Claudiu-Sorin Dragomir, Vasile Meita, Daniela Dobre, Emil-Sever Georgescu and Ioan-Sorin Borcia
and moisture content on shear resistance of collapsible soils located in the city of Galati , Romania, ROMANIA, SGEM, Conference Procedings vol. II, pp. 395-410, ISI Web of Science database up to 2011 is 3, 2012 and 2013 - in process of indexing, Albena, Bulgaria.
Călăraşu E., Dobrescu C.F., Siminea I. (2009). Decisive factors in evaluation of support elements in hazard, seismic risk and vulnerability analysis , Simpozion Ştiinţific cu participare internaţională “Protecţia mediului şi siguranţă alimentară”, Târgovişte, “Annals. Food Science and Technology
Tatiana G. Tashlykova, Tamara G. Ryashchenko, Anna A. Dolgaya and Elena A. Lukyanova
Caloi P. 1970. How nature reacts on human intervention - responsibilities of those who cause and who interpret such reaction. Ann. Geofis. (Rome), 23: 283-305.
Carder D.S. 1945. Seismic investigations in the Boulder Dam area, 1940-1944, and the influence of reservoir loading on earthquake activity. Bull. Seismol. Soc. Am., 35: 175-192.
Gahalaut K., Gahalaut V.K., Pandey M.R. 2007. A new case of reservoir triggered seismicity: Govind Ballav Pant reservoir (Rihand dam), central India. Tectonophysics
The Ust-Ilimsk water reservoir is located in the taiga zone in the Central-Siberian Upland. It was created between 1975-1977 as a result of storage of flood waters and water from the higher located Bratsk Reservoir. With an area of 1873 km2 and a water capacity amounting to 59.4 km3 it belongs to the group of largest water reservoirs in the world. It is the third level of the Angara cascade, projected as a multifunctional object - for the efficient functioning of the Ust-Ilimsk Hydroelectric Power Station, to streamline navigation on the lower Angara, to fulfil municipal and industrial water needs and also for floating timber. On the basis of the author’s own investigations and source materials obtained from the Irkutskgidromet and the Institute of the Earth’s Crust in Irkutsk, the fluctuations of the water level and the volumes of water outflow in the period 1975-2007 and the volume of processed material at the selected water shores in the period 1977-1990 were analysed. In addition, the data of seismic events in the region of the Ust-Ilimsk water reservoir were compiled. During this period the functioning changes of the reservoir in terms of the capacity of the water mass occurred under the influence of both natural and anthropogenic factors. It was determined that the creation of this natural-technical water object activated two geological processes in its shore zone - abrasion and induced seismicity. It was stated that the especially large transformations of the reservoir shore zone by these dangerous processes occurred in the first years of its intensive exploitation, in the period of small water resources in the drainage basin of Yenisei - Angara, which forced specific conditions of reservoir functioning. At rocky shores the predominating process is abrasion of their waterside parts, whereas at shores built of loose deposits the complete transformation of underwater parts of shallows takes place.
Alina Chicoș, Alina Huzui-Stoiculescu and Georgiana Toth
Paper No. 4, Stockholm Environment Institute, Oxford
Freedy J., Hobfoll S., Ribbe D. (1994), Life events, war and adjustment: Lessons for the middle east , Anxiety, Stress and Coping Review 7: 191-203
Georgescu E. S. et al. (2012), Istoria şi specificul riscului seismic în Bucureşti , Lucrările celei de-a VII-a ediţii a Conferinţei anuale a ASTR, București
Giddens A. (1999), Risk and responsibility , Modern law review 62(1):1–10
Guvernul României , Hotărâre nr. 548/2008 privind aprobarea Strategiei naționale de comunicare si informare
Gheorghe Romanescu, Alin Mihu-Pintilie and Donatella Carboni
from the seismic data. Marine Geology, 157, p. 249–265.
Dolukhanov P.M., Arslanov K.A., (2009), Ecological crises and early human migrations in the Black Sea. Quaternary International, 197, p. 35–42.
Dolukhanov P.M., Kadurin S.V., Larchenkov P., (2009), Dynamics of the coastal North Black sea area in Late Pleistocene and Holocene and Early Human Dispersal. Quaternary International, 197, p. 27–34.
Faraci G., (2016) Ensuring the Conservative Process: The Roman Walls of Lugo Maintenance Plan. Conservation and Management of Archaeological