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Hydrothermal venting at Vailulu'u Seamount: The smoking end of the Samoan chain

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Title Hydrothermal venting at Vailulu'u Seamount: The smoking end of the Samoan chain
Names Staudigel, H. (creator)
Hart, Stanley R. (creator)
Koppers, Anthony A. P. (creator)
Constable, C. (creator)
Workman, R. (creator)
Kurz, M. (creator)
Baker, E. T. (creator)
Date Issued 2004-02-10 (iso8601)
Note Copyrighted by American Geophysical Union
Abstract The summit crater of Vailulu’u Seamount, the youngest volcano in the Samoan chain, hosts an active
hydrothermal system with profound impact on the ocean water column inside and around its crater (2 km
wide and 407 m deep at a 593 m summit depth). The turbidity of the ocean water reaches 1.4 NTU, values
that are higher than in any other submarine hydrothermal system. The water is enriched in hydrothermal
Mn (3.8 ppb) and ³He (1 x 10¯¹¹ cc/g) and we measured water temperature anomalies near the crater floor
up to 0.2°C. The hydrothermal system shows complex interactions with the ocean currents around
Vailulu’u that include tidally-modulated vertical motions of about 40–50 m, and replenishment of waters
into the crater through breaches in the upper half of the crater wall. Inside and outside potential density
gradients suggest that hydrothermal venting exports substantial amounts of water from the crater (1.3 ±
0.2 x 10⁸ m³/day), which is in good agreement with fluxes obtained from a tracer release experiment
inside the crater of Vailulu’u (0.8 x 10⁸ m³/day [Hart et al., 2003]). This mass flux, in combination
with the differences in the inside and outside crater temperature, yields a power output of around
760 megawatts, the equivalent of 20–100 MOR black smokers. The Mn output of 300 kg/day is
approximately ten times the output of a single black smoker.
Genre Article
Topic hydrothermal
Identifier Staudigel, H., S. R. Hart, A. A. P. Koppers, C. Constable, R. Workman, M. Kurz, and E. T. Baker (2004), Hydrothermal venting at Vailulu’u Seamount: The smoking end of the Samoan chain, Geochem. Geophys. Geosyst., 5, Q02003.

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