EARTHQUAKES, LANDSLIDES AND THE PERFECT STORM: GEOARCHAEOLOGY OF COMPLEX LANDSCAPE INTERACTIONS AT MYCENAE, GREECE, 3.2 KA–2.8 KA
The site of Mycenae, located at the northern boundary of the Argolid horst-and-graben, is situated in a tectonically unstable and erosionally active zone. A previously discovered episode of fault activation, circa 3.2 ka, is marked by ceramic-dated alluvial deposits along the major axial channel, the Chavos stream. A 1.5 m thick deposit of debris flows, appearing to immediately post-date the fault activation, buried Bronze Age remains at the Lower Town of Mycenae. The author here outlines a multi-scalar approach utilizing soil micromorphology, granulometry, and standard geomorphological description for the reconstruction of the depositional history of this deposit. Initial results suggest a period of landscape instability resulting in multiple episodes of slope activation following 3.2 ka. While these results are preliminary, the emergent narrative results from the interaction of climatic and tectonic forces. The impact of human occupation on rapid landscape change is therefore questioned for the Argolid. It is hoped that the in-depth investigation of this period of rapid burial may lead to an understanding of the pre-conditions of sudden change and, by extension, to a better picture of the Argolid environment during the Mycenaean collapse.