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Lobster

No photo available for this volcano
  • Country
  • Volcanic Region
  • Landform | Volc Type
  • Last Known Eruption
  • 15.333°S
  • 176.283°W

  • -1,500 m
    -4,921 ft

  • 243112
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number


Most Recent Bulletin Report: June 2013 (BGVN 38:05) Citation IconCite this Report

Hydrothermally active submarine volcano found in 2008

The Australian Commonwealth Scientific and Industrial Research Organization (CSIRO) announced in press releases that several large active submarine volcanoes, spreading ridges, and rift zones had been discovered in the Northwest Lau back-arc basin, NE of Fiji Island (figure 1). The discoveries were made by a team of Australian and American scientists aboard the CSIRO Marine National Facility Research Vessel Southern Surveyor in Spring 2008 (CSIRO, 2008a). While mapping previously uncharted areas for submarine volcanic and hot spring activity, the team located several volcanoes, one of which they named Lobster. The depth of Lobster is given as 1,500 m in the InterRidge Vents Database [Ver. 3.1] (2013). The location of Lobster is shown in figure 1, based on coordinates given in Lupton and others (2012). The base maps in figure 1 came from Keller and others (2008), a study primarily discussing the area in the rectangle on the larger map. The sea floor was mapped with multibeam sonar. Lobster is located ~75 km NNW of Niuafo'ou volcano/island and ~680 km NE of Suva, Fiji (figure 1). Dugong volcano lies ~60 km E of Lobster.

Figure (see Caption) Figure 1. Two maps showing (lower left) North Island, New Zealand (in black) and selected plate tectonic features along the Kermadec and Tonga trenches (hachured line with teeth on upthrown side) and (larger map) Lobster (white square) and other features such as the main spreading centers, geographical features, and subaerial volcanoes (open yellow triangles). Note Niuafo'ou volcano and island, and the location of Lobster (and Dugong, a neighboring volcano discussed in a separate Bulletin report and plotted on a larger map). Abbreviations are as follows: VFR - Valu fa ridge; ELSC - East Lau spreading center; ILSC - Intermediate Lau spreading center; CLSC - Central Lau spreading center; LETZ - Lau Extentional transform zone; PR - Peggy Ridge; NWLSC - Northwest Lau spreading center; NSC - Niuafo'ou spreading center (location of Rochambeau Rifts); NELSC - Northeast Lau spreading center; FSC - Fonualei spreading center; and MTJ - Mangatolu triple junction. Courtesy of Keller and others (2008).

Lobster volcano's caldera is 2x2.5 km in diameter with a floor at 1.5 km depth (figure 2). It was described as residing amid four radiating rift zones.

Figure (see Caption) Figure 2. (a) Multibeam sonar three-dimensional (30 kHz swathmap) image made in 2008 of Lobster which sits in what was described as the center of a rift zone and astride a spreading ridge to its W (CSIRO, 2008). Image lacks scale for depth values, but in relative terms light blue is the deepest, trending upwards through dark-to-light green, yellow, orange, and then red as the shallowest. Image from news release of CSIRO (2008b). (b) Shaded relief, contour map of Lobster caldera on the Rochambeau rifts showing part of a survey track completed in 2010 by the research vessel Dorado Discovery. Taken from Lupton and others (2012). (c) Detail map of Lobster Caldera showing locations and profiles for two chemistry hydrocasts. Inserts show vertical profiles of δ3He (deviation of the 3He/4He ratio measured at depth from the atmospheric ratio), total Mn (manganese), and %T transmission of light (a measure of suspended particles) plotted versus depth. Taken from Lupton and others (2012).

The caldera's rim is about 100 m high on the W side whereas only ~20 m high on the E side.

Dredge samples from Lobster recovered in 2008 contained olivine and plagioclase in pillow basalts. A dredge sample taken on the smooth caldera floor recovered fresh flows as well as thick, black aphyric pillows with glassy rinds.

Age. According to Arculus (2008) and Lupton and others (2012), active venting was identified in the form of high helium anomalies (δ3He), suspended particles (%T), and trace metals (manganese and iron) at 60 m off the bottom in the SE corner of the summit caldera. Lupton and others (2012) reported, in 2012, that the site was still active.

The expedition mapped the seafloor using a 30 kHz multibeam sonar with Global Positioning System (GPS) and an Inertial Motion Unit (IMU) to track the ship's position and attitude. They also made vertical conductivity, temperature, and depth (CTD) measurements as well as rock dredging. In addition, by lowering the CTD package up and down a few hundred meters from the bottom, while moving the ship, they obtained a far greater density of data. This technique, often informally referred to as a CTD tow-yo, is effective for mapping and sampling hydrothermal plumes.

References. Arculus, R.J., 2008, Marine National Facility RV Southern Survey 2008 Program: Voyage Summary SS07/2008 Northern Lau Vents Expedition (NoLauVE), 23 p (URL: http://www.cmar.csiro.au/datacentre/process/data_files/cruise_docs/SS200807sum.pdf).

