1. Seawater seeps into the oceanic crust;
2. Oxygen, potassium and then calcium, sulfate and magnesium are removed from the water;
3. As water is heated up (underlying magma heats the water), iron, zinc, copper, and sulfur are dissolved;
4. Water rises back to the surface (upflow zone), where it mixes with the cold seawater, forming black metal-sulfide compounds.