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The Chimney Finn

The Chimney Finn

The Chimney Finn

  • Exhibition Text

    • The water flowing through this chimney was 302 degrees Centigrade. As this superheated water mixed with the cold ocean water, a dense black cloud of precipitating minerals formed. After the chimney was collected, the stump grew nearly 3 meters in three weeks, owing to the large amount of hot water flowing through it. The yellow, metallic mineral lining the channel inside the chimney is chalcopyrite, a copper-iron sulfide. The small black crystals are the zinc-iron sulfide mineral wurtzite, and the white mineral is the calcium sulfate anhydrite. The black walls of the chimneys are made of a mixture of iron sulfide and oxide minerals and silica.

      AMNH collection

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  • For Educators

    • Topic: Earth Science

      Subtopic: Oceans

      Keywords: Hydrothermal vents, Juan de Fuca Ridge, Minerals, Ocean bottom, Oceanography

      Audience: General

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