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Cobb Seamount
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Cobb Seamount is a (underwater volcano) and located west of , Washington, United States. Cobb Seamount is one of the seamounts in the Cobb–Eickelberg Seamount chain, a chain of underwater volcanoes created by the that terminates near the coast of Alaska. It lies just west of the Cascadia subduction zone, and was discovered in August 1950 by the U.S. Fish and Wildlife Service fisheries R/V John N. Cobb (FWS 1601). noaa.gov AFSC Historical Corner: John N. Cobb, Establishing a Rich Legacy nRetrieved August 25, 2018 By 1967, over of soundings and dozens of samples from the seamount had been collected.

Cobb Seamount is geologically interesting for its terraced, pinnacle structure, and its biological community. Like many other seamounts, Cobb Seamount acts as a biological center of diversity, and supports a dense oceanic ecosystem. Relatively convenient access and an interesting biological setting have made the seamount an object of several scientific cruises and dives.


Geology
Cobb Seamount lies off the coast of Washington, in the -deep . Argon–argon dating of basalts retrieved from the volcano show that it is about 3.3 million years in age. Cobb Seamount's slopes average 12° in grade, and are indented by four prominent terraces at various depths; this morphology is partly the result of sub-aerial exposure and wave erosion at sea level and partly due to volcanic processes far below wave base.Chaytor, J. D., R. A. Keller, R. A. Duncan, and R. P. Dziak (2007), Seamount morphology in the Bowie and Cobb hot spot trails, Gulf of Alaska, Geochem. Geophys. Geosyst., 8, Q09016, doi:10.1029/2007GC001712 The volcano's pinnacle is generally flat, and is defined by a pocketed area approximately by in size.


Biology
Although it is one of over 100 underwater features in the region, Cobb Seamount is the only one known to extend well upwards into the region of the ocean penetrated by light. Like many other seamounts, Cobb Seamount is a local biological hotspot and functions as an "island of stability" for local organisms. It supports an extensive fish population, mostly species and especially Sebastes miniatus. Bird life has been noted in the area of its summit, indicating that it is a prime fishing ground. For the complete known species inventory of Cobb Seamount, see Du Preez et al., 2015.

The summit of the volcano is dominated by a carpet of Hinnites multirugosus, which forms the base of a dense ecosystem of and other small, sessile organisms. The species is otherwise scarce in its distribution in the Pacific; its abundance is accommodated by the scarcity of its chief predator, the Orthasterias koehleri. The reason for the sea star's disparity is unknown, as it is extremely common on nearby seamounts.

The steeper flanks of the volcanoes are carpeted by of the and . In some areas, Borgiola pustulosa is more common. Red-colored colonies of and related species predominant the ecosystem, which includes , , , , and . While overall the species diversity on the seamount is lower than a comparable area on the surface, the species present have grown in greater numbers and have formed larger colonies, to the point that there was little to no bare rock surface on the seamount, and none has been found in expeditionary dives. Some endemism to the seamount has also been noted.

The seamount's abundant sea life has made it a target for heavy fishing since the 1960s. However, the fishing is very difficult to monitor, since Cobb lies outside of the U.S. Exclusive Economic Zone and therefore fishing vessels are not regulated. It is known that it has been the site of trawling, gill net, and long-line fishing for some time, mostly by the Japanese and fleets. In 1993, the National Oceanic and Atmospheric Administration sponsored a study on the seamount, which concluded that concerns about overfishing at the seamount have some merit. The study also notes that fishermen there have different fishing patterns, because of different physical conditions at the seamount.


Expeditions
Since its discovery in August 1950 by R/V John N. Cobb, Cobb Seamount has been the target of passing cruises and sampling missions, totaling to over of soundings and dozens of samples by 1967. In 1968, Project Sea Use,
(2025). 9780674972018, Harvard University Press.
a multi-party expedition aboard the United States Coast and Geodetic Survey research vessel USC&GS Oceanographer (R 101), visited the seamount, and much of what was initially known about it stems from the expedition. This was followed in 1970, two expeditions in the late 1970s, and 1992, however all have been fairly limited in scope. In 2012, an extensive scientific survey of Cobb Seamount was led jointly by Fisheries and Oceans Canada (DFO) and the United States National Oceanographic and Atmospheric Administration (NOAA). The survey used, among other methods, remotely operated vehicles (ROVs) and autonomous underwater vehicles (AUVs) to conduct high-resolution surveys of the benthic () community above a depth of 1200 meters (3,937 feet).

There was tentative expert interest in installing an experimentation platform on Cobb Seamount. The seamount is an easily accessible distance from shore, and would give scientists the ability to work with Cobb Seamount's unique, isolated, and scientifically significant seamount biology. The idea was proposed by P. L. Peterson et al. in a presentation to the Offshore Technology Conference in 1969.

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