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Detailed Reference Information |
Baker, E.T., Fox, C.G. and Cowen, J.P. (1999). In situ observations of the onset of hydrothermal discharge during the 1998 Submarine Eruption of Axial Volcano, Juan de Fuca Ridge. Geophysical Research Letters 26: doi: 10.1029/1999GL002331. issn: 0094-8276. |
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A volcanic eruption at the summit of Axial Volcano on January 25, 1998, instantaneously created extensive and vigorous hydrothermal discharge. Moorings 2 km apart along the eruption fissure recorded temperature increases of ~0.6 ¿C up to 115 m above bottom within hours of initial seismic activity. Water temperatures at the mooring sites remained high for about 5 days, then declined steadily over the next 2 weeks. A response cruise 18 days after the eruption found hydrothermal temperature anomalies of ~0.1 ¿C over the eruption site, and a more intense and much thicker plume 20 km downstream of the eruption. We estimate the steady-state heat flux required to produce this distal plume, evidence of discharge conditions perhaps 1--13 days after the eruption, as 60--230 GW. The Axial eruption thus produced the largest vent field heat flux yet measured, but these high levels lasted less than 3 weeks. ¿ 1999 American Geophysical Union |
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Abstract |
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Keywords
Marine Geology and Geophysics, Heat flow (benthic) and hydrothermal processes, Tectonophysics, Heat generation and transport, Tectonophysics, Hydrothermal systems |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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