CSIRO, 2008a, Active submarine volcanoes found near Fiji, CSIRO web site (URL: http://www.csiro.au/Organisation-Structure/Divisions/Earth-Science--Resource-Engineering/SubmarineVolcanoes.aspx).

CSIRO, 2008b, Active submarine volcanoes found near Fiji, CSIRO media release (URL: http://www.scienceimage.csiro.au/mediarelease/mr08-93.html).

de Ronde, C.E.J, Baker, ET, Massoth, G.J, Lupton, J.E, Wright, I.C., Feely, R.A., and Greene, R.R., 2001, Intra-oceanic subduction-related hydrothermal venting, Kermadec volcanic arc, New Zealand, Earth and Planetary Science Letters, v. 193, p. 359-369.

Graham, I.J., Reyes, A.G., Wright, I.C., Peckett, K.M., Smith, I.E.M., and Arculus, R.J., 2008, Structure and petrology of newly discovered volcanic centers in the northern Kermadec–southern Tofua arc, South Pacific Ocean, Journal of Geophysical Research, v. 113, B08S02, doi:10.1029/2007JB005453.

InterRidge Vents Database Ver. 3.1, 2013, Vent Fields (URL: http://www.interridge.org/irvents/ventsfields?).

Keller, N.S., Arculus, R.J., Hermann, J., and Simon, R., 2008, Submarine back-arc lava with arc signature: Fonualei Spreading Center, northeast Lau Basin, Tonga, Journal of Geophysical Research, v. 113, B08S07, doi:10.1029/2007JB005451.

Lupton, J.E., Arculus, R.J., Resing, J., Massoth, G.J., Greene, R.R., Evans, L.J., and Buck, N., 2012, Hydrothermal activity in the Northwest Lau Backarc Basin: Evidence from water column measurements, Geochemistry, Geophysics, Geosystems, v. 13, no. 5, doi: 10.1029/2011GC003891.

Information Contacts: Commonwealth Scientific and Industrial Research Organization (CSIRO) (URL: http://www.csiro.au).

The Global Volcanism Program has no Weekly Reports available for Lobster.

Bulletin Reports - Index

Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Click on the index link or scroll down to read the reports.

06/2013 (BGVN 38:05) Hydrothermally active submarine volcano found in 2008




Information is preliminary and subject to change. All times are local (unless otherwise noted)


June 2013 (BGVN 38:05) Citation IconCite this Report

Hydrothermally active submarine volcano found in 2008

The Australian Commonwealth Scientific and Industrial Research Organization (CSIRO) announced in press releases that several large active submarine volcanoes, spreading ridges, and rift zones had been discovered in the Northwest Lau back-arc basin, NE of Fiji Island (figure 1). The discoveries were made by a team of Australian and American scientists aboard the CSIRO Marine National Facility Research Vessel Southern Surveyor in Spring 2008 (CSIRO, 2008a). While mapping previously uncharted areas for submarine volcanic and hot spring activity, the team located several volcanoes, one of which they named Lobster. The depth of Lobster is given as 1,500 m in the InterRidge Vents Database [Ver. 3.1] (2013). The location of Lobster is shown in figure 1, based on coordinates given in Lupton and others (2012). The base maps in figure 1 came from Keller and others (2008), a study primarily discussing the area in the rectangle on the larger map. The sea floor was mapped with multibeam sonar. Lobster is located ~75 km NNW of Niuafo'ou volcano/island and ~680 km NE of Suva, Fiji (figure 1). Dugong volcano lies ~60 km E of Lobster.

Figure (see Caption) Figure 1. Two maps showing (lower left) North Island, New Zealand (in black) and selected plate tectonic features along the Kermadec and Tonga trenches (hachured line with teeth on upthrown side) and (larger map) Lobster (white square) and other features such as the main spreading centers, geographical features, and subaerial volcanoes (open yellow triangles). Note Niuafo'ou volcano and island, and the location of Lobster (and Dugong, a neighboring volcano discussed in a separate Bulletin report and plotted on a larger map). Abbreviations are as follows: VFR - Valu fa ridge; ELSC - East Lau spreading center; ILSC - Intermediate Lau spreading center; CLSC - Central Lau spreading center; LETZ - Lau Extentional transform zone; PR - Peggy Ridge; NWLSC - Northwest Lau spreading center; NSC - Niuafo'ou spreading center (location of Rochambeau Rifts); NELSC - Northeast Lau spreading center; FSC - Fonualei spreading center; and MTJ - Mangatolu triple junction. Courtesy of Keller and others (2008).

Lobster volcano's caldera is 2x2.5 km in diameter with a floor at 1.5 km depth (figure 2). It was described as residing amid four radiating rift zones.

