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The Climate, Environment and Industries of Stone Age Greece: Part II

Published online by Cambridge University Press:  27 May 2014

E. S. Higgs
Affiliation:
Department of Archaeology & Anthropology, Cambridge
C. Vita-Finzi
Affiliation:
University College, London

Extract

In 1965 the investigations described in the first paper of the series were resumed in Epirus. The excavation of the rock shelter of Asprochaliko was continued, and further geological observations made it possible to establish a continental sequence extending from the Last Interglacial to the present day.

The geological succession and its associated artifacts was worked out in the Louros valley (fig. 1) and confirmed in other parts of Epirus. It consists of the following three main formations:

3. Valley-floor Alluvium (pl. 1, upper). 2. Red Beds. 1. Tufa.

There are also extensive sheets of unconsolidated scree on the valley sides, as Hey has noted. These overlie the Red Beds, but as their relationship to the Valley-floor Alluvium is not known, and as the extent of contemporary scree formation (if any) is not yet clear, they cannot at this stage be placed in the succession.

Type
Research Article
Copyright
Copyright © The Prehistoric Society 1966

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References

page 1 note 1 Dakaris, S. I., Higgs, E. S. and Hey, R. W., ‘The Climate, Environment and Industries of Stone Age Greece’, Part 1. PPS, xxx, 1964, 199–244, 226, 228Google Scholar.

page 2 note 1 Dakaris, S. I., Higgs, E. S. and Hey, R. W., ‘The Climate, Environment and Industries of Stone Age Greece’, Part 1. PPS, xxx, 1964, 227–8Google Scholar.

page 2 note 2 ibid., 212.

page 3 note 1 Pettijohn, F. J., Sedimentary Rocks, Harper & Bros., N.Y., 2nd edition, 192–3.Google Scholar

page 3 note 2 Dakaris, S. I., Higgs, E. S. and Hey, R. W., ‘The Climate, Environment and Industries of Stone Age Greece’, Part 1. PPS, xxx, 1964, 213–29Google Scholar.

page 4 note 1 Tippett, H., PPS, xxx, 1964, 222–3Google Scholar.

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page 6 note 1 Paraskevaidis, I., ‘Observations sur le Quaternaire de la Grèce’, Actes IV Cong. Int. Quat. (INQUA), Rome-Pisa, 19531956, 167–8Google Scholar, reports a Tyrrhenian beach near Preveza which is overlain by what would appear to be the Red Beds.

page 7 note 1 See, for example, Negris, P., La Regression Quatemaire, Athens, 1912Google Scholar, and ‘Les terrasses marines de la Grèce’, 1st Rep. Com. Plio. Pleist. Terr., ed. Sandford, K. S., Oxford, 1928, 1826.Google ScholarMistardis, G. G., ‘Recherches sur l'influence des mouvement eustatiques du Quaternaire sur la morphologie de la zone côtière du nord du Peloponèse’, C.R. XVIII Cong. Int. Geog., Rio de Janeiro, 1956—vol. 2, 1960, 324–8, notes on p. 327Google Scholar the presence of red continental deposits over a 50-metre Tyrrhenian beach.

page 7 note 2 Probably the ‘neogene conglomerates’ mentioned by Mistardis, op. cit., 326.

page 8 note 1 7380±240 B.P. (I.1959).

page 8 note 2 Sestini, A., ‘Tracce glaciali nel Pindo epirota’, Boll. R. Soc. Geog. It., LXX, 136–56Google Scholar. Other references are discussed by Charlesworth, J. K., The Quaternary Era, vol. 2, Arnold, 1957, 296, 322, 652, 719 and 1220Google Scholar, and Butzer, K. W., Environment and Archeology, Methuen, London, 1965, 62, 102, 286Google Scholar.

page 8 note 3 Admiralty Handbook, Greece, vol. 3, 1945, 27Google Scholar.

page 8 note 4 Dakaris, Higgs and Hey, op. cit., 213.

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page 24 note 5 Higgs, E. S., ‘Faunal Fluctuation and Climate in Libya’, Wenner-Gren Foundation, Burg Wartenstein Symposium, 1965Google Scholar, on ‘Systematic Investigation of the African Later Tertiary and Quaternary’.

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