# data[].attributes.headline
divergent boundary: ocean - ocean (seafloor spreading) 

# data[].attributes.subject
divergent boundary: ocean - ocean (seafloor spreading) 

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

# data[].attributes.headline
divergent boundary: continental - continental 

# data[].attributes.subject
divergent boundary: continental - continental 

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

# data[].attributes.body
c-c move 2 plates ocean or continetal in opposite direction or in the same direction at different speeds

# data[].attributes.headline
convergent boundary: ocean- continental with subduction

# data[].attributes.subject
convergent boundary: ocean- continental with subduction

# data[].attributes.body
Convection currents cause the ocean plates to drive under continental plates. Ocean plates melt and form magma, and magma rises, forming volcanoes

# 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 always older colder and more dense and divers under theother

# data[].attributes.headline
convergent boundary: continental- continental no subduction 

# data[].attributes.subject
convergent boundary: continental- continental no subduction 

# data[].attributes.body
c-c causes 2 continental plates to move more toward each other. Both plates have the same density; therefore, no subdction occurs, and the 2 plates crumble up.