1. surface
2. thermocline
3. deep
rift zones
Convergent oceanic - continental and oceanic - oceanic boundaries.
Science Technical version Oceanic-Continental, Oceanic-Oceanic, and Continental-Continental. Normal Version 1.)Mixture of land and ocean 2.)Ocean 3.)Land
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
Science Technical version Oceanic-Continental, Oceanic-Oceanic, and Continental-Continental. Normal Version 1.)Mixture of land and ocean 2.)Ocean 3.)Land
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
No. Mid oceanic ridges are the places where new oceanic crust are forming.
oceanic lithosphere sinks at subduction zones but not at mid ocean ridges because at subduction zones the oceanic lithosphere is subducted, or sinks, under another plate. Oceanic Lithosphere sinks at subduction zones which are usually at convergent boundaries, but at mid-ocean ridges the plates are actually separating not coming together
subduction zones
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
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.