Adams Seamount

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Summit depth39 m (128 ft)[1]
Height3,500 m (11,500 ft)
Coordinates25°22′S 129°16′W / 25.367°S 129.267°W / -25.367; -129.267
Adams Seamount, Forty Mile Reef
Summit depth39 m (128 ft)[1]
Height3,500 m (11,500 ft)
Location
LocationPacific Ocean, SW of Pitcairn Island
Coordinates25°22′S 129°16′W / 25.367°S 129.267°W / -25.367; -129.267
Geology
Last eruption50 BCE ± 1000 years

Adams Seamount (also known as Forty Mile Reef[2]) is a submarine volcano above the Pitcairn hotspot in the central Pacific Ocean about 100 kilometres (62 mi) southwest of Pitcairn Island.

Adams is part of a field of about 90 seamounts 90 kilometres (56 mi) east-southeast away from Pitcairn Island, and the largest of these.[3] Adams lies southeast of another large seamount, Bounty Seamount.[4] Most of these seamounts except for Adams and Bounty are less than 0.5 kilometres (0.31 mi) high.[5] They were discovered in 1989 by the RV Sonne research ship.[6]

It is a conical[7] seamount rising 3,500 metres (11,483 ft) from the sea floor to about 39 metres (128 ft)[1] or 59–75 metres (194–246 ft) below the surface of the ocean.[2] The total volume of the seamount, whose base has a diameter of about 30 kilometres (19 mi), is about 858 cubic kilometres (206 cu mi).[8] Adams has two summits,[9] and coral and sand derived from coral has been found on Adams.[5] Given its height, during the Last Glacial Maximum Adams was likely an island.[10]

Its slopes are covered by recent lava flows, volcanic debris and hyaloclastite.[9] Lava flows feature aa lava characteristics and lava tubes, while deeper parts of the edifice are covered with lapilli and scoria.[11] Parasitic vents form cones and mounds on its flanks.[12]

Geology

Adams and the other seamounts were created by the Pitcairn hotspot, and these seamounts are its present-day location.[3] This hotspot is one among several hotspots in the Pacific Ocean, along with the Austral hotspot, Hawaii hotspot, Louisville hotspot, Samoa hotspot and Society hotspot.[6] The seamounts rise from a 30 million years old crust.[13]

Alkali basalt, trachyte[9] and tholeiite have been dredged from Adams Seamount.[14]

Eruption history

Biology

References

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