Low-Temperature Hydrothermal Plumes in the Near-Bottom Boundary Layer at Endeavour Segment, Juan de Fuca Ridge

Low-temperature (typically 5–75°C) fluid, commonly referred to as "diffuse" hydrothermal flow, emanates from fractures over a significant portion of the Juan de Fuca Ridge seafloor in the Northeast Pacific Ocean (Kelley et al., 2012, in this issue). Although some fraction of the diffuse ef...

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Bibliographic Details

Published in:	Oceanography
Main Authors:	Susan Hautala, H. Paul Johnson, Matthew Pruis, Irene García-Berdeal, Tor Bjorklund
Format:	Article
Language:	English
Published:	The Oceanography Society 2012-03-01
Subjects:	Ridge 2000 mid-ocean ridges spreading centers hydrothermal plumes Endeavour Segment Juan de Fuca Ridge
Online Access:	http://tos.org/oceanography/archive/25-1_hautala.pdf