- Info & Contacts
The Global Volcanism Program has no activity reports for Andahua-Orcopampa.
The Global Volcanism Program has no Weekly Reports available for Andahua-Orcopampa.
The Global Volcanism Program has no Bulletin Reports available for Andahua-Orcopampa.
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.
|Andagua Valley | Orcopampa Volcanic Field | Andahua Valley | Andagua-Orcopampa|
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Achacara, Loma||Pyroclastic cone||4150 m||15° 20' 0" S||72° 19' 41" W|
|Antaymarca, Volcán||Pyroclastic cone|
|Challhue Mauras, Volcán||Pyroclastic cone||4319 m||15° 22' 8" S||72° 19' 59" W|
|Chilcayoc Grande, Volcán||Pyroclastic cone||3150 m||15° 31' 59" S||72° 17' 17" W|
|Chilcayoc, Volcánes||Pyroclastic cone||3300 m||15° 31' 0" S||72° 18' 47" W|
|Cochapampa, Cerro||Pyroclastic cone|
|Cruz, Cerro la||Pyroclastic cone|
|Jajarana, Cerro||Pyroclastic cone||4600 m||15° 19' 23" S||72° 25' 1" W|
|Jechapita, Volcán||Pyroclastic cone||3350 m||15° 32' 0" S||72° 18' 40" W|
|Jenchana, Volcán||Pyroclastic cone||3550 m||15° 31' 1" S||72° 20' 35" W|
|Mauras, Cerro||Pyroclastic cone||4250 m||15° 20' 6" S||72° 19' 34" W|
|Misahuana Mauras, Volcán||Pyroclastic cone||4713 m||15° 15' 25" S||72° 28' 59" W|
|Pabellon Mauras, Volcán||Pyroclastic cone||4507 m||15° 17' 10" S||72° 27' 32" W|
|Pichihua, Cerro||Pyroclastic cone||4650 m||15° 17' 28" S||72° 25' 59" W|
|Pucu Mauras, Cerro||Pyroclastic cone||4287 m||15° 25' 26" S||72° 20' 13" W|
|Puma Ranga, Cerro||Pyroclastic cone||4653 m||15° 16' 0" S||72° 27' 29" W|
|Santa Rosa||Pyroclastic cone|
|Sayhua, Cerro||Pyroclastic cone||4650 m||15° 16' 1" S||72° 27' 22" W|
|Tichso, Cerro||Pyroclastic cone||3900 m||15° 28' 52" S||72° 22' 34" W|
|Yana Mauras, Volcán||Pyroclastic cone||4588 m||15° 18' 43" S||72° 25' 59" W|
|Yanamauras, Cerro||Pyroclastic cone||3775 m||15° 28' 41" S||72° 20' 53" W|
There is data available for 4 Holocene eruptive periods.
|Start Date||Stop Date||Eruption Certainty||VEI||Evidence||Activity Area or Unit|
|[ 1913 Mar 6 ]||[ Unknown ]||Uncertain|
|1490 ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)||Chilcayoc Grande|
|0940 BCE ± 100 years||Unknown||Confirmed||Radiocarbon (uncorrected)||Cerro Maurus I|
|2110 BCE ± 50 years||Unknown||Confirmed||Radiocarbon (uncorrected)||Cerro Tichsó|
There is no Deformation History data available for Andahua-Orcopampa.
There is no Emissions History data available for Andahua-Orcopampa.
|The cinder cones at the center and upper right, surrounded by a prominent field of lava flows, are located in the Andahua valley, known locally as the "Valley of the Volcanoes." The large 60 x 60 km scoria cone and lava field contains extremely youthful lava flows, some of which may be only a few hundred years old. The volcanic field was reported to have been active during the time of the Incas. Lava flows have repeatedly dammed the Río Andagua valley, and an existing small lake was impounded by the youngest lavas.
Photo by Norm Banks, 1988 (U.S. Geological Survey).
There are no samples for Andahua-Orcopampa in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.
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.|
|Large Eruptions of Andahua-Orcopampa||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).|
|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.|
|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).|