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Franchthi Cave is located on the northern tip of Kiladha Bay in the Argolid. It is a limestone formation about 150 m long and 45 m in maximum width. Most of the interior of the cave is today filled with massive breakdown from the roof. At the very back of the cave is a small pool of brackish water.

 

Excavations at the cave were carried out between 1967 and 1976 by an international archaeological team and local workers under the direction of Prof. Thomas Jacobsen. Trenches were opened in the front portion of the cave and along the beach outside the cave. The excavations revealed a rare sequence of human occupation spanning the Upper Palaeolithic to the end of the Neolithic period (ca. 25,000-3000 B.C.)

 

The life of the modern village of Kiladha revolves around the sea. Most of its residents are employed in the greek merchant marine or in commercial fishing in the immediate area and all over the world. But what was the relationship of the prehistoric residents of the area to the sea? This is the question that this exhibit will explore by means of a trip back in time. Our guides in this trip will be the changes of the prehistoric landscape as reconstructed with clues from underwater geophysical investigations in Kiladha Bay, together with some of the…trash left behind by the prehistoric users of the cave (e.g., thousands of fish bones, sea shells, and obsidian tools). Most of these finds are small and were found during the sifting of the excavated dirt in the dry and water sieves.

 

 
               

              

 

Our time trip starts ca. 25,000 B.C. in a period called Upper Palaeolithic. This is the beginning of the last Ice Age. At this time, the southern Argolid was not covered by glaciers as was northern Europe, but the climate was very dry and cold. The landscape was therefore very different than it is today. Kiladha Bay, as we know it, did not exist: The sea was about 100-120 m lower than current levels, the coast was about 6-7 km away from the cave, and in place of the bay was a vast flat plain.

 

During this time small groups of hunters of wild animals began to use the cave as a hunting camp. The excavations revealed no remains of buildings, but they did bring to light carcasses of animals (mostly of wild ass), projectile points used to hunt the prey, ashes from cooking, and small stone knives employed to cut the meat. Nothing was found (e.g., fish bones or sea shells) to suggest that these nomads exploited marine resources. It is possible, though, that they consumed both fish and shellfish at the beach without ever taking them all the way back to the cave.

The first secure evidence for the use of marine resources at Franchthi comes from the end of the Palaeolithic period, ca. 12,000-9500 B.C. By that time the Ice Age was ending, the climate got warmer, and the glaciers to the north had started to melt. The result was an expansion of the ocean and a dramatic change in the landscape: Sea level in the Franchthi area rose about 50-60 m, the plain in front of the cave shrank considerably, and the distance of the coast to the cave was reduced to about 3 km.

 

 

The cave was still not settled on a permanent basis, as indicated by the lack of architectural remains. It served as a base camp for nomadic groups that hunted primarily deer and gathered mostly wild lentils, pistachios, and almonds.

 

 
               

              

 

The nomads of the end of the Palaeolithic period , fished occasionally, as shown by a few fish bones found in deposits of this period. Most of them come from eel, sea bass, and gray mullet. These fish are typical of Mediterranean lagoons, suggesting that perhaps the beach closest to the cave at that time was a shallow lagoon. The fishing equipment of this period has not been preserved, but the catch was likely made with techniques similar to those used in modern lagoon fisheries (e.g., simple traps, spears, and complex reed enclosures).

 

The number of shells excavated in deposits of the end of the Palaeolithic period point to sea shell gathering as another activity of these nomads. The most common shells, limpets, were used as food. Shellfish was perhaps a delicacy for the prehistoric inhabitants of the cave as it is for local people today. Τhe so-called tusk shell, on the other hand, with its natural bead shape, was used as raw material for ornaments. The presence of tusk shell ornaments suggests at least two things:
• The people who used the cave at that time were interested in body ornamentation.
• They had time for activities not directly related to the everyday struggle for survival.

 

The most impressive evidence, however, for a relationship with the sea during the end of the Palaeolithic period comes from about 10 small pieces of a black shiny volcanic stone called obsidian. This is a very high quality raw material for the manufacture of tools (e.g., knives and arrowheads), and its source is located on the Cycladic island of Melos. The presence of obsidian in late Palaeolithic layers at Franchthi Cave attests to one of the oldest open sea voyages in the Mediterranean.

 

Almost all the pieces of obsidian found are less than 10 mm in maximum diameter and were found during water-sieving. Had this meticulous technique not been used at Franchthi, the tiny finds that put this site on the map of world prehistory would never have been discovered. This exceptional discovery owes a great deal to the local workers who participated in the operation of the water sieve and the Kiladha women who spent endless hours sorting the water sieve residue. They all deserve a big thank you.

 
               

              

 

Melian obsidian was taken to Franchthi either by the groups of hunter-gatherers who used the cave as one of their base camps at the end of the Palaeolithic period or through exchanges between Franchthi people and bands living closer to Melos. It can not have been taken to the cave by residents of Melos since this island was not yet permanently settled. Regardless of the way obsidian reached Franchthi, one thing is certain: some of the people who lived in southern Greece at the end of the Palaeolithic period were skillful seafarers and undertook many exploratory expeditions in the Cyclades and the Aegean in general. Otherwise they would not have discovered either the island of Melos or its obsidian sources.

 

With what means did the trip to Melos take place? Direct evidence of the seacraft from that era is lacking, since they were made of perishable materials. Boats could, however, have been similar to a papirella, a paddled reed boat used until recently in Corfu. Mr. Spyros Agathos built a papirella about 6 m long and 180 kg in weight for the archaeologists. This craft proved its worthiness during a trip it made from Laurion to Melos, surviving winds of 6 knots and waves 1.5 m high.

