Discolored water around the Kaitoku Seamount was visible in a 26 January Sentinel 2 satellite image. The plume was diffuse and dispersed a few kilometers E. No discolored water was visible in a 31 January image.
Source: Sentinel Hub
No water discoloration seen in 1990
No discolorations were observed at . . . Kaitoku . . . during 1990.
Information Contacts: Hydrographic Department, JMSA.
2023: January
2022: August
| December
Discolored water around the Kaitoku Seamount was visible in a 26 January Sentinel 2 satellite image. The plume was diffuse and dispersed a few kilometers E. No discolored water was visible in a 31 January image.
Source: Sentinel Hub
Discolored water around the Kaitoku Seamount was visible in 1 and 6 January Sentinel satellite images. Concentric circles of discolored water radiated out from the vent area and a plume drifted W. The plume of discolored water extended S in the 6 January image.
Source: Sentinel Hub
After JMA first reported new activity around the Kaitoku Seamount in August, discolored water continued to be periodically visible in Sentinel satellite images through 27 December. Though weather clouds sometimes prevented views of the vent area, and on occasion no activity was visible in clear images, plumes of discolored water drifting away from the vent area appeared to become more frequent in October. Images from 18 October, and 22 and 27 November possibly captured material at the surface or an eruption plume rising above the water. The Japan Coast Guard posted pictures of disturbed water around the vent in November. Recent Sentinel images on 17 and 27 December captured plumes of discolored water drifting as far as 10 km from the vent area.
Sources: Sentinel Hub; Japan Coast Guard
JMA reported that discolored water around the Kaitoku Seamount was visible during 18-19 August.
Sources: Japan Meteorological Agency (JMA); Japan Coast Guard
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.
Large area of discolored water; small plumes
On 7 March at 1230, the crew of a Japan Maritime Self-Defense Force (JMSDF) transport plane flying about 130 km N of Iwo-Jima observed a fan-shaped zone of discolored sea water that extended about [28] km WSW from a submarine vent. The maximum width of the discolored zone was about 9 km. A helicopter flew over the area shortly thereafter and its crew estimated that the extent of the reddish-brown water was roughly as large as Iwo Jima Island (about 5 x 8 km).
The next morning, JMSA personnel observed continuous submarine eruptive activity. Gray or yellowish brown water was ejected every 10 minutes and waves spread outward from the vents. The sea colors included gray, white, yellowish brown, and reddish brown. JMSA observers saw neither plumes nor floating ejecta, although small white plumes and rocks or reefs were seen during a flight by the JMSDF at about noon the same day. On 12 March, personnel aboard a JMSDF patrol plane again saw floating material, and a plume about 100 m above sea level. Only discoloration was found during a JMSA flight 13 March. As of the 13th, no new island had been observed at the eruption site.
The activity was located near the site of an eruption reported in 1543 at 26.00°N, 140.77°E.
Information Contacts: JMA.
Acoustic waves recorded in French Polynesia
RSP stations on Rangiroa, Tubuai, and Rikitéa recorded acoustic waves (T-phase) from a strong submarine volcanic eruption in the vicinity of the Izu Islands. Between 25 March and 30 April, more than 500 signals were received, 300 between 2 and 9 April. Most of the events were impulsive and of short duration, indicating explosive volcanic activity at a shallow depth. Some of the events were emergent and of longer duration indicating quiet emission of lava. J.M. Talandier noted that these events appear to be correlated with the submarine activity reported in 9:2.
Information Contacts: J. Talandier, Lab. de Géophysique, Tahiti.
Discolored water; floating lapilli; formal name
JMSA observations beginning 7 March indicated that eruptive activity was at its highest level in mid to late March, when floating ejecta and vapor plumes were nearly always seen. Beginning in April, activity subsided gradually. The area of discolored water decreased from 13 x 30 km in early March to 300 m in diameter in early May (table 1).
On either side of the submarine vent are two shallow areas, at 26.13°N, 141.10°E, and 26.05°N, 140.93°E (figure 1). JMSA has formally named the feature Kaitoku Kaizan (Kaitoku Seamount).
Information Contacts: JMA, Tokyo.
Discolored water after 3 months of quiet
JMSA reconnaissance revealed few signs of activity since the March eruption. Pumice was observed only around the eruption site; none washed up on shore.
