Global Volcanism Program | Bakony-Balaton Highland

The Global Volcanism Program has no activity reports for Bakony-Balaton Highland.

The Global Volcanism Program has no Weekly Reports available for Bakony-Balaton Highland.

The Global Volcanism Program has no Bulletin Reports available for Bakony-Balaton Highland.

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

Transdanubia

Cones

Feature Name

Feature Type

Elevation

Latitude

Longitude

Agarteto
Tikhegy
Bondoro

Shield volcano

513 m

46° 58' 0" N

17° 30' 0" E

Apatihegy

Cone

447 m

46° 55' 0" N

17° 35' 0" E

Badascony

Shield volcano

438 m

46° 48' 0" N

17° 30' 0" E

Boglari Varteto

Cone

162 m

46° 47' 0" N

17° 40' 0" E

Csobanc

Cone

376 m

46° 50' 0" N

17° 31' 0" E

Fekete-hegy Volcanic Complex

Cone

444 m

46° 54' 51" N

17° 34' 36" E

Gulacs

Cone

393 m

46° 50' 0" N

17° 30' 0" E

Halap

Cone

361 m

46° 55' 0" N

17° 28' 0" E

Halyagos

Cone

334 m

46° 53' 0" N

17° 31' 0" E

Harasztos

Cone

200 m

46° 51' 22" N

17° 33' 30" E

Hegyesd

Cone

281 m

46° 55' 0" N

17° 31' 0" E

Kabhegy
Pulai
Somhegy

Shield volcano

600 m

47° 3' 0" N

17° 40' 0" E

Kopacsihegy
Kopacsi-hegy

Cone

355 m

46° 54' 7" N

17° 32' 42" E

Kopasz-hegy Volcanic Complex

Cone

288 m

46° 52' 25" N

17° 32' 28" E

Koveshegy

Cone

46° 53' 0" N

17° 31' 0" E

Matehegy

Cone

46° 55' 0" N

17° 35' 0" E

Nagylaz
Kislaz

Vent

344 m

46° 54' 0" N

17° 19' 0" E

Sarvaly
Praga
Tatika

Shield volcano

413 m

46° 54' 0" N

17° 16' 0" E

Satormal

Cone

46° 55' 0" N

17° 35' 0" E

Szebike

Shield volcano

348 m

46° 54' 0" N

17° 18' 0" E

Szigliget

Cone

243 m

46° 48' 0" N

17° 27' 0" E

Szt. Gyorgyhegy

Shield volcano

414 m

46° 50' 0" N

17° 27' 0" E

Totihegy

Cone

346 m

46° 50' 0" N

17° 32' 0" E

Craters

Feature Name

Feature Type

Elevation

Latitude

Longitude

Tihanyi Felsziget

Maar

232 m

46° 54' 0" N

17° 51' 0" E

Basic Data

Volcano Number

Last Known Eruption

Elevation

Latitude
Longitude

210805

Pleistocene

600 m / 1968 ft

46.92°N
17.63°E

Volcano Types

Volcanic field

Tectonic Setting

Intraplate
Continental crust (> 25 km)

Geological Summary

The Bakony-Balaton Highland Volcanic Field ia a large area of monogenetic Pliocene-to-Pleistocene basaltic shield volcanoes and cinder cones located around Lake Balaton in western Hungary (Bleahu et al. 1973, Poka 1988). The age of volcanism, as summarized by Kereszturi and Nemeth (2011), extended from ~7.94 to 2.29 Ma.

References

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

Bleahu M D, Boccaletti M, Manetti P, Peltz S, 1973. Neogene Carpathian arc: a continental arc displaying the features of an 'island arc'. J Geophys Res, 78: 5025-5032.

IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..

Kereszturi G, Nemeth K, 2011. Shallow-seated controls on the evolution of the Upper Pliocene Kopasz-hegy nested monogenetic volcanic chain in the Western Pannonian Basin (Hungary). Geologica Carpathica 62:6, p. 535-546. http://dx.doi.org/10.2478/v10096-011-0038-3

Martin U, Nemeth K, Auer A, Breitkreuz C, 2003. Mio-Pliocene Phreatomagmatic Volcanism in a Fluvio-Lacustrine Basin in Western Hungary. GeoLines 15, p. 84-90.

Nemeth K, Martin U, 1999. Large hydrovolcanic field in the Pannonian Basin: general characteristics of the Bakony-Balaton Highland Volcanic Field, Hungary. Acta Vulcanologica 11:2, 271-282.

Pecskay Z, Lexa J, Szakacs A, Seghedi I, Balogh K, Konecny V, Zelenka T, Kovacs M, Poka T, Fulop, Marton E, Panaiotu C, Cvetkovic V, 2006. Geochronology of Neogene magmatism in the Carpathian arc and intra-Carpathian area. Geologica Carpathica 57:6, p. 511-530.

Poka T, 1988. Neogene and Quaternary volcanism of the Carpathian-Pannonian region: changes in chemical composition and its relationship to basin formation. Amer Assoc Petrol Geol Mem, 45: 257-277.

Eruptive History

The Global Volcanism Program is not aware of any Holocene eruptions from Bakony-Balaton Highland. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Bakony-Balaton Highland page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

Deformation History

There is no Deformation History data available for Bakony-Balaton Highland.

Emission History

There is no Emissions History data available for Bakony-Balaton Highland.

The Global Volcanism Program has no photographs available for Bakony-Balaton Highland.

Smithsonian Sample Collections Database

There are no samples for Bakony-Balaton Highland in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.

Affiliated Sites

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.

Large Eruptions of Bakony-Balaton Highland

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).