Unnamed

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  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 85.58°N
  • 85°E

  • -3800 m
    -12464 ft

  • 377020
  • Latitude
  • Longitude

  • Summit
    Elevation

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    Number

The Global Volcanism Program has no activity reports for Unnamed.

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

Index of Monthly Reports

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.

03/2001 (BGVN 26:03) Two recently active volcanoes discovered beneath Arctic Ocean pack ice

05/2009 (BGVN 34:05) Undated explosive volcanism at depth on Arctic mid-ocean ridge


Contents of Monthly Reports

All information contained in these reports is preliminary and subject to change.

All times are local (= UTC + 6 hours)

03/2001 (BGVN 26:03) Two recently active volcanoes discovered beneath Arctic Ocean pack ice

A sonar survey along the ultraslow-spreading Gakkel Ridge by the USS Hawkbill submarine revealed two previously undiscovered volcanoes beneath the pack ice of the Arctic Ocean. Lineated magnetic anomalies over the entire ridge suggested that seafloor volcanism occurred there, but theoretical modeling predicted that melt production should be extremely low given the ~1.0-1.3 cm/year rate at which the ridge spreads. Sidescan and bathymetric data from the East Gakkel Ridge survey showed two amorphously shaped topographic highs with 1,000 m (eastern volcano) and 500 m (western volcano) of relative relief, with a highly reflective acoustic character. The high reflectivity was interpreted to indicate a lack of significant sedimentary cover on young basaltic flows.

Edwards and others (2001) reported that "portions of the strongly reflective regions . . . abut lineaments, consistent with the ponding of lava against fault scarps. Terminations of acoustically reflective terrain in regions devoid of lineaments have shapes characteristic of lava flow fronts . . .. These flow toes are radially distributed about the two topographic highs. The morphology of the strongly reflective regions is consistent with submarine volcanic flow systems mapped at other mid-ocean ridges by acoustic and optical [methods] . . . . The two acoustically reflective regions are thus probably volcanoes that are largely devoid of sediment cover, and therefore erupted recently. The presence of these two young volcanoes covering approximately 20% of the 3,750 km2 surveyed along . . . the eastern Gakkel Ridge, proves that significant volcanism occurs at ultraslow spreading rates."

During January-September 1999 global seismic networks detected an earthquake swarm corresponding to the approximate location of the W volcano discovered along the East Gakkel Ridge (86°N, 85°E). About 75% of the swarm occurred before the end of May. Edwards and others (2001) noted that "The correlation between the locations of the earthquake epicenters and the location of the strongly reflective, untectonized W volcano together with the volcanic character of the seismic record provide evidence that lava erupted on the E Gakkel Ridge . . . . Because 12-kHz sonars can penetrate through thin sediments covering acoustically reflective lavas, it is possible that no eruption occurred on Gakkel Ridge in 1999; however, historical global seismic records indicate that this is the only earthquake swarm detected on Gakkel Ridge in about 100 years."

Reference. Edwards, M.H., Kurras, G.J., Tolstoy, M., Bohnenstiehl, D.R., Coakley, B.J., and Cochran, J.R., 2001, Evidence of recent volcanic activity on the ultraslow-spreading Gakkel Ridge: Nature, v. 409, no. 6822, p. 808-812.

Information Contacts: M.H. Edwards, Hawaii Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, POST 815, 1680 East-West Road, Honolulu, Hawaii 96822 USA (Email: margo@soest.hawaii.edu, URL: http://imina.soest.hawaii.edu/hmrg/).

05/2009 (BGVN 34:05) Undated explosive volcanism at depth on Arctic mid-ocean ridge

A sonar survey in 2001 along the ultraslow-spreading Gakkel Ridge (formerly known as the Nansen Cordillera and Arctic Mid-Ocean Ridge) by the USS Hawkbill submarine and the U.S. Coast Guard icebreaker Healy revealed two previously undiscovered volcanoes beneath the pack ice of the Arctic Ocean (BGVN 26:03). In July 2007, a research team led by Woods Hole Oceanographic Institution (WHOI) uncovered evidence of explosive volcanic eruptions in the same area of the seafloor.

