Fig. 1. Ophiolite mélange near the town of Srebrenik. Oblate to tabular blocks of basalt and diabase in sheared serpentinite matrix.

 Fig. 2. Panoramic view of the Tinja river valley with medieval caste of Srebrenik. The prominent ridge where the castle is build on is of Paleogene limestone.

 Fig. 3. Slump folding in Paleogene limestone along the Srebrenik Tuzla road. Geologists are Dražen Balen (left) and Hazim Hrvatović (right).

 Fig. 4. Outcrop of Lower Oligocene (30 Ma) high-K volcanic rocks (shoshonite rocks) in the town of Maglaj.

 Fig. 5. Conglomerates of the Pogari series exposed on Maglaj-Zavidovići roadcut comprising clasts of mafic and ultramafic rocks, limestones, red granites; geologist are Jakob Pamić (left), Dražen Balen (right).

 Fig. 6. Sandstone and conglomerate beds in Pogari series outcropping along the Maglaj-Zavidovići road, Bosna river valley.

 Fig. 7. Pogari series conglomerate with clasts of ultramafics (bottom left), red granites (centre) and limestones (top right) in sandy matrix.

 Fig. 8. Pillows in basalt of the Krivaja-Konjuh massif at the locality of Željava.

 Fig. 9. Tight to isoclinal folding in radiolarite series at the locality of Kovači.

 Fig. 10. Bedding-cleavage (trending from top left to bottom right) relationship indicating overturned strata in "flysch bosniaque" series at the locality of Vranduk, Bosna river valley.

 Fig. 11. Small-scale fold in overturned strata of "flysch bosniaque" series at the locality of Vranduk, Bosna river valley.

 Fig. 12. Panoramic view of the canyon of Neretva river cut in Jurassic carbonate platform sequence at the locality of Aleksin Han.

 Fig. 13. Spectacular folding at the front of a regional-scale fold nappe at the locality of Drežanka, Neretva canyon.

 Fig. 14. A sample showing kink-folding in "greenschists" from Mid-Bosnian Schist Mts, at locality of Bradina.

Foto 1. Late Anisian-Ladinian dolomite-chert sequence with green colored tuff intercalations ("Pietra verde") on the southern slope of Svilaja Mt. (30 km north of Split).

Foto 2. Folding in Lower Triassic (Scythian) sediments at the front of High Karst nappe (southern slope of Svilaja Mt., 30 km north of Split).

Foto 3. Panoramic view of Omiš bay showing imbricate slices of Late Cretaceous limestones (massive and white) and Middle to Late Eocen carbonate flysch (pale brown and mostly covered by vegetation).

Foto 4. Overturned syncline in Middle to Late Eocene carbonate flysch in the lowermost exposed imbricate slice near the town of Omiš.

Foto 5. Coastal hinterland north of Makarska.

Foto 6. Dubrovnik - PANCARDI 2000 Host Town.