(a) Major faults and earthquakes in the Athens region.
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Inferred faults are marked by short-dashed black lines.
It is, in central Greece, probably the dominant effect, which we illustrate in the next section, using GPS observations and a simple block model.GPS measurements, together with uplift and subsidence rates on the faults, indicate that the extension rate in the western Gulf of Corinth is almost double that in the east (Horizontal velocities of points in Greece measured by GPS, using data from Horizontal velocities of points in Greece measured by GPS, using data from It is also known that, because of the discrepancy between the roughly N-S slip vectors on normal faults in central Greece and the overall motion to the SW, the fault blocks in central Greece must rotate clockwise relative to Europe (Finally, GPS measurements show that the whole of the central Aegean Sea south of the Psara-Andros strike-slip fault (A simple block model can reconcile and illustrate these observations in central Greece ((a and b) A schematic cartoon, not drawn to scale, to illustrate how a simple model, which can be easily made with a sheet of paper, can reproduce some important features of the Aegean tectonics including: (i) strike-slip faulting which ends in a normal fault system that dies out to the west requiring clockwise rotation of the blocks to the south; (ii) the westward increase in extension within the Gulf of Corinth, required by the S. Aegean and Peloponnese moving SW as a single coherent block. Mary Goldsworthy, James Jackson, John Haines, The continuity of active fault systems in Greece, Evidence from geomorphology, the distribution of large earthquakes, and geodetic measurements suggests that the active faulting in mainland Greece and the north Aegean Sea is concentrated into a small number of discrete, linear zones that bound relatively rigid blocks.
It is clear from the geomorphology and Quaternary geology that the boundaries of the blocks have changed with time, with new faults migrating into the hanging walls of older faults and sometimes changing their orientation. (c) Topographic profile across the Volvi and Mavrouda faults. The zones are not always well defined even on land, and are clearest where the faulting produces large topographic offsets, particularly in hard footwall rocks.
As the ancient cities in the study are placed in such close proximity to the faults (directly above them), Mr Stewart believes that a relationship between the two is highly likely.Cnidus (left) and Ephesus (right) in Turkey are two more cities that are said to have been built directly above sites of earthquake activityEarly human settlers are also said to have used the underground fault lines and natural springs that erupted from the earthquakes to build cities such as Hierapolis in Turkey (pictured)The Temple, located at the ancient city of Delphi, was the most important sacred site in the Greek world.
Comments.
Το γράφηµα 11.3102 δείχνει το µέσο ποσό για τις παρατυπίες σε κάθε κράτος µέλος και τον τρόπο µε τον οποίο αυτές κατανέµονται σε σχέση µε τον γενικό µέσο όρο (οριζόντια ευθεία γραµµή).
This process is more familiar to geologists in cross-section, where domino-like arrays of normal faults can occur as sequential generations of subparallel sets (e.g. If you experience an earthquake while traveling in Greece, general earthquake safety tips still apply in the moment that the quake starts. Greece and its islands boast a high number of ancient temples and sanctuaries scattered throughout the territory, and many of the structures sit on a series of fault lines. The Stratoni fault is close to a strike-slip faulting earthquake in 1983 whose location is an offshore extrapolation of the Kavala-Xanthi fault system (It is clear that a case can be made, which we discuss later, for the major strike-slip systems of the north-central Aegean connecting to the main E-W graben systems on the east coast of Greece.
Englisch-Deutsch-Übersetzungen für fault line im Online-Wörterbuch dict.cc (Deutschwörterbuch). title: The neotectonic structure of the eastern margin of the submerged Axios-Thermaikos basin, West Chalkidiki region (C. Macedonia)(in Greek)Geologic history of the extensional basin of the Gulf of Corinth (?Miocene–Pleistocene), GreeceThe earthquake of April 30, 1954, in Sophades (Central Greece)A study of the 1980 summer seismic sequence in the Magnesia region of Central GreeceActive tectonic and sedimentary processes inwestern TurkeyNeotectonic and active faults along the Serbo-Macedonian zone (SE Chalkidiki, northern Greece)Extensional tectonics of north-west Macedonia, Greece, since the Late MioceneThe 7th September 1999, Athens, unexpected preliminary results on its seismotectonic environmentStructural characteristics of 2 strong earthquakes in the North Aegean: Ierissos (1932) and Agios Efstratios (1968)The 13 May 1995 (Kozani Grevena) earthquake; preliminary resultsSurficial sediment map of the Aegean sea floor.
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