# data[].attributes.body
Convection currents pull 2 ocean plates apart hot less dense magma rises in the middle, coolest hardens pushing the old seafloor out.

Ex: Mid-Ocean Ridge

# data[].attributes.body
Convection currents push 2 continental plates apart magma rises in the middle cools hardens then sinks forming a valley

Ex: Rift valleys

# data[].attributes.body
C-C more plates ocean or continental 2 in the opposite direction or the same direction at different speeds

Ex: Earthquake

# data[].attributes.body
Convection currents cause denser ocean plates to dive under continental plate ocean melt forms magma and magma rises forming a volcano

Ex: Mountains, Ocean Trenches, Volcanos

# data[].attributes.headline
Convergent Boundary: Ocean-Ocean with Subduction 

# data[].attributes.subject
Convergent Boundary: Ocean-Ocean with Subduction 

# data[].attributes.body
Convection currents cause 2 ocean plates to move towards each other plates are always older colder and dense and dive under the other plate.

Ex: Ocean Trenches Volcanic Islands

# data[].attributes.body
CC causes 2 continental plates to move toward each other plates are the same density there no subduction occurs and the 2 plates crumble up

Ex: Mountains