Deep Sea Floor Vents

Some features like canyons and seamounts might look familiar while others such as hydrothermal vents and methane seeps are unique to the deep.

Deep sea floor vents.

The cold seawater is heated by hot magma and reemerges to form the vents. They wondered how deep ocean temperatures could change so drastically from near freezing to 400 c 750 f in such a short distance. They also realized that an entirely unique ecosystem including hundreds of new species existed around the vents. This water which can reach temperatures of 400 c eventually rises back through the.

This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level. Deep sea vents are openings in the sea floor where hot water and nutrients spew out. As shown to the right they have a rich community of species. Hydrothermal vents in the deep ocean typically form along the mid ocean ridges such as the east pacific rise and the mid atlantic ridge these are locations where two tectonic plates are diverging and new crust is being formed.

As the water comes into contact with the veins and channels of superheated molten magma the sea water is superheated. Hot seawater in hydrothermal vents does not boil because of the extreme pressure at the depths where the vents are formed. The scientists had made a fascinating discovery deep sea hydrothermal vents. Deep sea hydrothermal vents form as a result of volcanic activity on the ocean floor.

Sea water seeps down into the cracks and fissures created by the spreading of the sea floor sometimes as much as two or three miles into the earth s crust. Seawater in hydrothermal vents may reach temperatures of over 700 fahrenheit. Deep sea vent hydrothermal hot water vent formed on the ocean floor when seawater circulates through hot volcanic rocks often located where new oceanic crust is being formed. A hydrothermal vent is a lot like an underwater geyser.

Mysterious deep sea hydrothermal vents where fissures in the sea floor allow the magma in the earth s mantle to heat trapped water to high temperatures before it is pumped back into the ocean. Water seeps through cracks in the earth s crust dissolving metals and minerals as it becomes super heated from nearby magma. In either case the hot solution emerging into cold seawater precipitates mineral deposits that are rich in iron copper zinc and other metals.