Esmeralda Bank

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  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 15°N
  • 145.25°E

  • -43 m
    -141 ft

  • 284210
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

The Global Volcanism Program has no activity reports for Esmeralda Bank.

The Global Volcanism Program has no Weekly Reports available for Esmeralda Bank.

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.

05/1975 (CSLP 38-75) Bubbling and boiling at the ocean surface, water discoloration

06/1982 (SEAN 07:06) Submarine sulfur emission

08/1987 (SEAN 12:08) Bubbling and discolored water


Contents of Monthly Reports

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

All times are local (= UTC + 10 hours)

05/1975 (CSLP 38-75) Bubbling and boiling at the ocean surface, water discoloration

Card 2185 (15 May 1975) Bubbling and boiling at the ocean surface, water discoloration

One of only two known submerged volcanoes in the Mariana Islands is erupting west of Tinian. Unnamed and virtually unstudied, this volcano -- estimated to be 30-40 km W of Tinian's southern tip -- was first spotted on 26 April by crew members of Continental Air Micronesia who reported that its underwater explosions were causing a bubbling action on the water's surface. Steam vapor was also noted. The activity in the area has been irregular since then and several new eruptions were seen on 29 April.

The surface of the water is marked by a series of boiling spots running north to south, with the southernmost fanning out in an open oval toward the SW for a distance estimated by pilots at about 3 km. Within this fan, the color of the water varies from light brown to greenish yellow.

According to Dr. Eldredge, this submerged volcano has not yet been studied in great detail as far as he can determine. He believes that the last eruption took place 4-5 years ago. Dr. Eldredge is especially interested in any possible fish kills in the area. Other studies of such volcanoes have reported large amounts of dead fish floating on the surface of the water.

This volcano is listed in the Catalogue of Active Volcanoes of the World as "Submarine Volcano Southwest of Saipan." It is a stratovolcano ... and its summit is 60 m below sea level. The height of the volcano above the ocean floor is about 1,000 m.

Information Contact: L.G. Eldredge, Marine Laboratory, University of Guam.

06/1982 (SEAN 07:06) Submarine sulfur emission

In April, "sulfur boil" activity was observed at the submarine volcano Esmeralda Bank from the U.S. National Marine Fisheries Service research vessel Townsend Cromwell. The sulfur emission can be seen as an area of strong mixing above the Bank on a 6 April bottom profile. The research vessel's log notes three sources of sulfur emission on 21 April, the strongest near a shoal at 50 m depth, a second S of a ridge just S of the main shoal, and the third in the saddle between these two shallow areas. The next day, the main source remained strongly active and emission continued from the saddle vent, but by 24 April sulfur emission was only barely visible.

Further Reference. Gorshkov, A.P., Gavrilenko, G.M., Seliverstov, N.I., and Scripko, K.A., 1982, Geologic Structure and fumarolic activity of the Esmeralda submarine volcano, in Schmincke, H.-U., Baker, P.E., and Forjaz, V.H. (eds.), Proceedings of the International Symposium on the Activity of Oceanic Volcanoes: Arquipélago, Serie Ciéncias da Natureza (Univ. Azores) no. 3, p. 271-298.

Information Contact: L. Eldredge, Univ. of Guam.

08/1987 (SEAN 12:08) Bubbling and discolored water

On 26 May, the pilot of a charter aircraft observed a heavy "boil" on the ocean surface over Esmeralda, feeding an elongate zone of discolored water. The pilot reported that he had not seen activity at Esmeralda in many years. On 4 June, L.G. Eldredge and the same pilot flew over Esmeralda, but saw no water movement or discoloration.

Information Contacts: L. Eldredge, University of Guam.

Esmeralda Bank is a massive submarine volcano with three summit cones oriented along a N-S line. Their summits are from 43 to 140 m beneath the sea surface. The highest, middle peak contains a 3-km-wide caldera open to the west and several parasitic cones. Frequent sulfur boils and water discoloration have been observed, which have variously been attributed to eruptive events or solfataric activity.

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

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
[ 1987 May 26 ] [ Unknown ] Uncertain 0  
[ 1982 Apr 6 ] [ Unknown ] Uncertain 0  
[ 1975 Apr 26 ] [ 1975 Apr 29 ] Uncertain 0  
[ 1970 ± 1 years ] [ Unknown ] Uncertain 0  
[ 1964 Apr 14 ] [ Unknown ] Uncertain 2  
[ 1944 Aug 20 ± 10 days ] [ Unknown ] Uncertain 0  

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

A bathymetric map with two time vertical exaggeration shows Esmeralda Bank submarine volcano, as seen from the NW. Depths in this image range from 54 to 2052 meters. Bathymetry data (~25 meter resolution) is overlaid on SeaBat data (~50 meter resolution) courtesy of Yoshihiko Tamura, JAMSTEC. Esmeraldo Bank is a massive submarine volcano with three summit cones, the middle of which is cut by a 3-km-wide caldera. Frequent sulfur boils and water discoloration from eruptive or solfataric activity have been observed.

Image courtesy of Susan Merle (Oregon State University/NOAA Vents Program).

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.

Bloomer S H, Stern R J, Smoot N C, 1989. Physical volcanology of the submarine Mariana and Volcano arcs. Bull Volc, 51: 210-224.

Corwin G, 1971. Quaternary volcanics of the Mariana Islands. Unpublished manuscript, 137 p.

Dixon T H, Stern R J, 1983. Petrology, chemistry, and isotopic composition of submarine volcanoes in the southern Mariana arc. Geol Soc Amer Bull, 94: 1159-1172.

Gorshkov A P, Gavrilenko G M, Seliverstov N I, Scripko K A, 1982. Geologic structure and fumarolic activity of the Esmeralda submarine volcano. In: Schmincke H-U, Baker P E, Forjaz V H (eds) {Proc Symp Activity Oceanic Volcanoes}, Arquipelago, Revista Univ Dos Acores, 3: 271-298.

IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..

Kuno H, 1962. Japan, Taiwan and Marianas. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 11: 1-332.

Stern R J, Bibee L D, 1984. Esmeralda Bank: geochemistry of an active submarine volcano in the Mariana Island Arc. Contr Mineral Petr, 86: 159-169.

Volcano Types

Submarine
Caldera

Tectonic Setting

Subduction zone
Crustal thickness unknown

Rock Types

Major
Basalt / Picro-Basalt
Andesite / Basaltic Andesite

Population

Within 5 km
Within 10 km
Within 30 km
Within 100 km
0
0
0
84,578

Affiliated Databases

Large Eruptions of Esmeralda Bank 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.