
Ridge spreading unfolds in rapid bursts, forming new ocean floor
A 2024 French study near the Amsterdam–Saint Paul Plateau shows mid-ocean ridge spreading can occur in intense bursts: dyke intrusions, sudden subsidence of a magma reservoir, and meters of horizontal extension happened within days, with some events lacking seismic signals. About 150 million cubic meters of new material were produced, and the total extension equates to roughly 38 years of normal spreading, suggesting ocean-floor creation may be episodic rather than steady.
