Mapping the Mendocino ridge and new volcanoes.

Obtaining detailed framework should contribute to a better understanding of the geological processes at an active plate boundary.

The Mendocino Ridge is a narrow structure on the seabed, coupled with the Mendocino fracture zone, which stretches more than 5,000 km away. in the eastern Pacific Ocean. North of the Mendocino Ridge, the Gorda plate dives under the North American plate along the Cascadia subduction zone. Near Cape Mendocino, three tectonic plates, the Pacific Plate, Gorda plate and the North American plate, come together to form a "triple junction point" migrating northward.

 

The research vessel Atlantis, from the Woods Hole Oceanographic Institution, discovered around  the ridge an area rich in small volcanoes and mounds (smaller than Seamont structure, and between 500 and 1,000 meters).

Among these mounds, the bathymetry shows a round-shaped structure like an underwater volcano, 7 km from basal diameter, having slopes estimated at 40 °, located at 400 nautical miles NW of San Francisco. She has not been named yet.

In 2009, the NOAA's ship Okeanos Explorer  revealed, north of the Mendocino ridge , a methane plume rising about 1,400 meters above a large depression in amphitheater on the ocean floor.

Sources :

- Return to Mendocino Ridge: U.S Extended Continental Shelf Project, Exploratory Mapping Expedition - link

- Center for coastal and ocean mapping joint Hydrogrephic center  - Return to Mendocino Ridge - link