The Global Volcanism Program has no activity reports available for Cordón del Azufre.
The Global Volcanism Program has no Weekly Reports available for Cordón del Azufre.
The Global Volcanism Program has no Bulletin Reports available for Cordón del Azufre.
The Global Volcanism Program has no synonyms or subfeatures listed for Cordón del Azufre.
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The Global Volcanism Program is not aware of any Holocene eruptions from Cordón del Azufre. If this volcano has had large eruptions (VEI >= 4) prior to 12,000 years ago, information might be found on the Cordón del Azufre page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
There is data available for 1 deformation periods. Expand each entry for additional details.
| Start Date: 1998 | Stop Date: 2011 | Direction: Uplift | Method: InSAR |
| Magnitude: Unknown | Spatial Extent: 40.00 km | Latitude: -22.000 | Longitude: -68.000 |
Remarks: Uplift centered at ""Lazufre"" region between Lastarria and Cordon del Azufre volcanoes. Deformation rate accelerated from 2 cm/yr to 3.5 cm/yr from 1998 to 2005, and has been constant from 2005 to 2011. | |||
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Stack of track 282 interferograms showing average LOS uplift at Lazufre between 1995 and 2011. Profiles along the approximate semi-major and semi-minor axis of the surface uplift pattern show the diameter of uplift varies between 50 and 70 km, with no evidence for a moat of subsidence. From: Henderson and Pritchard 2013. |
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Reference List: Pritchard and Simons 2002; Pritchard and Simons 2004a; Froger et al. 2007; Ruch et al. 2009; Henderson and Pritchard 2013.
Full References:
Froger, J. L., D. Remy, S. Bonvalot, and D. Legrand, 2007. Two scales of inflation at Lastarria-Cordon del Azufre volcanic complex, central Andes, revealed from ASAR ENVISAT interferometric data. Earth Planet. Sci. Lett., 255, 148-163. https://doi.org/10.1016/j.epsl.2006.12.012
Henderson, S. T., and M. E. Pritchard, 2013. Decadal volcanic deformation in the central Andes volcanic zone revealed by InSAR time series. Geochemistry Geophysics Geosystems, 14: 1358–1374. https://doi.org/10.1002.ggge.20074
Pritchard, M. E., and M. Simons, 2002. A satellite geodetic survey of large-scale deformation of volcanic centres in the central Andes. Nature, 418, 167-171. https://doi.org/10.1038/nature00872
Pritchard, M. E., and M. Simons, 2004. Surveying volcanic arcs with satellite interferometry: The central Andes, Kamchatka, and beyond. GSA Today, 14(8), 4-9. https://doi.org/10.1130/1052-5173(2004)014<4:SVAWSR>2.0.CO
Ruch J, A Manconi, G Zeni, G Solaro, A Pepe, M Shirzaei, T R Walter, R Lanari, 2009. Stress transfer in the Lazufre volcanic area, central Andes. Geophysical Research Letters, 36, L22303. https://doi.org/10.1029/2009GL041276
There is no Emissions History data available for Cordón del Azufre.
Maps are not currently available due to technical issues.
There are no samples for Cordón del Azufre in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.
| 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. |
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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 Cordón del Azufre. 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 Cordón del Azufre. 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 Cordón del Azufre | 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). |
Cordón del Azufre is in the center of this 22 May 2019 Planet Scope satellite image (N is at the top), located along the Chile-Argentina border. The darker lava flow originated from Volcán la Moyra, the youngest feature of the volcanic field, reaching 6 km to the W. The complex includes a N-S chain of four craters and numerous lava flows.
