File:Chimney-hires.jpg

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English: A hot vent (255 degrees C) near the top of a 38-m-high sulfide chimney in the Loloa Kakai vent field on the Fonualei rift, sampled during dive Q233. The vent fluids forming these giant columnar chimneys are a result of water/rock reaction deep below the seafloor. They have a pH of approximately 5.2, not nearly as acidic as Volcano O cone fluids. Image courtesy of MARUM, University of Bremen and NOAA-Pacific Marine Environmental Laboratory. For educational and outreach purposes only. Image courtesy of MARUM, University of Bremen and NOAA-Pacific Marine Environmental Laboratory. Image courtesy of Submarine Ring of Fire 2012: NE Lau Basin, NOAA-OER.
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Source https://oceanexplorer.noaa.gov/explorations/12fire/logs/sept15/media/chimney-hires.jpg
Author NOAA Vents Program

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This image is in the public domain because it contains materials that originally came from the U.S. National Oceanic and Atmospheric Administration, taken or made as part of an employee's official duties.

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current23:15, 2 February 2023Thumbnail for version as of 23:15, 2 February 20231,920 × 1,080 (362 KB)Reego41 (talk | contribs)Uploaded a work by NOAA Vents Program from https://oceanexplorer.noaa.gov/explorations/12fire/logs/sept15/media/chimney-hires.jpg with UploadWizard

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