By D'Amico, Sebastiano; Department of Physics, University of Malta, Msida, Malta; Nappi, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia; Alessio, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia

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2001. Neotectonics of Turkey-a synthesis. Geodinamica Acta, 14, 3-30. , Jimenez, S. , 1998. Microdeformation of lacustrine laminite sequences from Late Miocene formations of SE Spain: an interpretation of loop bedding. Sedimentology, 45, 279– 292. Cojan, I. , 1992. Seismically-induced deformation structures in Oligocene shallow marine and eolian coastal sands (Paris Basin). Tectonophysics, 206, 79-89. , 1998. Recumbent flame structures in the Lower Gondwana rocks of the Jharia Basin, India- a plausible origin.

1996). 1A, pp. ; Burnet, R. & Strazzeri, D. (1998). Histoire et connaissance des phénomenes naturels extremes. Ingénieres-EAT, pp. 15-26 Coronelli, P. (1693). Epitome cosmografica: delle cause de’ tremuoti, Cologne, Germany Credner, H. (1884). Die erzgebirgisch-vogtländischen Erdbeben während der Jahre 1878 bis Anfang 1884. 57, pp. 1-29 Earthquakes in History – Ways to Find out About the Seismic Past of a Region 17 Credner, H. (1907). 59, pp. 333-355 Dewey, J. & Byerly, P. (1969). Earthquake Monitoring.

12) is available one more absolute age determination: in the bottom part of modern soil. Age of this sample by results of the radiocarbon analysis is 4465 ± 130 years old (SOAN-6522). This is the minimum age of the second seismic event, recorded by us: in the middle Holocene. After the 1st earthquake on the examined site of the fault the tectonic dam was formed, which has led to accumulation of impounded deposits on which the soil cover, eventually, was formed. 5 thousand years ago, was not the last earthquake on given site of the TFF.

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