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Little Hungarian Plain volcano

Volcanic field 433 m / 1421 ft
Hungary, 47.19°N / 17.2°E
Current status: (probably) extinct (0 out of 5) | Reports
Little Hungarian Plain volcano books
Typical eruption style: unspecified
Little Hungarian Plain volcano eruptions: None during the past 10,000 years
Less than 2.58 million years ago (Pleistocene) No recent earthquakes
TimeMag. / DepthDistanceLocation

Background:

The Little Hungarian Plain Volcanic Field (also called the Kemenesalja Hills) area in western Hungary contains a group of Pliocene-to-Pleistocene cones (Bleahu et al. 1973, Poka 1988). Martin et al. (2003) described it, and the Bakony-Balaton Highland field to the south, as an eroded phreatomagmatic field with remnants of nested maar complexes, multiple vent systems, and individual tuff rings.
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Smithsonian / GVP volcano information


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