PILOT SITES

Pilot Site 1 – Kalopodi, Greece
Pilot Site 2 – Ventotene, Italy
Pilot Site 3 – Aegina Island, Greece
Pilot Site 4 – Choirokoitia, Cyprus
Pilot Site 5 – Epidaurus, Greece   
Pilot Site 6 – Roseninsel, Germany
Pilot Site 7 – Argilliez, Switzerland
Pilot Site 8 – Smuszewo, Poland

Pilot Site 1 – Kalopodi, Greece

In ancient Phokis, lies the sanctuary of Kalapodi. Since 1974, in excavations conducted by the DAI, two temple complexes and surrounding structures, (ca. 1300 BC to 700 AD), came to light. Phenomena of frost pose a constant danger to the site’s materials which, in combination with the vulnerable structural materials, cause decay problems.

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Pilot Site 2 – Ventotene, Italy

Ventotene was recently voted the historical capital of European morals and intellect. The archaeological site of Villa di Giulia is located at Capo Eolo, in correspondence with a stretch of coast facing west in the northern sector of the island of Ventotene, in the province of Latina. The Island of Ventotene is of volcanic origin and constitutes the wreck of an ancient caldera of which only the islands of Ventotene and Santo Stefano, are witnesses today. The geological nature of the rocky outcrops in Ventotene predisposes them to phenomena of intense alteration connected to meteorological agents and marine erosion that occurs intensely along the coasts. These cause an extensive and visible landslide which manifests itself in the form of blocks delimited by a steep coastal wall and delimited upstream by open fractures.

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Pilot Site 3 – Aegina Island, Greece

Aegina Kolonna, a major archaeological site at the North-West tip of the island of Aegina in the Saronic Gulf, was one of the major hubs of the Aegean Bronze Age. The site lies next to the shore; it opens to the sea on the west side, which is characterized by a steep cliff. The prehistoric settlement consists of an inner area and suburbs on the east site. Due to the long excavation since the end of the 19th century, many prehistoric to archaic walls in the Outer suburb were exposed for decades, leading to underwashing of walls and foundations. The deep excavation cuts with high upcoming walls were problematic for the stability of the walls. This area is exposed to winter storms and constant waves produced by the heavy traffic between Aegina and Athens (a commercial ferry boat every half hour; heavy private traffic).  

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Pilot Site 4 – Choirokoitia, Cyprus

Choirokoitia is listed as a UNESCO World Heritage Site as it is one of the best-preserved Neolithic sites in the Mediterranean. It represents the Aceramic Neolithic of Cyprus at its peak, around the beginning of 9th millennium. The Choirokoitia site is located in the District of Larnaka, about 6 km from the southern coast of Cyprus, in the valley of the Agios Minas River, at the foot of the Troodos mountain range, on the slopes of a hill partly enclosed in a loop of the Maroni River. Monitoring natural hazards due to CC of CH sites facilitate the early recognition of potential risks and enables effective conservation monitoring and planning. Landslides, earthquakes, rock falls, ground subsidence and erosion are the predominant natural hazards in Cyprus, which pose serious disadvantages to CH sites as well as potential danger to tourists.

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Pilot Site 5 – Epidaurus, Greece

Ancient Epidaurus comprises a CH site of highly significant underwater and coastal CH dated to 12th century B.C. The Sunken City, is located in the bay of Agios Vlasios, near Ancient Epidaurus. Bio-erosion is one of the most obvious risks faced by these underwater and coastal archaeological findings. The Sunken City and the coastal CH findings are slowly being eroded by the presence of water and microorganisms. The danger due to sea level rise is threatening the coastal archaeological findings, while coastal erosion is yet another threat.

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Pilot Site 6 – Roseninsel, Germany

Roseninsel and the surrounding shallow water area form one of the 111 sites of the transnational serial UNESCO World Heritage Site “Prehistoric Pile Dwellings around the Alps”. In addition, the site comprises archaeological remains of the Roman, Early Medieval, Medieval, and post Medieval periods as well as historical monuments and a garden monument dating to the 19th century. As a first step towards systematic monitoring of the site, BLFD established a measuring system that serves as the basis for systematic observation of the site. A total of 174 measuring posts were positioned into the shallow water zone around Roseninsel. The programme produced evidence for a substantial reorganisation of the shore-zone of the island in the early medieval period, which is dendrochro nologically dated to the years around 700 AD.

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Pilot Site 7 – Argilliez, Switzerland

Les Argilliez is one of the 111 sites of the transnational serial UNESCO World Heritage Site “Prehistoric Pile Dwellings around the Alps”. It is a fully submerged pile dwelling located in the bay of Gorgier on the north shore of Lake Neuchâtel, at a depth of 2 to 3 meters, covered by a layer of pebbles of anthropic and natural origin. Dating suggests the construction of two successive villages in the Classical Cortaillod, between 3841 and 3817 BC, then in the Late Cortaillod, around 3500 BC. This palafitte is listed as UNESCO World Heritage Sites (CH-NE-02).

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Pilot Site 8 – Smuszewo, Poland

In Smuszewo, relics of fortified settlement from the Late Bronze/Early Iron Age have been found. It is listed as the highest level of archaeological heritage protection in Polish legislation. It is located, at the bottom of a postglacial valley now filled by waters of two lakes, separated by an isthmus on top of which the fortified settlement is located. Only a few such settlements have been recorded and all of them are threatened by climate changes and related anthropogenic activities. Fluctuating water level affects the wooden structures of the fortified settlement and other organic materials both within and around the settlement. The decrease in precipitation transforms farming practices, in particular attempts to retain water in the fields surrounding the valley and lakes. This further aggravates the lowering of the water level in the reservoirs.

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