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

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
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
Series:Oceanography
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

Internet

http://tos.org/oceanography/archive/25-1_hautala.pdf

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