- Info & Contacts
The Global Volcanism Program has no activity reports for Baluran.
The Global Volcanism Program has no Weekly Reports available for Baluran.
The Global Volcanism Program has no Bulletin Reports available for Baluran.
The Global Volcanism Program is not aware of any Holocene eruptions from Baluran. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Baluran page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
The Global Volcanism Program has no synonyms or subfeatures listed for Baluran.
|An aerial view from the SW on September 12, 1991 shows an eruption plume from Raung volcano in eastern Java blown by strong winds to the NW. Behind Raung is the massive Ijen caldera, capped by the post-caldera cone of Gunung Merapi (upper right). The light spot below and to the left of Merapi is Kawah Ijen, a renowned crater lake. The flat-topped volcano at the upper left is Gunung Baluran, which occupies the NE-most tip of the island of Java.
Photo by Jeff Post, 1991 (Smithsonian Institution).
|An atmospheric cloud drifts to the east from the summit of the small 1247-m-high andesitic volcano of Baluran, seen here from the SW, along the saddle between it and Ijen volcano. Gunung Baluran, which occupies the very NE tip of Java, contains a broad horseshoe-shaped crater breached to the NE. The volcano lies within a national park and game reserve featuring savannah grasslands and monsoon forests.
Photo by Lee Siebert, 1995 (Smithsonian Institution).
There are no samples for Baluran in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.
|Large Eruptions of Baluran||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.|