- Info & Contacts
The Global Volcanism Program has no activity reports for Gorny Institute.
The Global Volcanism Program has no Weekly Reports available for Gorny Institute.
The Global Volcanism Program has no Bulletin Reports available for Gorny Institute.
Summary of Holocene eruption dates and Volcanic Explosivity Indices (VEI).
|Start Date||Stop Date||Eruption Certainty||VEI||Evidence||Activity Area or Unit|
|1250 (?)||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1000 (?)||Unknown||Confirmed||Radiocarbon (uncorrected)|
|4250 BCE (?)||Unknown||Confirmed||0||Radiocarbon (uncorrected)||South flank (Sedanka lava flow)|
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.
|Gornogo Instituta | Gornyi Institute|
|Gorny Institute volcano, seen here from the south, lies at the NE end of chain of small late-Quaternary volcanoes extending NE from Kebeney volcano in the central Sredinny Range. Gorny Institute is one of the few large stratovolcanoes in the Sredinny Range that has been active throughout the Holocene. More than 20 pyroclastic horizons have been documented, and the last major eruption took place about 700 years ago.
Copyrighted photo by Maria Pevzner, 2004 (Russian Academy of Sciences, Moscow).
|An aerial photo shows the Sedankinsky lava flow, with the source and the terminal part of the flow marked with red stars. The vent lies at about 1600 m elevation on the south flank of Gorny Institute volcano. Based on tephrochronological dating, the eruption took place ~ 6200 years ago. The flow descended the Sedanka River valley.
Photo from Holocene Kamchataka volcanoes (http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
A listing of samples from the Smithsonian collections will be available soon.
|Large Eruptions of Gorny Institute||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.|