A mid-ocean ridge (MOR) is a seafloor mountain system formed by plate tectonics. It typically has a depth of ~ 2,600 meters (8,500 ft) and rises about two kilometers above the deepest portion of an ...

A program designed to study the mid-ocean ridge system and enhance understanding of the relationship between the geological processes that lead to planetary renewal in the deep ocean and life forms ...

Scientists from the Woods Hole Oceanographic Institution (WHOI) have identified a new type of ocean ridge that is spreading so slowly that Earth's mantle is exposed over large regions of the sea floor ...

Ken Sims, a professor in UW’s Department of Geology and Geophysics, recently received a $325,841 National Science Foundation grant to look at understanding the processes and timescales of basalt ...

New research reveals that the Earth's ocean floor is cracking open faster and more dynamically than previously thought, significantly reshaping ocean basins.

Hydrothermal systems at mid-ocean ridges (MOR) transfer heat, metals, and carbon from Earth’s interior to the deep ocean, influencing pathways of chemical elements and compounds as they move between ...

Ocean scientists have discovered a number of mysterious holes in the seafloor that look human-made despite being located 2,540 meters (8,333 feet), or 1.6 mile underwater. The holes were discovered ...

Earth's ocean floor is not just steadily pulling apart; new research reveals rapid, dynamic cracking along mid-ocean ridges.