Academic literature on the topic 'Anatolian Plateau'

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Journal articles on the topic "Anatolian Plateau"

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Özdoğan, Mehmet. "Amidst Mesopotamia-centric and Euro-centric approaches: the changing role of the Anatolian peninsula between the East and the West." Anatolian Studies 57 (December 2007): 17–24. http://dx.doi.org/10.1017/s0066154600008462.

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AbstractDue to its geographical position, the Anatolian plateau has always been considered as a bridge in transmitting cultural formations that originated in the Near East to southeastern Europe and to the Aegean. Such a standpoint downgrades the role played by the Anatolian plateau to a transit route between the East and the West, overlooking its distinct structure. It seems that the main bias is in considering the Anatolian plateau as a single cultural unit, ignoring the multifarious nature of its structure. The role the Anatolian plateau played between the ‘East’ and the ‘West’ was much mor
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Steadman, Sharon R., Gregory McMahon, Benjamin S. Arbuckle, et al. "Stability and change at Çadır Höyük in central Anatolia: a case of Late Chalcolithic globalisation?" Anatolian Studies 69 (2019): 21–57. http://dx.doi.org/10.1017/s0066154619000036.

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AbstractScholars have recently investigated the efficacy of applying globalisation models to ancient cultures such as the fourth-millennium BC Mesopotamian Uruk system. Embedded within globalisation models is the ‘complex connectivity‘ that brings disparate regions together into a singular world. In the fourth millennium BC, the site of Çadır Höyük on the north-central Anatolian plateau experienced dramatic changes in its material culture and architectural assemblages, which in turn reflect new socio-economic, sociopolitical and ritual patterns at this rural agro-pastoral settlement. This stud
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Bikoulis, Peter. "Revisiting prehistoric sites in the Göksu valley: a GIS and social network approach." Anatolian Studies 62 (November 13, 2012): 35–59. http://dx.doi.org/10.1017/s0066154612000026.

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AbstractUsing a variety of quantitative approaches, interactions between prehistoric sites in the Göksu valley and south-central Anatolia are modelled within their wider multi-regional and diachronic socio-economic networks to assess the prominence and influence of communities in south-central Anatolia from the Late Chalcolithic to the end of the Early Bronze Age (c. 4200–2000 BC). Since the 1950s, some have understood the valley as significant in terms of movement and communication through the Taurus mountain chain that divides the southern Anatolian plateau from the Mediterranean coast. This
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Summers, Geoffrey D. "The Median Empire reconsidered: a view from Kerkenes Dağ." Anatolian Studies 50 (December 2000): 55–74. http://dx.doi.org/10.2307/3643014.

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SummaryThe city on the Kerkenes Dağ in central Anatolia is the largest pre-Hellenistic urban centre on the plateau (figs 1–2). It has plausibly been identified with a city of the Medes, called Pteria by Herodotus (1.76). If the identification is accepted, the city represents an expansion and imposition of Iranian power over the northern part of the central plateau. Kerkenes might thus provide evidence concerning the first sustained cultural, political and military contact between an Iranian imperial regime and Anatolian powers. Unique circumstances and developing technologies are providing an
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Brocard, Gilles Y., Maud J. M. Meijers, Michael A. Cosca, et al. "Fast Pliocene integration of the Central Anatolian Plateau drainage: Evidence, processes, and driving forces." Geosphere 17, no. 3 (2021): 739–65. http://dx.doi.org/10.1130/ges02247.1.

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Abstract Continental sedimentation was widespread across the Central Anatolian Plateau in Miocene–Pliocene time, during the early stages of plateau uplift. Today, however, most sediment produced on the plateau is dispersed by a well-integrated drainage and released into surrounding marine depocenters. Residual long-term (106–107 yr) sediment storage on the plateau is now restricted to a few closed catchments. Lacustrine sedimentation was widespread in the Miocene–Pliocene depocenters. Today, it is also restricted to the residual closed catchments. The present-day association of closed catchmen
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Erpehlivan, Hüseyin. "Anatolian-Persian grave stelae from Bozüyük in Phrygia: a contribution to understanding Persian presence and organisation in the region." Anatolian Studies 71 (2021): 59–74. http://dx.doi.org/10.1017/s0066154621000053.

