Some 2,000 years ago, the ancient Greek historian Strabo mentioned the presence of an important shrine on the west coast of the Peloponnese. Archaic temple ruins have recently been discovered near Samikon at the Kleidi site, which was apparently once part of Poseidon’s shrine.
The Austrian Archaeological Institute, in collaboration with colleagues from Johannes Gutenberg University Mainz (JGU), Kiel University, and the Ephorate of Antiquities of Elis, discovered the remains of an early temple-like structure within the Poseidon sanctuary site, which was possibly dedicated to the deity himself. With its drilling and direct push techniques, the Mainz-based team from the JGU Institute of Geography led by Professor Andreas Vött contributed to the investigation.
Exceptional coastal configuration of the Kleidi/Samikon region
The form of the western coast of the Peloponnese peninsula, the region in which the site is located, is very distinctive. Along the extended curve of the Gulf of Kyparissa is a group of three hills of solid rock surrounded by coastal alluvial sediments in an area otherwise dominated by lagoons and coastal swamps.
Because this location was easily accessed and secure, a settlement was established here during the Mycenaean era that continued to flourish for several centuries and was able to maintain contacts to the north and south along the coast.
Professor Andreas Vött of Mainz University has been undertaking geoarchaeological surveys of this area since 2018 intending to clarify how this unique situation evolved and how the coast in the Kleidi/Samikon region has changed over time.
For this purpose, he has collaborated in several campaigns with Dr. Birgitta Eder, Director of the Athens Branch of the Austrian Archaeological Institute, and Dr. Erofili-Iris Kolia of the local monuments protection authority, the Ephorate of Antiquities of Elis.
“The results of our investigations to date indicate that the waves of the open Ionian Sea actually washed up directly against the group of hills until the 5th millennium BCE. Thereafter, on the side facing the sea, an extensive beach barrier system developed in which several lagoons were isolated from the sea,” said Vött, who is a Professor of Geomorphology at JGU.
However, evidence has been found that the region was repeatedly afflicted by tsunami events in both the prehistoric and historic periods, most recently in the 6th and 14th centuries CE. This tallies with surviving reports of known tsunamis that occurred in the years 551 and 1303 CE. “The elevated situation provided by the hills would have been of fundamental importance in antiquity as it would have made it possible to move on dry land along the coast to the north and to the south,” Vött pointed out.
In autumn 2021, geophysicist Dr. Dennis Wilken of Kiel University found traces of structures at a site at the eastern foot of the hill group in an area that had already been identified as of interest following previous exploration.
After initial excavation work under the supervision of Dr. Birgitta Eder in autumn 2022, these structures proved to be the foundations of an ancient temple that could well be those of the long-sought temple to Poseidon.
“The location of this uncovered sacred site matches the details provided by Strabo in his writings,” emphasized Eder, who is working for the Austrian Archaeological Institute.
An extensive archaeological, geoarchaeological, and geophysical analysis of the structure is to be conducted over the next few years. The researchers hope to establish whether it has a specific relationship with a coastal landscape that is subject to extensive transformation.
Hence, based on the geomorphological and sedimentary evidence of the recurrent tsunami events here, the geomythological aspect is also to be investigated.
It seems possible that this location may have actually been explicitly selected for the site of the Poseidon temple because of these extreme occurrences. After all, Poseidon, with his cult title of Earthshaker, was considered by the ancients to be responsible for earthquakes and tsunamis.
Natural Hazard Research and Geoarchaeology team at JGU studies the processes of coastal change and extreme wave events
For the past 20 years, the Natural Hazard Research and Geoarchaeology group at Mainz University, headed by Professor Andreas Vött, has been examining the development of the coast of Greece over the last 11,600 years. They particularly focus on the western side of Greece from the coast of Albania opposite Corfu, the other Ionian Islands of the Ambrakian Gulf, the western coast of the Greek mainland down to the Peloponnese and Crete.
Their work involves identifying relative sea level changes and the corresponding coastal changes. Another core feature of their investigations is the detection of extreme wave events of the past, which in the Mediterranean mainly take the form of tsunamis and the analysis of their impact on coasts and the communities living there.
Innovative direct push sensing—a new technique in geoarchaeology
The JGU team may posit hypotheses of what changes happened along the coastlines and throughout the terrain based on sediment cores that reveal vertical and horizontal aberrations in depositional layers. The organization currently has a collection of over 2,000 core samples gathered primarily throughout Europe.
Furthermore, they have been investigating the subterranean since 2016 utilizing a unique direct push approach. The use of hydraulic pressure to force different sensors and equipment into the ground to collect sedimentological, geochemical, and hydraulic information on the subsurface is known as direct push sensing. The Institute of Geography at Johannes Gutenberg University Mainz is the only university in Germany with the requisite equipment.