No visible fumarolic activity; strong sulfur odor near sumit craters
Geologists visited the summit 16, 17, and 18 February. There was no visible fumarolic activity around the summit, or in the explosion craters from the volcano's last eruption in 1972. The geologists smelled a strong sulfur odor in the immediate vicinity of the summit craters.
Information Contacts: T. Bornhorst and C. Chesner, Michigan Tech. Univ.
The Global Volcanism Program has no Weekly Reports available for Acatenango.
Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Click on the index link or scroll down to read the reports.
Eruption from three central vents in mid-November; first activity since 1927
Card 1513 (19 December 1972) Eruption from three central vents in mid-November; first activity since 1927
R. Stoiber reported the following on 18 December 1972. "The volcano Acatenango started erupting on approximately 13 November 1972 for the first time since 19 May 1927. Ascents by Dartmouth teams have documented a deepened crater and five active vents located in the saddle between the two peaks of Acatenago. These vents are situated on the N-S line along the axis of the peaks of Acatenango and the adjacent volcano Fuego. On 5 December 1972 the three central vents were ejecting, steam, ash, and gases included H2S and SO2. Five to 10 cm of ash covers the summit area. No ash had fallen outside this zone. New white sublimates, possibly gypsum, were noted. A prior ascent on 30 October 1972 had revealed only weak fumarolic activity. Observations continue."
Information Contacts: Samuel Bonis, Instituto Geografico Nacional, Guatemala; Richard Stoiber, Dartmouth College, USA
No visible fumarolic activity; strong sulfur odor near sumit craters
Geologists visited the summit 16, 17, and 18 February. There was no visible fumarolic activity around the summit, or in the explosion craters from the volcano's last eruption in 1972. The geologists smelled a strong sulfur odor in the immediate vicinity of the summit craters.
Information Contacts: T. Bornhorst and C. Chesner, Michigan Tech. Univ.
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 |
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Mayor, Pico | Central, Pico | ||||
Cones |
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Feature Name | Feature Type | Elevation | Latitude | Longitude |
Yepocapa
Chico, Pico Tres Hermanas Tres Marías |
Stratovolcano | 3820 m | 14° 30' 29" N | 90° 52' 23" W |
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There is data available for 8 confirmed Holocene eruptive periods.
1972 Nov 12 - 1972 Dec 16 ± 15 days Confirmed Eruption VEI: 1
Episode 1 | Eruption | Pico Central-Yepocapa saddle | |||||||||||||||||||||||||||||
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1972 Nov 12 - 1972 Dec 16 ± 15 days | Evidence from Observations: Reported | |||||||||||||||||||||||||||||
List of 4 Events for Episode 1 at Pico Central-Yepocapa saddle
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1926 Aug - 1927 May 19 Confirmed Eruption VEI: 2
Episode 1 | Eruption | Pico Central | ||||||||||||||||||||||||||||||||||
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1926 Aug - 1927 May 19 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||
List of 5 Events for Episode 1 at Pico Central
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1924 Dec 18 - 1925 Jun 7 Confirmed Eruption VEI: 3
Episode 1 | Eruption | North slope of Pico Central | |||||||||||||||||||||||||||||||||||||||
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1924 Dec 18 - 1925 Jun 7 | Evidence from Observations: Reported | |||||||||||||||||||||||||||||||||||||||
List of 6 Events for Episode 1 at North slope of Pico Central
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1450 ± 50 years Confirmed Eruption
Episode 1 | Eruption | |||||||||||||||
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1450 ± 50 years - Unknown | Evidence from Correlation: Anthropology | ||||||||||||||
List of 1 Events for Episode 1
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0090 ± 100 years Confirmed Eruption
Episode 1 | Eruption | Pico Central | |||||||||||||||||||
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0090 ± 100 years - Unknown | Evidence from Isotopic: 14C (uncalibrated) | |||||||||||||||||||
List of 2 Events for Episode 1 at Pico Central
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0260 BCE ± 75 years Confirmed Eruption
Episode 1 | Eruption | Pico Central | |||||||||||||||||||
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0260 BCE ± 75 years - Unknown | Evidence from Isotopic: 14C (uncalibrated) | |||||||||||||||||||
List of 2 Events for Episode 1 at Pico Central
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0370 BCE ± 200 years Confirmed Eruption
Episode 1 | Eruption | Pico Central | ||||||||||||||||||||||||
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0370 BCE ± 200 years - Unknown | Evidence from Isotopic: 14C (uncalibrated) | ||||||||||||||||||||||||
List of 3 Events for Episode 1 at Pico Central
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2710 BCE ± 75 years Confirmed Eruption
Episode 1 | Eruption | Yepocapa | ||||||||||||||||||||||||||||||||||
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2710 BCE ± 75 years - Unknown | Evidence from Isotopic: 14C (uncalibrated) | ||||||||||||||||||||||||||||||||||
List of 5 Events for Episode 1 at Yepocapa
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There is no Deformation History data available for Acatenango.
There is no Emissions History data available for Acatenango.
Maps are not currently available due to technical issues.
The maps shown below have been scanned from the GVP map archives and include the volcano on this page. Clicking on the small images will load the full 300 dpi map. Very small-scale maps (such as world maps) are not included.
The following 1 samples associated with this volcano can be found in the Smithsonian's NMNH Department of Mineral Sciences collections, and may be availble for research (contact the Rock and Ore Collections Manager). Catalog number links will open a window with more information.
Catalog Number | Sample Description | Lava Source | Collection Date |
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NMNH 117395-7 | Lava | -- | 2 Feb 1980 |
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. |
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 Acatenango. 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 Acatenango. 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 Acatenango | 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). |