Cleopatra’s beach is one of the most famous in Turkey for its distinctive white sand, composed largely of ooids. Legend has it that the Roman leader, Mark Antony, had this sand shipped from Alexandria in Egypt to create a beach for his lower Cleopatra, on Sedir Island in Gökova Bay, SE Aegean Sea. This study examines the reality of this leagend from a comparison of the oolitic sand from Cleopatra’s beach in Turkey with oolitic sand from the coast west of Alexandria in Egypt, the home city of Cleopatra, and only place in the Mediterranea where Holocene ooids occur in abundance.
The ooids on Cleopatra’s beach gave a pale browncreamy colour and dull surface texture. Most grains are spherical, with nuclei of terrigenous grains, peloids and bioclasts. The Cleopatra ooids have all the features typical of high-energy, shallow-marine ‘classic” ooids, but they occur in a very low energy bay and shown evidence of being out place there (microborings, discolouration, dull surface). In terms of size, shape, cortex fabric and mineralogy, the Cleopatra ooids show great similarities to those from the northern coast of Egypt, west of Alexandria. The Alexandria ooids examined have a white-cream colour with a high polish, although there are fewer silicate nuclei compared to the Cleopatra ooids. On the basis of textures and microfabrics, the hydrographic conditions at Gökova bay, the relatively small quantity of oolitic sand in this tiny pocket beach and the absence of this type of sand any-where else in Turkey, it is concluded that the oolitic sand was brought to Cleopatra’s beach from somewhere else, and that the northern Egyptian coast was the most likely source. This lends credence to the Antony and Cleopatra story. Calculations suggest that some 15 Roman corn barges would have been required to transport the quantity of sand now present on the beach in Turkey.
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Anwar, Y.M., El-Askary, M.A. and Nasr, S.M. (1981): Petrography and origin of the oolitic carbonate sediments of Arab's Bay, western part of the continental shelf of Egypt.—Neues Jahrbuch Geol. Paläont. Mh.,1981/2, 65–75 Stuttgart.
Bathurst, R.G.C. (1986): Carbonate sediments and their Diagenesis (2nd Edition), 658 pp. Amsterdam, (Elsevier).
Carozzi, A.V. (1960): Microscopic Sedimentary Petrology.— 485 pp. New York, (Wiley).
El-Asmar, H.M. and Wood, P. (2000): Quaternary shoreline development: the northwestern coast of Egypt.—Quaternary Science Reviews,19, 1137–1149, Amstzerdam.
El-Sammak, A.A. and El-Sabrouti, M.A. (1992): Cortical fabrics in the coated grains of the shelf sediments between Sidi Ab del Rahman and Matruh, Egypt.—Rapp. Comm. int. Mer. Mediterranean,33, p. 130.
El-Shaikh, H. (1987): Studies in History of the Egyptian, Roman and Greek Civilizations.—181 pp., Alexandria, Egypt (Marefa Publications,in Arabic).
Eseller, G. (1990): Modern ooids from Sedir Island (Cleopatra Beach). South Aegean Sea.—International Earth Sciences Congress on Aegean Region, p. 101–102, Izmir-Türkiye.
Flügel, E. (1982). Microfacies Analysis of Limestones.—633 pp., Berlin, (Springer-Verlag).
Hilmy, M.E. (1951): Beach sands of the Mediterranean coast of Egypt.—J. Sediment. Petrology,21, 109–120, Tulsa.
Millero, F. and Sohn, M. (1991): Chemical Oceanography.—350 pp., Florida, (CRC Press Inc.).
Özhan, E. (1990): The legend of Cleopatra Beach: May it be true? —Eurocoast, 98–103, Marseilles.
Parker, A.J. (1992): Ancient Shipwrecks of the Mediterranean and the Roman Provinces.—547 pp. Oxford (Hadrian Books Ltd).
Rickman, G. (1980): The corn Supply of Ancient Rome.—280 pp., Oxford (Clarendon Press).
Said, R. (1993): The river Nile: Geology, Hydrology and Utilization.— 250 pp., Oxford (Pergamon Press).
Sass, E, Weiler, Y. and Katz A (1972). Recent sedimentation and oolite formation in the Ras Materma Lagoon, Gulf of Suez. In: Stanley, D. (Ed) The mediterranean Sea, p. 279–192. New York (Dowden, Hutchinson and Ross Inc).
Selim, A.A. (1974): Origin and lithification of the Pleistocene carbonates of the Salum area, western coastal plain of Egypt.— J. Sediment. Petrology,44, 70–78. Tulsa.
Shukri, N.M., Philip, G. and Said, R. (1956): The geology of the mediteranean coast between Rosetta and Bardia. Part II. Pleistocene sediments, geomorphology and microfacies. Bull. Inst. Egypt37, 395–433, Cairo.
Stanley, D.J. and Hamza, F.H. (1992): Terrigenous-carbonate sediment interface (Late Quaternary) along the northwestern margin of the Nile deltam, Egypt. J. Coastal Res.,8, 153–171. Fort Lauderdale.
Strabo, 7BC. Geography, book 14, chapter 5, section 3.
Strasser, A., Davaud, E. and Jedouni, Y. (1989): Carbonate cements in holocene beachrock: an example from Bahirit el Biban, southern Tunisia. Sedimentary geology,62, 89–100, Amsterdam.
Tucker, M.E. and Wright, V.P. (1990): Carbonate sedimentatology. —482 pp., Oxford (Blackwell Science).
Üsenmez, S., Varol, B., Friedman, G. and Tekin, E. (1993): Modern ooids of Cleopatra beach, Gökova (South Aegean Sea) Turkey: results from petrography and scanning electron microscopy.— Carbonates and Evaporites,8, 1–8, New York.
Wali, A.M.A., Brookfield, M.E. and Schreiber B.C. (1994): The depositional and diagenetic evolution of the coastal riges of northwestern Egypt.—Sedimentary Geology,90, 113–136, Amsterdam.
Warne, A.G. and Stanley, D.J. (1993): Late Quaternary evolution of the northwest Nile Delta and adjacent coast in the Alexandria region, Egypt. J. Coastal Res.,9, 26–64, Fort Lauderdale.
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El-Sammak, A., Tucker, M. Ooids from Turkey and Egypt in the Eastern Mediterranean and a love-story of Antony and Cleopatra. Facies 46, 217–227 (2002). https://doi.org/10.1007/BF02668082
- Recent ooids
- oolitic beach sands
- eastern mediterranean
- antony and cleopatra
- cleopatra’s Beach (Turkey)