At a depth of ~ 4 km, researchers found fresh, unweathered, jagged, glassy fragments of rock (pyroclastic deposits) spread out over an area of ~ 10 km2 around a series of small volcanic craters on the Gakkel Ridge (figure 1). According to WHOI geophysicist Rob Reves-Sohn, chief scientist of the expedition, as quoted in the 14 August 2008 issue of Oceanus, "These are the first pyroclastic deposits we've ever found in such deep water, at oppressive pressures that inhibit the formation of steam, and many people thought this was not possible. This means that a tremendous blast of carbon dioxide was released into the water column during the explosive eruption." Although no speculation was made by the scientists as to the age of the eruption(s) that caused these pyroclastics, the fresh nature of these surficial materials argue to their recency.

Figure 1. Detailed bathymetry (30-m grid spacing) of the Gakkel Ridge at 85°E in the Arctic Ocean based on July 2007 WHOI research cruise. The inset map shows the location of the 85°E segment (yellow star) along the Gakkel ridge (red line) in the Arctic basin. The main panel shows illuminated, color bathymetry of the 85° E segment acquired during the Arctic Gakkel Vents (AGAVE) expedition. The axial valley contains large numbers of distinctive, cratered volcanoes, including a cone on a fault terrace of the northern valley wall. Photographic bottom surveys were conducted along profiles shown as thin black lines on the map. Pyroclastic deposit samples were collected at sites shown by white circles, and the photographs shown in figure 2 were taken at the sites shown by the lettered (red) stars. Named features include two volcanic ridges in the center of the axial valley (Jessica's hill and Duque's hill), and three cratered volcanoes along a ridge-parallel fissure to the S (Oden, Thor, and Loke). Courtesy of Sohn and others (2008).

According to Cochran (2008), the Gakkel Ridge is the slowest spreading portion of the global system of mid-ocean ridges. Total spreading rates vary from 12.8 mm/yr near Greenland to 6.5 mm/yr at the Siberian margin.

A recent article by Sohn and others (2008) concerning the July 2007 expedition noted that roughly 60% of the Earth's outer surface is composed of oceanic crust formed by volcanic processes at mid-ocean ridges. Although only a small fraction of this vast volcanic terrain has been visually surveyed or sampled, the available evidence suggests that explosive eruptions are rare on mid-ocean ridges, particularly at depths below the critical point for seawater (a depth of ~ 3,000 m). A pyroclastic deposit has never been observed on the sea floor below 3,000 m, presumably because the volatile content of mid-ocean-ridge basalts is generally too low to produce the gas fractions required for fragmenting a magma at such high hydrostatic pressure. Liu and others (2008) reported on recent analyses of many major and trace element collected from Gakkel Ridge.

The July 2007 expedition acquired photographs and video images of 'zero-age' volcanic terrain along the ridge and beneath the ice-cover ocean's surface. The axial valley at 4,000 m water depth was blanketed with unconsolidated pyroclastic deposits. Those included bubble-wall fragments (limu o Pele, also know as Pele's seaweed–fragments of large glass bubbles that shatter into pieces of curved, paper-thin, bubble walls), covering a large (greater than 10 km2) area (figure 2). At least 13.5 weight percent CO2 is necessary to fragment magma at these depths, which is about tenfold above the highest values previously measured in a mid-ocean-ridge basalt.

Figure 2. Photographs of pyroclastic deposits taken during July 2007 WHOI research cruise. (a) One frame from a high-definition video camera taken on the S side of Duque's hill (see figure 1 for location). About 10 cm (visually estimated and confirmed during sampling) of pyroclastic material is piled atop a high-standing, weathered, pillow feature. The exoskeleton of an as yet unidentified species of hexactinellid sponge (glass sponge, or a sponge with a skeleton made of 4- and/or 6-pointed siliceous spicules) is visible in the foreground. (b) High-definition video frame grab of talus blocks possibly representing ejecta from a vulcanian explosion on Oden volcano (see figure 1 for location). (c) Glassy, granular, pyroclastic material. (d) Bubble wall fragment from pyroclastic deposit. Courtesy of Sohn and others (2008).

