The deep oceans are far from flat. They feature ridges, trenches, seamounts, and valleys, creating a diverse and dramatic ...
PROF. v. BEMMELEN recently asked me to calculate the thermal effect of Serpentinization of an upper layer of the mantle, if fresh peridotite is supplied through a process of convexion currents or ...
The basement was formed about 60 million years ago at the mid-ocean ridge crest, and the uplift of the ridge and opening of Kings Trough occurred about 27 million years ago.
in hydrothermal flux near oceanic ridges. They suggest this drop may have caused significant changes in the ocean's chemistry. In previous work, some of the same researchers proposed that the 35% ...