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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1975): Geological Hazards, Cambridge University Press, ISBN 3-540-06948-8, Cambridge, UK Bonito, M. (1691). Terra tremante, Naples, Italy Brunhuber, A. (1903). 2, pp. 1-14 Cavallini, F. & Rebez, A. (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.
3. The up slope facing scarp cuts channels of temporary springs where the tectonic dams are formed. An existence of the tectonic dams is the direct evidence of impulse movements along the fault during a moment of its seismic refreshment (Khromovskikh and Nikonov, 1984). 4. An intake of frontal parts of recent taluses by the upslope facing scarp testifies on youth and instantaneity of its formation. This phenomenon one can observe east of the Kara-Bura pass. If not, an ancient upslope facing scarp would be covered by the colluvial material, the talus would gush over the scarp and will continue its movement down the slope.
07 m). We examined the bore pit (Fig. 12) in the flood plain of the dry rivulet - in the SW wing of the TFF. Here the tectonic dam and impounded deposits, in connection with right-lateral Parameters of the Strong Paleoearthquakes Along the Talas-Fergana Fault, the Kyrgyz Tien Shan 37 displacements along the NE wing of the TFF, were formed. , 1992), we took a sample with absolute age of 6100 ± 200 years (SOAN-6523). At this particular time, apparently, there was the first earthquake which has displaced for the first time the body of the moraine and fluvial deposits.