PDF Aegean and Black Sea 2006 Expedition Plate Tectonics - A Haiku Deck by Julia Wilson Greece is located in an area of the world where there are multiple plate boundaries, sitting in between Europe and Asia. Provide each student or student group with a This 1,500-km-long, right-lateral strike-slip fault, which extends from the Karliova triple junction in eastern Turkey westward across northern Turkey and into the Aegean Sea, forms the boundary between the Eurasian plate to the north and the Anatolian plate to the south (Barka, 1992). Volcanic Eruption. Plate Tectonics Movements. The tectonic setting in the Aegean Sea is rare due to the several processes that are constantly in motion. Movement of the plates causes huge stresses, breaks portions of the rock, and produces earthquakes. The northern part of Greece lies on the Eurasian Plate while the southern part lies on the Aegean Sea Plate. Obviously, plate motions did not start just in this century. To estimate the tectonic regime, 7-year primary raw geodetic datasets are implemented, deriving from 32 permanent GPS/GNSS stations. The boundaries of the Anatolian/Aegean Plates are characterized by large strain rates due to rapid W-SW oriented movement that reaches 35 mm/y. At the eastern end of the Turkish plate the motion is taken up by thrust . What plate boundary is Santorini volcano on? - Answers At the same time extensional tectonics were also present further to the east, namely the Aegean Sea and the Pannonian basin. . Are earthquakes common in Crete? - Colors-NewYork.com Geodetic analysis of the tectonic crustal deformation ... The Mediterranean is characterized by complex tectonics related to the interaction of three main lithospheric plates (Nubia, Eurasia and Arabia) and a number of small sub-plates and crustal blocks (e.g., Alboran, Hyblean-Malta, Aegean, Anatolia and Sinai). The main objective of the research was to quantify the building stock's vulnerability to tsunami hazard. Earth and Planetary Science Letters, 96 (1990) 393-406 Elsevier Science Publishers B.V., Amsterdam - Printed in The Netherlands [CH] Present-day kinematics of the plate boundary zone between Africa and Europe, from the Azores to the Aegean Rob Westaway Department of Geological Sciences, University of Durham, South Road Durham DHI 3LE, (UK) Received March 7, 1989; revised version accepted . launchpad keyboard shortcut windows. Eurasian Plate: Tectonic Boundary and Movement. Some Famous Transform Boundaries In The World You Should ... View the full answer. Basins, the Alboran Sea, Liguro-Provencal basin and the Tyrrhenian Sea (Figure 1). J. Tuzo Wilson had identified three basic elements of geodynamics: plate tectonics, mantle plumes of deep origin, and the Wilson Cycle of ocean opening and closing, which provides evidence of plate tectonic behavior in times before quantifiable . Seismic imaging of the interplate boundary and deformation within the overriding Aegean lithosphere Lead PI: Dr. Anne Becel. Aegean Sea - Geography Lori Dengler: Complications in a plate boundary - Times ... This microplate is bordered by an orogenic belt, the peri-Adriatic mountain chain that runs through Italy and Greece, in the region surrounding the Adriatic Sea (Channell and . This transform plate boundary lies between the Eurasian and Anatolian plate boundaries. (Orogen boundaries omitted.) In Chapter 2, I investigate the nature/type of the plate boundary between the eastern Aegean region and the Africa plate. The magnitude 7.0 temblor occurred in an area of complex geologic movement, where multiple tectonic plates crack the . 9. The Cyclades island group lies within a zone of extensional tectonics in the Aegean Sea Plate, between the South Aegean Volcanic Arc to the south and the continuation of the North Anatolian Fault to the north. INTRODUCTION New geodetic instrumentation and improved spaceborne measuring 10 . 5.2 Earthquake Strikes East of Crete on Sunday ACTIVE TECTONICS OF THE AEGEAN REGION. The Hellenic Subduction zone has a complex lithospheric structure and shows complex . The plate is moving south westward at a speed of 37mm per year relative to the African Plate. At the Hellenic trench south of the Aegean Sea, the eastern Mediterranean lithosphere (frontal part of the African plate) subducts with a velocity of ∼4 cm/ yr and a mean dip angle of 25 . At subduction zones, the more dense plate, usually the oceanic plate, subducts under the less dense plate. The Hellenic Subduction zone has a complex lithospheric structure and shows complex . The Hellenic Subduction zone, which has high seismicity, is the main tectonic feature of the eastern Mediterranean Sea related to the subduction of the African Plate beneath the Aegean Sea Plate. Its southern edge is a subduction zone south of Crete, where the African Plate is being swept under the Aegean Sea Plate. Western Anatolia has been formed by the motions of the African plate, Arabian plate and Hellenic Subduction zone. Adriatic Plate. The Cretan Trough is a depression between Crete subject reaching a depth of about 2000 m. The most interesting feature of the northern Aegean is the northern . Three main types of plate boundaries: Divergent: extensional; the plates move apart. The combination of this motion in the north