Sohn and others (2008) note that these observations raise important questions about the accumulation and discharge of magmatic volatiles at ultraslow spreading rates on the Gakkel ridge. They also demonstrate that large-scale pyroclastic activity is possible along even the deepest portions of the global mid-ocean ridge volcanic system.

References. Sohn, R.A., Willis, C., Humphris, S., Shank, T.M., Singh, H., Edmonds, H.N., Kunz, C., Hedman, U., Helmke, E., Jakuba, M., Liljebladh, B., Linder, J., Murphy, C., Nakamura, K., Sato, T., Schlindwein, V., Stranne, C., Tausenfreund, M., Upchurch, L., Winsor, P., Jakobsson., M., and Soule, A., 2008, Explosive volcanism on the ultraslow-spreading Gakkel ridge, Arctic Ocean: Nature, v. 453, p. 1236-1238 (doi:10.1038/nature07075).

Cochran, J.R., 2008, Seamount volcanism along the Gakkel Ridge, Arctic Ocean, Geophysical Journal International, v. 174, no. 3, p. 1153-1173.

Liu,C-Z, Snow, J.E., Hellebrand, E., Brügmann, G., von der Handt, A., Büchl, A., and Hofmann, A.W., 2008, Ancient, highly heterogeneous mantle beneath Gakkel ridge, Arctic Ocean: Nature, v. 452, p. 311-316 (doi:10.1038/nature06688).

Carlowicz, M., 2008, Deeply submerged volcanoes blow their tops: Telltale rocks reveal evidence of a phenomenon scientists thought was impossible: Oceanus, 14 August 2008.

Information Contacts: Oceanus: The Online Magazine of Research from Woods Hole Oceanographic Institution (URL: http://www.whoi.edu/oceanus/).

Two young volcanoes were discovered along the eastern part of the slow-spreading Gakkel Ridge during a bathymetric survey from a submarine in 1999. The westernmost volcano showed evidence of highly reflective, sediment-free surfaces and young faults overprinted by lava flows. During January-September 1999 global seismic networks detected an earthquake swarm corresponding to the approximate location of this volcano. The correlation between the locations of the earthquake epicenter locations and the strongly reflective, untectonized western volcano together with the volcanic character of the seismic record provided evidence that lava erupted on the East Gakkel Ridge within days to months prior to a May 1999 submarine survey (Edwards et al., 2001). Because 12-kHz sonars can penetrate through thin sediments covering acoustically reflective lavas, it is possible that no eruption occurred on Gakkel Ridge in 1999. Historical global seismic records indicate that this was the only earthquake swarm detected on the Gakkel Ridge in about 100 years.

Summary of Holocene eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
[ 1999 Jan (?) ] [ 1999 Sep (?) ] Uncertain 0   East Gakkel Ridge

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

The Global Volcanism Program has no photographs available for Unnamed.

The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title.

Edwards M H, Kurras G J, Tolstoy M, Bohnenstiehl D R, Coakley B J, Cochran J R, 2001. Evidence of recent volcanic activity on the ultraslow-spreading Gakkel Ridge. Nature, 409: 808-812.

Vogt P, 2003. . (pers. comm.).

Volcano Types

Submarine

Tectonic Setting

Rift zone
Oceanic crust (< 15 km)

Rock Types

Major
No Data (checked)

Population

Within 5 km
Within 10 km
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Affiliated Databases

Large Eruptions of Unnamed Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
WOVOdat WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.
EarthChem EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS).
Smithsonian Collections Search the Smithsonian's NMNH Department of Mineral Sciences collections database. Go to the "Search Rocks and Ores" tab and use the Volcano Name drop-down to find samples.