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  • The eruptive history of the Tihany Peninsula (Lake Balaton, Hungary) has been studied in detail to understand the evolution of volcanic and tectonic structures. Tectonic and depositional features indicate a maar-type origin of the Outer Lake
  • . This is the main volcanic structure of peninsula and phreatomagmatic activity probably began here. The lapilli and coarse ashes in the pyroclastites are generally mud-coated, accretionary lapilli are common, and the tuffs are frequently light brownish, suggesting