Activity gradually declined. To the crew that overflew the area at noon on 9 April, the water discoloration was barely distinguishable, and no ejecta or plume was seen (table 1). JMSA and JMSDF saw no discolored water or other activity on 10 and 31 July, 1 August, and 6 and 26 September. However, the crew of the MV Emblem reported a 3.5-5-km area of upwelling and water discoloration on 15 October.
Table 1. JMSA observations at Kaitoku Seamount, March-June 1984. Courtesy of JMA.
Date | Observation |
07 Mar 1984 | 9 x [28] km of discolored water |
08 Mar 1984 | Floating lapilli; 0.5-3 x 50 km of discolored water |
09 Mar 1984 | Seawater temperature at vent 0.5°C higher than floating lapilli; 9-13 x 30 km of discolored water |
12 Mar 1984 | Floating lapilli; discolored water |
13 Mar 1984 | Seawater near vent 0.5-1°C higher; floating lapilli; vapor plume |
15 Mar 1984 | Floating lapilli |
16-19 Mar 1984 | Floating lapilli; vapor plume |
22 Mar 1984 | Dark plume; luminescence at night |
23 Mar 1984 | Vapor plume; luminescence at night |
24-25 Mar 1984 | Vapor plume |
26 Mar 1984 | Floating lapilli |
09 Apr 1984 | 0.3 x 5 km of very weak water discoloration |
09-10 May 1984 | Area of discolored water 0.3 km in diameter |
15 May 1984 | White upwelling and discoloration, 3.5 km in diameter |
18 May 1984 | Milky white discoloration, 0.18 km wide |
09 Jun 1984 | Weak green discoloration, 0.15 x 0.05 km |
Further Reference. Tsuchide, M., Kato, S., Uchida, A., Sato, H., Konishi, N., Osaka, J., and Hirabayashi, J., 1985, Submarine volcanic activity at the Kaitoku seamount in 1984: Rep. Hydrograph. Res., v. 20, p. 47-82.
Information Contacts: JMA, Tokyo.
No water discoloration seen in 1990
No discolorations were observed at . . . Kaitoku . . . during 1990.
Information Contacts: Hydrographic Department, JMSA.
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
Synonyms |
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Kaitoku Kaizan | Kaitoku-okanoba | ||||
Cones |
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Feature Name | Feature Type | Elevation | Latitude | Longitude |
Higashi-Kaitokuba | Cone | |||
Nishi-Kaitokuba | Cone |
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There is data available for 3 confirmed Holocene eruptive periods.
2022 Aug 18 - 2023 Jan 26 Confirmed Eruption
Episode 1 | Uncertain Episode | |||||||||||||||
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2022 Aug 18 - 2023 Jan 26 | Evidence from Observations: Reported | ||||||||||||||
Discolored water around the Kaitoku Seamount was visible during 18-19 August 2022. | |||||||||||||||
List of 1 Events for Episode 1
|
[ 1986 Jun 18 - 1986 Jun 18 ] Uncertain Eruption
[ 1984 Dec 23 - 1984 Dec 23 ] Uncertain Eruption
1984 Mar 8 - 1984 Mar 26 (?) Confirmed Eruption Max VEI: 0
Episode 1 | Eruption Episode | Higashi-Kaitokuba | |||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1984 Mar 8 - 1984 Mar 26 (?) | Evidence from Observations: Reported | |||||||||||||||||||
List of 2 Events for Episode 1 at Higashi-Kaitokuba
|
1543 Confirmed Eruption Max VEI: 0
Episode 1 | Eruption Episode | West flank of Nishi-Kaitokuba | ||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1543 - Unknown | Evidence from Observations: Reported | ||||||||||||||
List of 1 Events for Episode 1 at West flank of Nishi-Kaitokuba
|
There is no Deformation History data available for Kaitoku Seamount.
There is no Emissions History data available for Kaitoku Seamount.
The Global Volcanism Program has no photographs available for Kaitoku Seamount.
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. The maps database originated over 30 years ago, but was only recently updated and connected to our main database. We welcome users to tell us if they see incorrect information or other problems with the maps; please use the Contact GVP link at the bottom of the page to send us email.
There are no samples for Kaitoku Seamount in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.
WOVOdat
Single Volcano View Temporal Evolution of Unrest Side by Side Volcanoes |
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.
