Global Volcanism Program

The Global Volcanism Program has no activity reports for Kostakan.

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

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

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.

Cones

Feature Name

Feature Type

Elevation

Latitude

Longitude

Domashnii

Pyroclastic cone

842 m

Glavny

Pyroclastic cone

847 m

53° 49' 59" N

158° 3' 6" E

Krasny

Pyroclastic cone

990 m

Ochkovyi

Pyroclastic cone

850 m

Serpovidny

Pyroclastic cone

830 m

Craters

Feature Name

Feature Type

Elevation

Latitude

Longitude

Zmeya

Crater

1150 m

Basic Data

Volcano Number

Last Known Eruption

Elevation

Latitude
Longitude

300122

1350 CE

1150 m / 3773 ft

53.833°N
158.052°E

Volcano Types

Pyroclastic cone(s)
Maar

Rock Types

Major
Basalt / Picro-Basalt
Andesite / Basaltic Andesite

Tectonic Setting

Subduction zone
Continental crust (> 25 km)

Population

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

13
13
1,352
232,577

Geological Summary

A group of basaltic cinder cones lies south of Bakening volcano, west of the Srednaya Avacha (Middle Avacha) river valley. They are part of a broad zone of regional late Pleistocene to Holocene basaltic volcanism west of the Eastern volcanic zone of Kamchatka that extends from the Kostakan Lake area to the south. Several of the cinder cones are breached by lava flows, some of which extend into the Srednaya Avacha valley. The highest-elevation vent, Zmeya crater, was constructed within a landslide scarp. An unnamed maar is located about 2 km S of Kostakan Lake. Eruptions have occurred during two time periods, between about 11,000 to 7,000 years ago and between about 1,200 and 600 years ago.

References

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

Braitseva O, Ponomareva V, Melekestsev I, Sulerzhitsky L, Pevzner M, 2002-. Holocene Kamchatka volcanoes. http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm.

Dirksen O V, Melekestsev I V, 1999. Chronology, evolution and morphology of Plateau Basalt eruptive centers in Avacha River area, Kamchatka, Russia. Volc Seism, 21: 1-28 (English translation).

Dorendorf F, Churikova T, Koloskov A, Worner G, 2000. Late Pleistocene to Holocene activity at Bakening volcano and surrounding monogenetic centers (Kamchatka): volcanic geology and geochemical evolution. J. Volcanol. Geotherm. Res., 104: 131-151.

Erlich E N, 1985. (pers. comm.).

Eruptive History

There is data available for 6 confirmed Holocene eruptive periods.

1350 (?) Confirmed Eruption Max VEI: 1 (?)

Episode 1 | Eruption Episode

Glavny

1350 (?) - Unknown

Evidence from Correlation: Tephrochronology

List of 3 Events for Episode 1 at Glavny

Start Date	End Date	Event Type
- - - -	- - - -	Explosion
- - - -	- - - -	Ash
1350 (?)	- - - -	VEI (Explosivity Index)

1200 ± 50 years Confirmed Eruption Max VEI: 2

Episode 1 | Eruption Episode

Glavny

1200 ± 50 years - Unknown

Evidence from Correlation: Tephrochronology

List of 7 Events for Episode 1 at Glavny

Start Date	End Date	Event Type
- - - -	- - - -	Explosion
- - - -	- - - -	Lava flow
- - - -	- - - -	Cinder Cone
- - - -	- - - -	Ash
- - - -	- - - -	Lapilli
- - - -	- - - -	Scoria
1200 ± 50 years	- - - -	VEI (Explosivity Index)

1000 ± 50 years Confirmed Eruption Max VEI: 3

Episode 1 | Eruption Episode

Serpovidny

1000 ± 50 years - Unknown

Evidence from Correlation: Tephrochronology

List of 6 Events for Episode 1 at Serpovidny

Start Date	End Date	Event Type
- - - -	- - - -	Explosion
- - - -	- - - -	Lava flow
- - - -	- - - -	Cinder Cone
- - - -	- - - -	Ash
- - - -	- - - -	Bombs
1000 ± 50 years	- - - -	VEI (Explosivity Index)

0800 ± 50 years Confirmed Eruption Max VEI: 3

Episode 1 | Eruption Episode

Maar S of Lake Kostakan, Krasny cone

0800 ± 50 years - Unknown

Evidence from Correlation: Tephrochronology

List of 7 Events for Episode 1 at Maar S of Lake Kostakan, Krasny cone

Start Date	End Date	Event Type
- - - -	- - - -	Explosion
- - - -	- - - -	Lava flow
- - - -	- - - -	Cinder Cone
- - - -	- - - -	Ash
- - - -	- - - -	Lapilli
- - - -	- - - -	Bombs
0800 ± 50 years	- - - -	VEI (Explosivity Index)

6550 BCE ± 500 years Confirmed Eruption Max VEI: 3

Episode 1 | Eruption Episode

Ochkovy

6550 BCE ± 500 years - Unknown

Evidence from Correlation: Tephrochronology

List of 7 Events for Episode 1 at Ochkovy

Start Date	End Date	Event Type
- - - -	- - - -	Explosion
- - - -	- - - -	Lava flow
- - - -	- - - -	Cinder Cone
- - - -	- - - -	Ash
- - - -	- - - -	Bombs
- - - -	- - - -	Scoria
6550 BCE ± 500 years	- - - -	VEI (Explosivity Index)

8050 BCE ± 1000 years Confirmed Eruption Max VEI: 3

Episode 1 | Eruption Episode

Domashnii

8050 BCE ± 1000 years - Unknown

Evidence from Correlation: Tephrochronology

List of 6 Events for Episode 1 at Domashnii

Start Date	End Date	Event Type
- - - -	- - - -	Explosion
- - - -	- - - -	Cinder Cone
- - - -	- - - -	Ash
- - - -	- - - -	Blocks
- - - -	- - - -	Scoria
8050 BCE ± 1000 years	- - - -	VEI (Explosivity Index)

Deformation History

There is no Deformation History data available for Kostakan.

Emission History

There is no Emissions History data available for Kostakan.

Photo Gallery

GVP Map Holdings

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.

Smithsonian Sample Collections Database

There are no samples for Kostakan 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 Kostakan. 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 Kostakan. 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 Kostakan

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).