Bely

No photo available for this volcano
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  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 57.88°N
  • 160.53°E

  • 2080 m
    6822 ft

  • 300640
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

The Global Volcanism Program has no activity reports for Bely.

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

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

Basic Data

Volcano Number

Last Known Eruption

Elevation

Latitude
Longitude
300640

Unknown - Evidence Uncertain

2080 m / 6822 ft

57.88°N
160.53°E

Volcano Types

Shield(s)
Stratovolcano

Rock Types

Major
Basalt / Picro-Basalt

Tectonic Setting

Subduction zone
Continental crust (> 25 km)

Population

Within 5 km
Within 10 km
Within 30 km
Within 100 km
0
0
20
1,320

Geological Summary

The late-Quaternary Icelandic-type basaltic Bely shield volcano in the northern Sredinny Range is topped by a small stratovolcano. The smaller shields Sergeeva and Keveneytunup are located to the south and east, respectively, and the late-Pleistocene Lagerny shield lies to the SE. Keveneytunup at 2133 m is the highest of these volcanoes, slightly exceeding the 2080-m-high Bely volcano. Early geologic studies in the Sredinny Range (Ogorodov et al. 1972) identified numerous Holocene eruptive centers based primarily on morphological criteria. However, later work has suggested that Sredinny Range volcanoes are less mantled by Holocene tephras than eastern Kamchatka volcanoes and therefore appear more youthful, so that Holocene eruptions are uncertain for many of these Sredinny Range eruptive vents.

References

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

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

Erlich E N, Gorshkov G S (eds), 1979. Quaternary volcanism and tectonics in Kamchatka. Bull Volc, 42:1-4.

Ogorodov N V, Kozhemyaka N N, Vazheevskaya A A, Ogorodov A S, 1972. Volcanoes and the Quaternary Volcanism of the Sredinny Ridge in Kamchatka. Moscow: Nauka Pub, 190 p (in Russian).

Ponomareva V V, 2001. (pers. comm.).

The Global Volcanism Program is not aware of any Holocene eruptions from Bely. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Bely page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

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

Belyi

Cones

Feature Name Feature Type Elevation Latitude Longitude
Keveneytunup Shield volcano 2133 m 57° 53' 0" N 160° 36' 0" E
Lagerny Shield volcano 1842 m 57° 51' 0" N 160° 37' 0" E
Sergeeva Shield volcano 1742 m 57° 49' 0" N 160° 30' 0" E

The Global Volcanism Program has no photographs available for Bely.

Smithsonian Sample Collections Database


A listing of samples from the Smithsonian collections will be available soon.

Affiliated Sites

Large Eruptions of Bely 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).
MODVOLC - HIGP MODIS Thermal Alert System 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.
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.