with the local obstruction of the rotation near Rhodes, must create a torque and a new pattern of rotation for the western part of the plate complex . place where two plates converge (collide) 9. aegean sea plate volcanic arc. 7000 inhabitants) Greece and Turkey earthquake driven by wild tectonics of the Aegean Sea Maya Wei-Haas 10/30/2020. The boundary between the Aegean and Turkish plates forms a north-south belt of seismicity across western Turkey and the eastern Aegean. The plate shares a boundary with the Eurasian Plate, the African Plate, the Arabian Plate and the Aegean Sea Plate. . In addition to the 14 large plates whose motion was described by the . Mediterranean region. The Aegean Sea Plate (also called the Hellenic Plate or Aegean Plate) is a small tectonic plate located in the eastern Mediterranean Sea under southern Greece and far western Turkey.Its southern edge is a subduction zone south of Crete, where the African Plate is being swept under the Aegean Sea Plate. The two cross-hatched regions are the Alps and Persia-Tibet-Burma orogens in the west and east, respectively. The African Plate subducts beneath the southern edge of Aegean Plate at the Hellenic Trench. Considering the history of tsunamis in the Aegean Sea, an extreme sea-level rise after a 10 m a.s.l. information on the overall geometry of the plate boundary including the thickness of sediment subducting along the plate boundary, interplate . The Adriatic plate, also known as the Apulian plate, is situated in the deformation zone at the boundary between the Eurasian and the African plates. Panama Plate, Aegean Sea Plate, Iranian Plate, Okinawa Plate, Timor Plate, Sri Lanka Plate, Greenland Plate, Easter Plate, Solomon Sea Plate and North Andes Plate among others. Aegean Sea AS AT Anatolia BU Burma NB Manus (MN) Juan de Fuca JF North America (NA) Caribbean (CA) Cocos (CO) Rivera RI Galápagos (GP) North Andes ND PA Panama Nazca (NZ) Easter EA Juan FernandezJZ The Aegean Sea Plate (also called the Hellenic Plate or Aegean Plate) is a small tectonic plate located in the eastern Mediterranean Sea under southern Greece and far western Turkey.Its southern edge is a subduction zone south of Crete, where the African Plate is being swept under the Aegean Sea Plate. Where tectonic plates are moving apart, they form a divergent plate boundary. The propagation of the NAF and extension in the Corinth Rift suggest a strongly localising rheology whereas the formation of MCC in the Cyclades and the Rhodope suggests instead a more viscous behaviour. ACTIVE TECTONICS OF THE EASTERN MEDITERRANEAN REGION The tectonic framework of the eastern Mediterranean and Middle East region is dominated by the collision of the Arabian and African plates with Eurasia (e.g., McKenzie, 1970; Jackson and McKenzie, 1988). Transcribed image text: What is the opposing plate involved in the formation of the volcanoes of the Aegean Sea? Plate boundaries are commonly associ-ated with geological events such as earthquakes and . This will cause earthquakes. transform plate boundary. The Aegean Sea Plate (also called the Hellenic Plate or Aegean Plate) is a small tectonic plate located in the eastern Mediterranean Sea under southern Greece and far western Turkey. Santorini, or officially called Thira, consists actually of a group of islands: - The main island Thera (75,8 km 2, ca. The common onset of extension in various smaller-scale domains around 30 Ma might be related to a slow down of absolute African plate For this purpose, a "worst-case run-up scenario" was developed. The latest earthquake struck roughly 13 miles beneath the Aegean seafloor, some nine miles off the shore of Samos. The Hellenic arc parallels the subduction zone at a distance of about 120 km to the north, and contains several active volcanic centers (Methana, Santorini, Nisyros, the Bodrum Peninsula). Our model covers the Eurasia-Africa plate boundary region from the Azores to the eastern Mediterranean Sea. The Aegean Sea Plate (also called the Hellenic Plate or Aegean Plate) is a small tectonic plate located in the eastern Mediterranean Sea under southern Greece and far western Turkey.Its southern edge is a subduction zone south of Crete, where the African Plate is being swept under the Aegean Sea Plate. The plate boundary segments of the three arcs where slab continuity is possibly maintained are indicated in Fig. What plate boundaries are in Greece? The Aegean Sea Plate (also called the Hellenic Plate or Aegean Plate) is a small tectonic plate located in the eastern Mediterranean Sea under southern Greece and far western Turkey.Its southern edge is a subduction zone south of Crete, where the African Plate is being swept under the Aegean Sea Plate. On the other side of the Anatolian-Aegean plate complex, relatively free motion occurs along the North Anatolian fault zone including in the Aegean Sea. This complex tectonic context exposes a wide spectrum of inter-related geodynamic processes such as subduction (e.g., Calabrian Arc . The Aegean Sea Plate is moving southwestward with respect to the Eurasian Plate at about 30 mm/yr while the African Plate is subducting northwards beneath the Aegean Sea Plate at a rate of about 40 mm/yr. 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