Deep ocean minerals not only by its mineral density but cold temperature, cleanliness and trace elements. DOW is present at depths of between 250 and 1500 meters. This deep ocean current moves very slowly under the influence of density and temperature gradients. The high mineral density is attributed to the depth related pressure and the change in temperature from 20 °C+ at the surface to 8 °C at 600 meters depth generates the movement of this layer. "Very deep ocean water" has been discovered in a number of troughs in the Atlantic and Pacific Oceans. Depths can range from 1500 meters to 15
Deep ocean minerals land at Taiwan, then Okinawa and Hawaii and then arching back south, towards the Antarctica where the changing sea water temperatures from the summer sun force the deep ocean water to the surface to feed the largest micro and macro food chain on our planet. The east coast of Taiwan is directly adjacent to one of the largest reservoirs of accessible DOW. The southern islands off Japan and Hawaii also have land access to deep ocean water. Taiwan´s East Coast is ideally located to siphon deep ocean water directly to the surface from the coast. It is then micro filtered,