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.
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.
Because oceanic lithosphere is more dense than continental lithosphere.
That's because the oceanic lithosphere is more dense, and less bouyant than the continental lithosphere.
The oceanic lithosphere is denser than the continental lithosphere.
No, it is destroyed at convergent boundaries.
Convergent oceanic-continental boundary
An island arc forms.
The three types of convergent plate boundaries are Oceanic-Oceanic, Continental-Continental, Continental-Oceanic.
Rift Valleys are the most common at oceanic-continental convergent 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.
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.
No, it is destroyed at convergent boundaries.
Convergent oceanic-continental boundary
There are three types of convergent boundaries: Oceanic, continental, and continental-oceanic convergent boundaries. Continental-continental convergent boundaries form mountain ranges. Continental-oceanic boundaries result in subduction zones and the recycling of lithosphere. The continental side of the boundary may form a mountain range. Oceanic-oceanic form deep oceanic trenches and sometimes volcanoes.
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.
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
The three types of convergent plate boundaries are Oceanic-Oceanic, Continental-Continental, Continental-Oceanic.
Oceanic lithosphere is destroyed when it is subducted at a convergent plate boundary and forced into the mantle where it melts. You shouldn't use the internet to look up answers on a test. You should use your notes and textbook! DW Thanks for the answer but um, What about people in online school, where the only "textbook" you get is an agenda? yeah the awnser for Gradpoint is Convergent Boundary
An island arc forms.
trench
Convergent oceanic - continental and oceanic - oceanic boundaries.