Manganese concentration of hydrothermal plume at Pele’s Pit, Loihi Seamount, Hawaii

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Manganese concentration of hydrothermal plume at Pele’s Pit, Loihi Seamount, Hawaii

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dc.contributor.author Min, Brian
dc.date.accessioned 2012-03-30T23:39:55Z
dc.date.available 2012-03-30T23:39:55Z
dc.date.issued 2011-03
dc.identifier.uri http://hdl.handle.net/1773/19685
dc.description Senior thesis written for Oceanography 444 en_US
dc.description.abstract Manganese (Mn) in hydrothermal vent plumes is an indicator of the vent characteristics that spawned the plume. Mn concentrations in Pele's Pit in Hawaii and the Cleft segment in the Juan de Fuca Ridge were compared. Mn was lower in Pele's Pit, an indication of weaker seismic activity. en_US
dc.language.iso en_US en_US
dc.subject Hydrothermal vents--Loihi seamount--Observations en_US
dc.subject Chemical oceanography--Loihi seamount en_US
dc.title Manganese concentration of hydrothermal plume at Pele’s Pit, Loihi Seamount, Hawaii en_US
dc.type Other en_US


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