid-ocean ridge. This type of boundary is where new oceanic crust is created as molten rock rises up from the mantle and solidifies along the spreading center. Over time, as the plates continue to move apart, the new crust forms a continuous ridge on the ocean floor.
Divergent Boundaries happen when two plates (oceanic or contental) begin to diverge, or move apart. Convergent Boundaries occur when two plates (again, oceanic or contential) begin to converge or move apart
On continents it is called a Rift Valley or Graben. in the ocean it is call a Mid Oceanic Ridge.
When two lithospheric plates move apart, a divergent boundary is formed. This process results in the creation of new oceanic crust as magma rises to fill the gap between the plates, forming a mid-ocean ridge.
New oceanic plates/crust are created in the space of separation.
Mid-ocean ridges form at diverging oceanic plates. As the plates move apart, magma rises to fill the space, creating new oceanic crust. This process results in the formation of underwater mountain ranges along the divergent boundary.
This is an example of seafloor spreading, a process where tectonic plates diverge and new oceanic crust forms as magma rises and solidifies at mid-ocean ridges. As the plates move apart, they create new oceanic lithosphere and contribute to the Earth's tectonic activity.
Yes; at divergent/constructive boundaries, plates move apart and new oceanic lithosphere forms.
At a mid-ocean ridge, tectonic plates move apart from each other due to seafloor spreading. Magma rises up from the mantle, solidifies at the ridge, and forms new oceanic crust. This process pushes the plates away from each other, causing them to move in opposite directions.
an earthquake
an earthquake