Why did the trip to Melos take place? Given that the quantity of obsidian found from this period is very small compared to the local flint used also for tool making, it is almost certain that the acquisition of obsidian was an incidental activity of the trip to Melos. What its principal goal was is for the moment a mystery.

 

 

 

                        

              

Our next stop is the mesolithic period, which spans 9500 to 7000 B.C. Temperatures kept rising, raising the sea level another 20 m, and bringing the coastline about 2 km from the cave.

The cave was still used, although more intensively, as a base camp for hunters of wild animals (primarily deer) and gatherers of wild plants (e.g., lentils, pears, pistachios, barley, and oats). No architectural remains have been found from this period either, but the cave was used as a place for burying some of the dead.

 

The mesolithic inhabitants of franchti fished more intensively than their predecessors. Tuna is the dominant species, but many grouper and barracuda bones were also found. These fish live in a fully marine rather than a lagoon environment. Methods suited for lagoon fisheries were no longer employed. Nets, traps, and boats were probably used, although none has been preserved. Most of the tuna caught weighed about 8-15 kg. Some, however, weighed about 200 kg!
 

 

The mesolithic inhabitants of franchti gathered large numbers of sea shells from a species called Cerithium vulgatum to eat and probably also for use as a bait. They also gathered thousands of the small sea shells known as Cyclope neritea. They ate the flesh and often turned the shell into an ornament by piercing it with a stone drill. These shells were probably strung together to form a necklace. Small sea pebbles--another material of marine origin--were also used for making ornaments in this period. A hole was made in the pebble using a stone drill, a rather difficult and time-consuming process. Some of these ornaments might look crude and unattractive but we should remember that each social group and each era has its own taste. In this sense it is unlikely that prehistoric people would find us moderns elegant.
 

 

The number of obsidian tools found in the mesolithic deposits of franchti is much higher than before, but still low compared to the number of tools made of local flint. This suggests either that the open sea voyages were not undertaken for the procurement of obsidian or that obsidian reached the cave through exchanges between the franchti dwellers and other groups. It is even possible that the shiny and exotic obsidian came to the site more like a souvenir from a faraway place rather than because it was a first rate raw material for the manufacture of tools.

 

                       

              

The fourth and last stop of our trip is during the neolithic period, which spans ca. 7000-3000 B.C. By that time sea level had risen even higher and the coast of the southern Argolid had been broken into small bays. At the beginning of this period Franchthi Cave was less than 1 km away from the coast.
 

The nature of the neolithic occupation at Franchthi was very different than earlier ones. The changes may even be called revolutionary:
• The cave no longer served as a base camp for hunter-gatherers. There was instead a permanent settlement at Franchthi--a village--which extended beyond the confines of the cave into the area in front of the cave, and also into an area that is now under-water.
• The main subsistence activities were farming and animal husbandry. Franchthi people cultivated domesticated plants (e.g., wheat, barley, and lentils) and raised domesticated animals (e.g., sheep, goats, and pigs).
• The neolithic period also marks the beginning of pottery making.
 

Although the coast was now much closer to the cave, little emphasis was given to fishing. Sea bream were the most numerous fish caught throughout the neolithic period; large tuna were rarely fished. The low emphasis on fishing may have to do with the central role of farming and husbandry in the life of the neolithic community. Only a few fishhooks made of bone were found from this period. These hooks, however, are too large to have been used to catch small fish. For this purpose, other tools, which were not preserved (e.g., nets or traps of a fine mesh), must have been employed.
 

 

               

              

The neolithic inhabitants of Franchthi gathered large numbers of cockle shells. They ate their flesh and used the shells as raw material for the manufacture of beads. They also made pendants and bracelets from the tough sea shell called spondylus and from the brittle pinna shell. The processing of these materials must have been difficult and time-consuming and was probably done by a group of ornament specialists or jewelers, as we would call them today.
 

 

The situation with obsidian is very different during the neolithic period. Obsidian now came to Franchthi in large quantities, as was the case for many other villages around Greece. There is evidence to suggest that now relatively few specialists sailed to Melos to acquire obsidian, and then traveled from village to village, making tools on demand at each location. There is no doubt that Franchthi people had the skills to sail to Melos. Nevertheless, they chose to procure this important raw material from itinerant specialists.
 

Our trip stops sometime around 3000 B.C. and ends, of course, with the sea. The sea level continued to rise, giving the bay its present configuration, shrinking the vital farming space of the Franchthi community, and eventually flooding the coastal part of the settlement. Franchthi was abandoned at that time, perhaps also as a result of massive breakdown from the roof of the cave. Exhibition: Anna Stroulia, Ph.D., Archaeology and Anthropology.
Technical supervision: Gregory Manariotis.
Sponsors: Schrader Endowment and Municipality of Kranidi.
The exhibit text is based on studies by T. Cullen, T. Jacobsen, M. Jameson, J. Hansen, M. Miller, S. Payne, C. Perlès, M. Rose, C. Runnels, J. Shackleton, T. Van Andel, and K. Vitelli.
Most of the photographic material comes from the Indiana University Archives.
M. Antoniadis, V. Dimitriou, M. Fotiadis, A. Kalogirou, M. Liossi, O. Mantzari, D. Kamizis, C. Perlès, M.R. Strezewski, M. Strezewski, and K. Vitelli helped in the preparation of the exhibit.

 

 

   
 


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