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ReportsA Sea-Floor Spreading Event Captured by Seismometers
Two-thirds of Earth's surface is formed at mid-ocean ridges, yet sea-floor spreading events are poorly understood because they occur far beneath the ocean surface. At 9°50'N on the East Pacific Rise, ocean-bottom seismometers recently recorded the microearthquake character of a mid-ocean ridge eruption, including precursory activity. A gradual ramp-up in activity rates since seismic monitoring began at this site in October 2003 suggests that eruptions may be forecast in the fast-spreading environment. The pattern culminates in an intense but brief (
1 Lamont-Doherty Earth Observatory (LDEO) of Columbia University, Palisades, NY 10964, USA. * To whom correspondence should be addressed. E-mail: tolstoy{at}ldeo.columbia.edu
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Science. ISSN 0036-8075 (print), 1095-9203 (online)