Geological Structure of the Research Area
The catchment area of Peiros-Vergas-Pinios (EL02), is geologically structured by the alpine formations of the Ionian, Tripoli and Pindos geotectonic zones and by Quaternary and Neogene deposits that have covered the tectonic subsidence in the west and south of the basin. To the east of the Ionian zone, the Gavrovos-Tripoli unit is thrusted in the […]
Geological Structure of the Research Area Read More »