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 ...

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 ...

Researchers from the University of Delaware’s College of Earth, Ocean and Environment helped lead the charge of underwater ...

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 ...

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

Preface / W. Roger Buck...[et al] -- Global systematics of mid-ocean ridge morphology / Christopher Small -- Linkages between faulting, volcanism, hydrothermal activity and segmentation on fast ...

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