Larderello

Photo of this volcano
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  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 43.25°N
  • 10.87°E

  • 500 m
    1640 ft

  • 211001
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

The Global Volcanism Program has no activity reports for Larderello.

The Global Volcanism Program has no Weekly Reports available for Larderello.

The Global Volcanism Program has no Bulletin Reports available for Larderello.

Basic Data

Volcano Number

Last Known Eruption

Elevation

Latitude
Longitude
211001

1282 CE

500 m / 1640 ft

43.25°N
10.87°E

Volcano Types

Explosion crater(s)

Rock Types

Major
No Data (checked)

Tectonic Setting

Subduction zone
Continental crust (> 25 km)

Population

Within 5 km
Within 10 km
Within 30 km
Within 100 km
8,678
13,609
106,985
3,243,642

Geological Summary

Larderello, one of the world's most productive geothermal areas, is located in the southern part of the Tuscany region of Italy. This extensive solfatara field lies in an area underlain by sediments of Eocene-to-Pliocene age. The geothermal activity is considered to be related to a cooling granitic pluton of Pliocene age beneath sedimentary and metamorphic rocks ranging from Paleozoic to Tertiary age, although the area is cut by faults with hydrothermal mineralization related to Pliocene-to-Quaternary Tuscan magmatism. The only surficial morphological manifestation of volcanism is a series of about a dozen explosion craters 30-250 m in diameter. The Lago Vecchienna crater, now filled by a 250-m-wide lake, ejected blocks and ash during a phreatic eruption in about 1282 CE (Marinelli, 1969).

References

The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography.

Bellani S, Brogi A, Lazzarotto A, Liotta D, Ranalli G, 2004. Heat flow, deep temperatures and extensional structures in the Larderello geothermal field (Italy): constraints on geothermal fluid flow. J Volc Geotherm Res, 132: 15-29.

Boyce A J, Fulignati P, Sbrana A, 2003. Deep hydrothermal circulation in a granite intrusion beneath Larderello geothermal area (Italy): constraints from mineralogy, fluid inclusions and stable isotopes. J Volc Geotherm Res, 126: 243-262.

Katsui Y (ed), 1971. List of the World Active Volcanoes. Volc Soc Japan draft ms, (limited circulation), 160 p.

Keller W D, 1946. The natural steam at Larderello, Italy. J Geol, 54: 327-334.

Krafft M, 1974. Guide des Volcans d'Europe. Neuchatel: Delachaux & Niestle, 412 p.

Marinelli G, 1969. Some geological data on the geothermal areas of Tuscany. Bull Volc, 33: 319-333.

Petrucci E, Sheppard S M F, Turi B, 1993. Water/rock interaction in the Larderello geothermal field (southern Tuscany, Italy): an 18O/16O and D/H isotope study. J Volc Geotherm Res, 59: 145-160.

Ruggieri G, Gianelli G, 1999. Multi-stage fluid circulation in a hydraulic fracture breccia of the Larderello geothermal field (Italy). J Volc Geotherm Res, 90: 241-261.

Villa I M, Riggieri G, Puxeddu M, Bertini G, 2006. Geochronology and isotope transport systematics in a subsurface granite from the Larderello-Travale geothermal system (Italy). J Volc Geotherm Res, 152: 20-50.

Eruptive History


Summary of Holocene eruption dates and Volcanic Explosivity Indices (VEI).


Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1282 (in or before) Unknown Confirmed 3 Historical Observations Lago Vecchienna

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

Lardarello | Larderello-Travale

Craters

Feature Name Feature Type Elevation Latitude Longitude
Vecchienna, Lago
    Sulfureo, Lago
Crater

Photo Gallery


Steam pours from cooling towers at Larderello, one of the world's most productive geothermal areas. Larderello is located in the Tuscany region of Italy, at a solfatara field in an area underlain by sediments of Eocene-to-Pliocene age. The only surficial morphological manifestation of volcanism is a series of about a dozen explosion craters 30-250 m in diameter. The youngest of these, the Lago Vecchienna crater, ejected blocks and ash during a phreatic eruption in about 1282 AD and is now filled by a 250-m-wide lake.

Photo by Giuseppina Kysar, 1985 (Smithsonian Institution).

Smithsonian Sample Collections Database


A listing of samples from the Smithsonian collections will be available soon.

Affiliated Sites

Large Eruptions of Larderello 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.