Yes; at divergent/constructive boundaries, plates move apart and new oceanic lithosphere forms.
There are two kinds of plates- continental lithosphere and oceanic lithosphere. There are many types of plate boundaries, like convergent, divergent, transform, and more. Continental lithosphere is granite and oceanic is basalt.
Plate boundaries, essentially, are the areas where two lithospheric plates meet. When this happens, one of three things can happen. Plates can move apart from each other, creating divergent boundaries. Plates can collide together, created convergent boundaries. Or plates can rub against each other in a parallel motion, created transform fault boundaries. Divergent boundaries, usually between two oceanic plates, creates an upswelling of magma from the lithosphere. Convergent boundaries, usually between oceanic and continental plates, causes the oceanic plate to subduct underneath the continental plate, leading to the destruction of seafloor. Transform fault boundaries neither destroy nor create lithosphere.
divergent
No, divergent boundaries do not cause the formation of mountains. Instead, mountains are typically formed at convergent boundaries where tectonic plates collide. Divergent boundaries are where plates move away from each other, creating rifts and oceanic ridges.
divergent boundaries mostly occur when 2 tectonic plates move apart from each other and this is due to the currents movement. On earth, the form drift vallies and fault. Example can be san andreas fault on western side of united state of america.
divergent boundaries
Yes, divergent boundaries can occur between continental and oceanic crust. An example of this is the Mid-Atlantic Ridge, where new oceanic crust is formed as the North American and Eurasian plates move apart. This process leads to seafloor spreading and the creation of new oceanic lithosphere.
On the seafloor. Yes, the mid oceanic ridges are all divergent boundaries.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
There are two kinds of plates- continental lithosphere and oceanic lithosphere. There are many types of plate boundaries, like convergent, divergent, transform, and more. Continental lithosphere is granite and oceanic is basalt.
continetal and oceanic
Plate boundaries, essentially, are the areas where two lithospheric plates meet. When this happens, one of three things can happen. Plates can move apart from each other, creating divergent boundaries. Plates can collide together, created convergent boundaries. Or plates can rub against each other in a parallel motion, created transform fault boundaries. Divergent boundaries, usually between two oceanic plates, creates an upswelling of magma from the lithosphere. Convergent boundaries, usually between oceanic and continental plates, causes the oceanic plate to subduct underneath the continental plate, leading to the destruction of seafloor. Transform fault boundaries neither destroy nor create lithosphere.
divergent, transform and convergent divergent plate boundaries move away from each other, convergent plate boundaries move toward each other, and transform plate bounties slide past each other.
oceanic ridges
Oceanic or continental rifts.
it makes mid-oceanic ridges
The 3 general types are constructive, destructive, and conservative boundaries. Constructive (divergent) - plates move away from each other, typically creating a rift Destructive (convergent) - one plate will be subducted, or continental plates collide Conservative (transform) - plates grind past each other, stalling and slipping