The result when divergence occurs between two oceanic plates is SEAFLOOR SPREADING.
Seafloor spreading is a geologic process caused by the tensional stress at the mid-oceanic ridges due to convection.
This process occurs where two oceanic plates are pulling apart from each other at mid-oceanic ridges.
As these tectonic plates diverge, they create a space in which new crust forms.
In conclusion, the result when divergence occurs between two oceanic plates is SEAFLOOR SPREADING.
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