# data[].attributes.body
makes new crust and forms rifts and ridges

# data[].attributes.body
new crust gets pushed up and old crust gets pushed down

# data[].attributes.body
seafloor spreading

# data[].attributes.body
Oceanic sinks

# data[].attributes.body
Seafloor spreading (ridge)

# data[].attributes.body
causes rift valleys on land and mountains in water

# data[].attributes.body
moves away from each other

# data[].attributes.body
sea floor spreading

# data[].attributes.body
gets moved apart

# data[].attributes.body
Sea floor spreading

# data[].attributes.body
new crust is formed and old crust is destroyed

# data[].attributes.body
The plates don't subduct, the just create rift valleys and ridges.
"Rift"s apart, Rifts are formed on land (Such as Iceland) while Ridges are underwater (Such as the Mid Atlantic Ridge)
-Lillian Chester

# data[].attributes.body
Makes new crust

# data[].attributes.body
Divides( only on with D)

# data[].attributes.body
ridge

# data[].attributes.body
rifts and ridges

# data[].attributes.body
goes away