The correct response for how mineral deposits form at divergent ocean plate boundaries is:
Metals dissolve in superheated water, forming minerals when the water cools.
At divergent boundaries, such as mid-ocean ridges, seawater seeps into the ocean floor and interacts with magma. This interaction creates superheated hydrothermal vents, where metals are dissolved in the water. As the water rises and cools, the metals precipitate out, leading to the formation of mineral deposits.