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Hydrothermal Vent Notes
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What is a hydrothermal vent?
A geyser on the seafloor. It continuously gushes super-hot (400oC), mineral-rich water that supports a diverse community of organisms.
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Formation of a Hydrothermal Vent
Step 1 – Sea water seeps into cracks in the sea floor around mid-ocean ridges. Step 2 – Water gets super-heated by molten rock in the asthenosphere.
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Step 3 – Super-heated water becomes saturated
with minerals from rock in the asthenosphere. Step 4 – Super-heated water is forced upward by heat & pressure & spews from the ocean floor.
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Step 5 – Minerals precipitate out of the cooled
water & steep chimneys are produced.
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Chemosynthesis Process where bacteria converts chemicals from the vents into energy
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Hydrothermal Vent Communities
Vast “extremophiles” grow near hydrothermal vents where chemosynthetic bacteria are the base of the food chain. Check em out…
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