PROVIDING A RESEARCH COMPONENT TO A GEOLOGY AND ARCHAEOLOGY FIELD TRIP TO GREECE
The goal of the first project is determine which palace destructions, if any, can be attributed to the same seismic event. Vectors determined from fallen blocks/walls were measured at Agia Triada, Mochlos, Palaikastro, and Knossos. Encouraging preliminary results suggest that enough evidence may survive to delineate paleoepicenters. The second project developed from recognition that palace walls at Phaistos and Agia Triada, in southeastern Crete, are exactly oriented to the modern magnetic pole which has a declination of 2º off of true north. This contrasts with the orientations of most sites on the north side of the island.
A frustrating problem of the Minoan eruption of Santorini (Thera) is the inability to date the exact year in which the c. 1630 BCE eruption took place. Since the eruption, numerous headward-eroding ravines have exposed many kilometers along the basal contact. We assume that the Minoan/Cycladic culture that inhabited Santorini grew olives like their counterparts on Crete. Detailed examination along the base of the airfall deposits at bottom of the Minoan ash may reveal carbonized wood for dendrochronological study. We plan to return with a team of students for further investigation.
Student involvement in research stemming from collaborative teaching in geology and archaeology provides the potential to develop reliable relative and numerical chronologies in Minoan archaeology. It may also offer important insight on prehistoric Minoan architectural design.