About the same time Morgan was forming his theory, the Canadian geologist and geophysicist J. The inactive portions of the fracture zone on the ridge flanks are scars on the ocean floor created in the transform faults. Morgan proposed that opposing plates along an oceanic ridge crest offset by fracture zones are divided by the spreading centres and transform faults. Jason Morgan, one of the several outstanding pioneers in plate tectonics, recognized that transform faults are zones where opposing lithospheric plates slip past one another. Transform faults are the only segments of fracture zones that are seismically active. The spatial orientation of transform faults is typically parallel to plate motions however, this is not always the case. A transform fault may occur in the portion of a fracture zone that exists between different offset spreading centres or that connects spreading centres to deep-sea trenches in subduction zones. Transform fault, in geology and oceanography, a type of fault in which two tectonic plates slide past one another. SpaceNext50 Britannica presents SpaceNext50, From the race to the Moon to space stewardship, we explore a wide range of subjects that feed our curiosity about space!.Learn about the major environmental problems facing our planet and what can be done about them! Saving Earth Britannica Presents Earth’s To-Do List for the 21st Century.Britannica Beyond We’ve created a new place where questions are at the center of learning.100 Women Britannica celebrates the centennial of the Nineteenth Amendment, highlighting suffragists and history-making politicians.
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