Scientists Discover First Seafloor Vents On Ultraslow-spreading Ridge

Scientists Discover First Seafloor Vents On Ultraslow-spreading Ridge

Science Daily — Scientists have found one of the largest fields of seafloor vents gushing super-hot, mineral-rich fluids on a mid-ocean ridge that, until now, remained elusive to the ten-year hunt to find them.

The Southwest Indian Ridge is a spreading center between the African tectonic plate (top left, yellow-orange) and the Antarctic plate (bottom left, red). (Credit: NOAA Geophysical Data Center)

“The discovery of the first active vents ever found on an ultraslow-spreading ridge is a significant milestone event,” said Jian Lin, leader of a team of Woods Hole Oceanographic Institution (WHOI) scientists who participated in a Chinese expedition to the remote Southwest Indian Ridge in the Indian Ocean in February and March.

Since deep-sea hydrothermal vents were first discovered 30 years ago in the Pacific Ocean, scientists have studied them all along the Mid-Ocean Ridge, a 40,000-mile-long mountain range that zigzags through the middle of the world’s ocean basins like a giant zipper. The ridge marks the area where the Earth’s giant tectonic plates spreads apart and new ocean crust forms from hot lava rising from deep within Earth’s mantle.

Most studies of the chimney-like vent structures have taken place along ridges in the “fast-spreading” East Pacific Rise (100 to 200 millimeters per year) and the “slow-spreading” Mid-Atlantic Ridge (20 to 40 millimeters per year). Only in recent years have scientists explored “ultraslow-spreading ridges” (less than 20 millimeters per year) in the Arctic and Indian Oceans—remote areas tough to get to, and therefore the least studied.

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Last Edited by SPUD on 10/18/2011 12:51 PM