- Info & Contacts
The Global Volcanism Program has no activity reports for Nishihitokappuyama [Bogatyr Ridge].
The Global Volcanism Program has no Weekly Reports available for Nishihitokappuyama [Bogatyr Ridge].
The Global Volcanism Program has no Bulletin Reports available for Nishihitokappuyama [Bogatyr Ridge].
The Global Volcanism Program is not aware of any Holocene eruptions from Nishihitokappuyama [Bogatyr Ridge]. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Nishihitokappuyama [Bogatyr Ridge] 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.
|Hitokappu Volcano Group|
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Stratovolcano||1634 m||44° 50' 0" N||147° 22' 0" E|
|The Bogatyr Ridge, seen here looking southward across Iturup Island, consists of a cluster of small NE-SW-trending late-Pleistocene to Holocene cones and craters. The larger Stokap stratovolcano (upper left) occupies the SW end of the ridge. Stokap volcano is capped by a complex of 8-10 cones and explosion craters, the largest of which contains a lake. The volcanic chain was constructed over a high Pleistocene base of glaciated Pleistocene volcanic rocks. No historical eruptions are known from the volcanic chain.
Photo by A. Tsvetkov, 1968.
|Snow-capped Stokap volcano (center) lies at the SW end of Bogatyr Ridge, an elongated chain of small volcanoes on southern Iturup Island. Bogatyr Ridge (left of Stokap) consists of a cluster of small NE-SW-trending late-Pleistocene to Holocene cones and craters. Stokap volcano is capped by a complex of 8-10 cones and explosion craters, the largest of which contains a lake. The slopes of conical Atsonupuri volcano form the ridge in the right foreground.
Photo by Alexander Rybin, 2001 (Institute of Marine Geology and Geophysics, Yuzhno-Sakhalin).
There are no samples for Nishihitokappuyama [Bogatyr Ridge] in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.
|Large Eruptions of Nishihitokappuyama [Bogatyr Ridge]||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.|