Global Volcanism Program

The Global Volcanism Program has no activity reports available for Taisetsuzan.

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

The Global Volcanism Program has no Bulletin Reports available for Taisetsuzan.

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

Daisetu-zan | Nutaku Kamusyupe | Nutaku Kamushupe | Taisetsu-zan | Daisetsu

Cones

Feature Name

Feature Type

Elevation

Latitude

Longitude

Aka-dake

Stratovolcano

2078 m

Asahi-dake

Stratovolcano

2290 m

Eboshi-dake
Ebosi-dake

Stratovolcano

2120 m

Koizumi-dake

Stratovolcano

2160 m

Kuma-dake

Stratovolcano

2210 m

Nagayama-dake

Stratovolcano

Ushiro-Asahi-dake
Usiro-Asahi-dake

Stratovolcano

2213 m

Craters

Feature Name

Feature Type

Elevation

Latitude

Longitude

Ohachidaira

Pleistocene caldera

Sugatamino-ike

Crater

Domes

Feature Name

Feature Type

Elevation

Latitude

Longitude

Hakuun-dake

Dome

2230 m

Hokuchin-dake
Hokutin-dake

Dome

2246 m

Keigetsu-dake
Keigetu-dake

Dome

1945 m

Kuro-dake

Dome

1984 m

Ryoun-dake

Dome

2125 m

Thermal

Feature Name

Feature Type

Elevation

Latitude

Longitude

Sounkyo

Thermal

800 m

Takahara

Thermal

1250 m

Basic Data

Volcano Number

Last Known Eruption

Elevation

Latitude
Longitude

285060

1739 CE

2,291 m / 7,516 ft

43.664°N
142.854°E

Morphology

Volcano Landform
Composite

Volcano Types
Stratovolcano(es)
Caldera
Lava dome(s)

Rock Types

Major
Andesite / Basaltic Andesite
Dacite

Tectonic Setting

Subduction zone
Continental crust (> 25 km)

Population

Within 5 km
Within 10 km
Within 30 km
Within 100 km

19
119
16,391
1,304,267

Geological Summary

The Taisetsuzan volcano group lies at the northern end of the Taisetsu-Tokachi graben in central Hokkaido. It consists of a complex of stratovolcanoes and lava domes associated with a 2-km-wide caldera. The eight satellitic volcanoes are aligned along a ring fracture that is centered over the eastern rim of the caldera. Asahidake, the highest peak of the complex, was constructed 3 km SW of the center of the caldera. Other stratovolcanoes are located along a NE-SW line cutting through the caldera that trends toward the Tokachi volcano complex to the SW. In contrast to the Tokachi group, no historical eruptions are known, although the latest phreatic eruption took place sometime after 1739 CE. Fumarolic areas are located on Asahidake, where at one time sulfur was mined, and in the caldera.

References

The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography.

Japan Association Quaternary Research, 1987. Quaternary Maps of Japan: Landforms, Geology, and Tectonics. Tokyo: Univ Tokyo Press.

Japan Meteorological Agency, 1996. National Catalogue of the Active Volcanoes in Japan (second edition). Tokyo: Japan Meteorological Agency, 502 p (in Japanese).

Japan Meteorological Agency, 2013. National Catalogue of the Active Volcanoes in Japan (fourth edition, English version). Japan Meteorological Agency.

Kudo T, Hoshizumi H, 2006-. Catalog of eruptive events within the last 10,000 years in Japan, database of Japanese active volcanoes. Geol Surv Japan, AIST, https://gbank.gsj.jp/volcano/index_e.htm.

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

Nakano S, Yamamoto T, Iwaya T, Itoh J, Takada A, 2001-. Quaternary Volcanoes of Japan. Geol Surv Japan, AIST, http://www.aist.go.jp/RIODB/strata/VOL_JP/.

Newhall C G, Dzurisin D, 1988. Historical unrest at large calderas of the world. U S Geol Surv Bull, 1855: 1108 p, 2 vol.

Eruptive History

There is data available for 5 confirmed Holocene eruptive periods.

1739 (after) Confirmed Eruption

Episode 1 | Eruption

Asahi-dake

1739 (after) - Unknown

Evidence from Correlation: Tephrochronology

List of 4 Events for Episode 1 at Asahi-dake

Start Date	End Date	Event Type
- - - -	- - - -	Phreatic activity
- - - -	- - - -	Ash
1958 Jul 21	- - - -	Fatalities
1961 Jun 18	- - - -	Fatalities

0550 BCE ± 500 years Confirmed Eruption

Episode 1 | Eruption

Asahi-dake, Ash-b tephra

0550 BCE ± 500 years - Unknown

Evidence from Correlation: Tephrochronology

List of 3 Events for Episode 1 at Asahi-dake, Ash-b tephra

Start Date	End Date	Event Type
- - - -	- - - -	Phreatic activity
- - - -	- - - -	Avalanche
- - - -	- - - -	Ash

1450 BCE ± 50 years Confirmed Eruption

Episode 1 | Eruption

Asahi-dake, As-B tephra

1450 BCE ± 50 years - Unknown

Evidence from Isotopic: 14C (calibrated)

List of 2 Events for Episode 1 at Asahi-dake, As-B tephra

	Start Date	End Date	Event Type	Event Remarks
	- - - -	- - - -	Phreatic activity
	- - - -	- - - -	Ash

2800 BCE ± 100 years Confirmed Eruption

Episode 1 | Eruption

Asahi-dake, As-A tephra

2800 BCE ± 100 years - Unknown

Evidence from Isotopic: 14C (calibrated)

List of 2 Events for Episode 1 at Asahi-dake, As-A tephra

	Start Date	End Date	Event Type	Event Remarks
	- - - -	- - - -	Phreatic activity
	- - - -	- - - -	Ash

3200 BCE ± 75 years Confirmed Eruption

Episode 1 | Eruption

Asahi-dake, Asahi Scoria deposit

3200 BCE ± 75 years - Unknown

Evidence from Isotopic: 14C (calibrated)

List of 2 Events for Episode 1 at Asahi-dake, Asahi Scoria deposit

	Start Date	End Date	Event Type	Event Remarks
	- - - -	- - - -	Explosion
	- - - -	- - - -	Ash

Deformation History

There is no Deformation History data available for Taisetsuzan.

Emission History

There is no Emissions History data available for Taisetsuzan.

Photo Gallery

Geothermal activity and recent craters occupy the western slope of Asahidake, one of the Daisetsu group volcanoes in central Hokkaido. Taisetsuzan is a complex group of cones and lava domes associated with a 2-km-wide caldera. Asahidake, the highest peak of the complex, was constructed 3 km SW from the caldera center.

Photo by Ichio Moriya, 1993 (Kanazawa University).

GVP Map Holdings

Maps are not currently available due to technical issues.

Smithsonian Sample Collections Database

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

External Sites

Copernicus Browser

The Copernicus Browser replaced the Sentinel Hub Playground browser in 2023, to provide access to Earth observation archives from the Copernicus Data Space Ecosystem, the main distribution platform for data from the EU Copernicus missions.

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.

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.

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 Taisetsuzan. 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 Taisetsuzan. 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 Taisetsuzan

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).