The suevite page
According to the IUGS Subcommission on the Systematics of Metamorphic Rocks, Study Group for Impactites, a suevite or suevite breccia is a polymict impact breccia with clastic matrix and mineral clasts in various stages of shock metamorphism including cogenetic impact melt particles which are in a glassy or crystallized state.
Suevite, Lake Mien (Sweden) impact structure.
Originally, suevite was the name of a melt breccia in the Ries crater and derived from the province of Swabia in southern Germany, and such means "Swabian stone". For decades, the Ries crater suevite was considered a peculiar volcanic breccia and unique in the world. Both the volcanic origin and the uniqueness had to be abandoned when the Ries suevite was shown to be a strongly shocked impactite and comparable rocks were found in many other impact structures worldwide.
Only recently, within the frame of a new debate about the impactite nomenclature [see, e.g., http://www.lpi.usra.edu/meetings/lmi2008/pdf/3033.pdf , http://www.bgs.ac.uk/SCMR/docs/papers/paper_11.pdf ], the Ries suevite and its classification have been revisited (Osinski,G.R., 2003, MAPS 38, 1641-1668; Osinski, G.R., 2004, EPSL 226, 529-543), and it is suggested the Ries suevite to be rather an impact melt rock (also see discussion on http://www.impact-structures.com/impactmeltpage.html).
On this page, we show and describe suevites from different impact structures (Ries - according to the customary classification, Rochechouart, Dellen, Mien, Sääksjärvi, Lappajärvi, Siljan, Kara, Wanapitei) with special emphasis on the suevites from the Azuara and Rubielos de la Cérida impact structures (Spain).