GVMID Data on Volcano Monitoring Infrastructure The Global Volcano Monitoring Infrastructure Database GVMID, is aimed at documenting and improving capabilities of volcano monitoring from the ground and space. GVMID should provide a snapshot and baseline view of the techniques and instrumentation that are in place at various volcanoes, which can be use by volcano observatories as reference to setup new monitoring system or improving networks at a specific volcano. These data will allow identification of what monitoring gaps exist, which can be then targeted by remote sensing infrastructure and future instrument deployments. |
Volcanic Hazard Maps | The IAVCEI Commission on Volcanic Hazards and Risk has a Volcanic Hazard Maps database designed to serve as a resource for hazard mappers (or other interested parties) to explore how common issues in hazard map development have been addressed at different volcanoes, in different countries, for different hazards, and for different intended audiences. In addition to the comprehensive, searchable Volcanic Hazard Maps Database, this website contains information about diversity of volcanic hazard maps, illustrated using examples from the database. This site is for educational purposes related to volcanic hazard maps. Hazard maps found on this website should not be used for emergency purposes. For the most recent, official hazard map for a particular volcano, please seek out the proper institutional authorities on the matter. |
MIROVA | Middle InfraRed Observation of Volcanic Activity (MIROVA) is a near real time volcanic hot-spot detection system based on the analysis of MODIS (Moderate Resolution Imaging Spectroradiometer) data. In particular, MIROVA uses the Middle InfraRed Radiation (MIR), measured over target volcanoes, in order to detect, locate and measure the heat radiation sourced from volcanic activity. |
MODVOLC Thermal Alerts | Using infrared satellite Moderate Resolution Imaging Spectroradiometer (MODIS) data, scientists at the Hawai'i Institute of Geophysics and Planetology, University of Hawai'i, developed an automated system called MODVOLC to map thermal hot-spots in near real time. For each MODIS image, the algorithm automatically scans each 1 km pixel within it to check for high-temperature hot-spots. When one is found the date, time, location, and intensity are recorded. MODIS looks at every square km of the Earth every 48 hours, once during the day and once during the night, and the presence of two MODIS sensors in space allows at least four hot-spot observations every two days. Each day updated global maps are compiled to display the locations of all hot spots detected in the previous 24 hours. There is a drop-down list with volcano names which allow users to 'zoom-in' and examine the distribution of hot-spots at a variety of spatial scales. |
Sentinel Hub Playground
Sentinel Hub EO Browser |
The Sentinel Hub Playground provides a quick look at any Sentinel-2 image in any combination of the bands and enhanced with image effects; Landsat 8, DEM and MODIS are also available. Sentinel Hub is an engine for processing of petabytes of satellite data. It is opening the doors for machine learning and helping hundreds of application developers worldwide. It makes Sentinel, Landsat, and other Earth observation imagery easily accessible for browsing, visualization and analysis. Sentinel Hub is operated by Sinergise |
IRIS seismic stations/networks | Incorporated Research Institutions for Seismology (IRIS) Data Services map showing the location of seismic stations from all available networks (permanent or temporary) within a radius of 0.18° (about 20 km at mid-latitudes) from the given location of Kaitoku Seamount. Users can customize a variety of filters and options in the left panel. Note that if there are no stations are known the map will default to show the entire world with a "No data matched request" error notice. |
UNAVCO GPS/GNSS stations | Geodetic Data Services map from UNAVCO showing the location of GPS/GNSS stations from all available networks (permanent or temporary) within a radius of 20 km from the given location of Kaitoku Seamount. Users can customize the data search based on station or network names, location, and time window. Requires Adobe Flash Player. |
DECADE Data | The DECADE portal, still in the developmental stage, serves as an example of the proposed interoperability between The Smithsonian Institution's Global Volcanism Program, the Mapping Gas Emissions (MaGa) Database, and the EarthChem Geochemical Portal. The Deep Earth Carbon Degassing (DECADE) initiative seeks to use new and established technologies to determine accurate global fluxes of volcanic CO2 to the atmosphere, but installing CO2 monitoring networks on 20 of the world's 150 most actively degassing volcanoes. The group uses related laboratory-based studies (direct gas sampling and analysis, melt inclusions) to provide new data for direct degassing of deep earth carbon to the atmosphere. |
Large Eruptions of Kaitoku Seamount | 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). |
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). |