TELL EL-RETABA
EGYPT
E-W. Local anomalies of lowered resistivity
on the ERT section along survey line M2
mark the location of clayey material which
is 2 m thick. Below it, at a depth from 3 to
6 m, there are features of greater resistivity,
approximately 3 m thick, interpreted as being
of stone. These could be the foundations of
mud-brick structures, for example.
REFERENCES
Adriani, A.
1932-1933 Scoperte e scavi. Alessandria. Scoperte di tombe ellenistiche della necropoli di
Hadra, Annuario del Museo Greco-roma.no 1, Alexandria
Neuffer, E., Bittel, K., Schott, S.
1932 Bericht iiber die zweite vom Deutschen Institut fur Agyptische Altertumskunde nach dem
Ostdelta-Rand und in das Wadi Tumilat unternommene Erkundungsfahrt, MDAIK 2,
39-73
Klemm, R., Klemm, D.D.
1993 Steine und Steinbrincke im Alten Aegypten, Berlin: Springer
Lucas, A., Harris, J.R.
1962 Ancient Egyptian Materials and Industries, Mineola, NY: Dover
Morris, E.F.
2005 The architecture of imperialism. Military bases and the evolution of foreign policy in Egypt’s
New Kingdom [=Probleme der Agyptologie 22], Leiden: Brill Academic Publishers
Naville, E.
1887 The Shrine of Soft El Henneh and the Land of Goshen (1885) [-Egypt Exploration Fund
Memoir 5], London: Triabner
Nenna, M-D., Seif El-Din, M.
2000 La vaisselle en faience d’epoque greco-romaine [-Etudes Alexandrines 4], Cairo: IFAO
Petrie, W.M.F., Duncan, J.G.
1906 Hyksos and Israelite Cities, London: Office of the School of Archaeology
Redissi, T.
1994 Les coupelles a bee verseur en faience de Carthage [in:] C. Berger El-Naggar (ed.), Etudes
isiaques, Hommages a Jean Leclant, 3 [-BdE 106], Cairo: IFAO, 423-434
Redmount, C.A.
1989 On an Egyptian/Asiatic Frontier: An Archaeological History of the Wadi Tumilat, Chicago:
University of Chicago Press
Rushdi, S. (ed.)
1962 The Geology of Egypt, Amsterdam: Elsevier
151
Polish Archaeology in the Mediterranean 19, Reports 2007
EGYPT
E-W. Local anomalies of lowered resistivity
on the ERT section along survey line M2
mark the location of clayey material which
is 2 m thick. Below it, at a depth from 3 to
6 m, there are features of greater resistivity,
approximately 3 m thick, interpreted as being
of stone. These could be the foundations of
mud-brick structures, for example.
REFERENCES
Adriani, A.
1932-1933 Scoperte e scavi. Alessandria. Scoperte di tombe ellenistiche della necropoli di
Hadra, Annuario del Museo Greco-roma.no 1, Alexandria
Neuffer, E., Bittel, K., Schott, S.
1932 Bericht iiber die zweite vom Deutschen Institut fur Agyptische Altertumskunde nach dem
Ostdelta-Rand und in das Wadi Tumilat unternommene Erkundungsfahrt, MDAIK 2,
39-73
Klemm, R., Klemm, D.D.
1993 Steine und Steinbrincke im Alten Aegypten, Berlin: Springer
Lucas, A., Harris, J.R.
1962 Ancient Egyptian Materials and Industries, Mineola, NY: Dover
Morris, E.F.
2005 The architecture of imperialism. Military bases and the evolution of foreign policy in Egypt’s
New Kingdom [=Probleme der Agyptologie 22], Leiden: Brill Academic Publishers
Naville, E.
1887 The Shrine of Soft El Henneh and the Land of Goshen (1885) [-Egypt Exploration Fund
Memoir 5], London: Triabner
Nenna, M-D., Seif El-Din, M.
2000 La vaisselle en faience d’epoque greco-romaine [-Etudes Alexandrines 4], Cairo: IFAO
Petrie, W.M.F., Duncan, J.G.
1906 Hyksos and Israelite Cities, London: Office of the School of Archaeology
Redissi, T.
1994 Les coupelles a bee verseur en faience de Carthage [in:] C. Berger El-Naggar (ed.), Etudes
isiaques, Hommages a Jean Leclant, 3 [-BdE 106], Cairo: IFAO, 423-434
Redmount, C.A.
1989 On an Egyptian/Asiatic Frontier: An Archaeological History of the Wadi Tumilat, Chicago:
University of Chicago Press
Rushdi, S. (ed.)
1962 The Geology of Egypt, Amsterdam: Elsevier
151
Polish Archaeology in the Mediterranean 19, Reports 2007