Figure (see Caption) Figure 2. (a) Multibeam sonar three-dimensional (30 kHz swathmap) image made in 2008 of Lobster which sits in what was described as the center of a rift zone and astride a spreading ridge to its W (CSIRO, 2008). Image lacks scale for depth values, but in relative terms light blue is the deepest, trending upwards through dark-to-light green, yellow, orange, and then red as the shallowest. Image from news release of CSIRO (2008b). (b) Shaded relief, contour map of Lobster caldera on the Rochambeau rifts showing part of a survey track completed in 2010 by the research vessel Dorado Discovery. Taken from Lupton and others (2012). (c) Detail map of Lobster Caldera showing locations and profiles for two chemistry hydrocasts. Inserts show vertical profiles of δ3He (deviation of the 3He/4He ratio measured at depth from the atmospheric ratio), total Mn (manganese), and %T transmission of light (a measure of suspended particles) plotted versus depth. Taken from Lupton and others (2012).

The caldera's rim is about 100 m high on the W side whereas only ~20 m high on the E side.

Dredge samples from Lobster recovered in 2008 contained olivine and plagioclase in pillow basalts. A dredge sample taken on the smooth caldera floor recovered fresh flows as well as thick, black aphyric pillows with glassy rinds.

Age. According to Arculus (2008) and Lupton and others (2012), active venting was identified in the form of high helium anomalies (δ3He), suspended particles (%T), and trace metals (manganese and iron) at 60 m off the bottom in the SE corner of the summit caldera. Lupton and others (2012) reported, in 2012, that the site was still active.

The expedition mapped the seafloor using a 30 kHz multibeam sonar with Global Positioning System (GPS) and an Inertial Motion Unit (IMU) to track the ship's position and attitude. They also made vertical conductivity, temperature, and depth (CTD) measurements as well as rock dredging. In addition, by lowering the CTD package up and down a few hundred meters from the bottom, while moving the ship, they obtained a far greater density of data. This technique, often informally referred to as a CTD tow-yo, is effective for mapping and sampling hydrothermal plumes.

References. Arculus, R.J., 2008, Marine National Facility RV Southern Survey 2008 Program: Voyage Summary SS07/2008 Northern Lau Vents Expedition (NoLauVE), 23 p (URL: http://www.cmar.csiro.au/datacentre/process/data_files/cruise_docs/SS200807sum.pdf).

CSIRO, 2008a, Active submarine volcanoes found near Fiji, CSIRO web site (URL: http://www.csiro.au/Organisation-Structure/Divisions/Earth-Science--Resource-Engineering/SubmarineVolcanoes.aspx).

CSIRO, 2008b, Active submarine volcanoes found near Fiji, CSIRO media release (URL: http://www.scienceimage.csiro.au/mediarelease/mr08-93.html).

de Ronde, C.E.J, Baker, ET, Massoth, G.J, Lupton, J.E, Wright, I.C., Feely, R.A., and Greene, R.R., 2001, Intra-oceanic subduction-related hydrothermal venting, Kermadec volcanic arc, New Zealand, Earth and Planetary Science Letters, v. 193, p. 359-369.

Graham, I.J., Reyes, A.G., Wright, I.C., Peckett, K.M., Smith, I.E.M., and Arculus, R.J., 2008, Structure and petrology of newly discovered volcanic centers in the northern Kermadec–southern Tofua arc, South Pacific Ocean, Journal of Geophysical Research, v. 113, B08S02, doi:10.1029/2007JB005453.

InterRidge Vents Database Ver. 3.1, 2013, Vent Fields (URL: http://www.interridge.org/irvents/ventsfields?).

Keller, N.S., Arculus, R.J., Hermann, J., and Simon, R., 2008, Submarine back-arc lava with arc signature: Fonualei Spreading Center, northeast Lau Basin, Tonga, Journal of Geophysical Research, v. 113, B08S07, doi:10.1029/2007JB005451.

Lupton, J.E., Arculus, R.J., Resing, J., Massoth, G.J., Greene, R.R., Evans, L.J., and Buck, N., 2012, Hydrothermal activity in the Northwest Lau Backarc Basin: Evidence from water column measurements, Geochemistry, Geophysics, Geosystems, v. 13, no. 5, doi: 10.1029/2011GC003891.

Information Contacts: Commonwealth Scientific and Industrial Research Organization (CSIRO) (URL: http://www.csiro.au).

The Global Volcanism Program has no synonyms or subfeatures listed for Lobster.

Eruptive History

The Global Volcanism Program is not aware of any Holocene eruptions from Lobster. If this volcano has had large eruptions (VEI >= 4) prior to 12,000 years ago, information might be found on the Lobster page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

Deformation History

There is no Deformation History data available for Lobster.

Emission History

There is no Emissions History data available for Lobster.

Photo Gallery

The Global Volcanism Program has no photographs available for Lobster.

GVP Map Holdings

Maps are not currently available due to technical issues.

The maps shown below have been scanned from the GVP map archives and include the volcano on this page. Clicking on the small images will load the full 300 dpi map. Very small-scale maps (such as world maps) are not included.

Smithsonian Sample Collections Database

There are no samples for Lobster in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.

External Sites