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AbstractThis paper provides an assessment of four grave stelae that were found recently in the area surrounding Bozüyük, on the Anatolian plateau in the south of the Bilecik province. The plateau was part of the core of the kingdom of Phrygia during the Early and Middle Iron Ages, and part of the satrapy of Phrygia during the Achaemenid period of the Late Iron Age in Anatolia. The main focus is to examine the place of such stelae among Anatolian-Persian examples and to explore elements of Persian presence and organisation in the region. The precise archaeological contexts of these stelae are u
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Baird, Douglas, Andrew Fairbairn, Emma Jenkins, et al. "Agricultural origins on the Anatolian plateau." Proceedings of the National Academy of Sciences 115, no. 14 (2018): E3077—E3086. http://dx.doi.org/10.1073/pnas.1800163115.

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This paper explores the explanations for, and consequences of, the early appearance of food production outside the Fertile Crescent of Southwest Asia, where it originated in the 10th/9th millennia cal BC. We present evidence that cultivation appeared in Central Anatolia through adoption by indigenous foragers in the mid ninth millennium cal BC, but also demonstrate that uptake was not uniform, and that some communities chose to actively disregard cultivation. Adoption of cultivation was accompanied by experimentation with sheep/goat herding in a system of low-level food production that was int
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ŞIRIN, DENIZ, MEHMET SAIT TAYLAN, RIFAT BIRCAN, GÜRKAN AKYILDIZ, and LEVENT CAN. "Phylogenetic and phylogeographic analysis of Myrmeleotettix maculatus (Orthoptera: Acrididae: Gomphocerinae) species group in Anatolia." Zootaxa 4949, no. 1 (2021): 149–62. http://dx.doi.org/10.11646/zootaxa.4949.1.8.

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Six Anatolian and one European populations of the Myrmeleotettix maculatus species group, which contains M. maculatus and M. ethicus species, have been studied by using molecular genetics methods with mitochondrial COI gene. Myrmeleotettix ethicus is an Anatolian endemic species with local distribution whereas M. maculatus is distributed in western Palearctic. The phylogenetic analysis (ML and BI analyses) of the M. maculatus species group in Anatolia reveals that it consistently recovered two well-supported main clades and four different lineages. Molecular time estimates suggest that the div
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Massa, Michele, Orlene McIlfatrick, and Erkan Fidan. "Patterns of metal procurement, manufacture and exchange in Early Bronze Age northwestern Anatolia: Demircihüyük and beyond." Anatolian Studies 67 (2017): 51–83. http://dx.doi.org/10.1017/s0066154617000084.

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AbstractThis paper adds a new interpretive layer to the already extremely well-investigated site of Demircihüyük, a small Early Bronze Age settlement at the northwestern fringes of the central Anatolian plateau. It presents a reassessment of the evidence for prehistoric mining in the region, as well as a new programme of chemical composition analysis integrated with an object functional and technological typology of the site's metal assemblages. The results reveal complex manufacturing techniques (such as bivalve mould casting, plating and lost wax) and the co-occurrence of several alloying ty
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Özsayin, Erman, and Kadir Dirik. "The role of oroclinal bending in the structural evolution of the Central Anatolian Plateau: evidence of a regional changeover from shortening to extension." Geologica Carpathica 62, no. 4 (2011): 345–59. http://dx.doi.org/10.2478/v10096-011-0026-7.

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The role of oroclinal bending in the structural evolution of the Central Anatolian Plateau: evidence of a regional changeover from shortening to extensionThe NW-SE striking extensional Inönü-Eskişehir Fault System is one of the most important active shear zones in Central Anatolia. This shear zone is comprised of semi-independent fault segments that constitute an integral array of crustal-scale faults that transverse the interior of the Anatolian plateau region. The WNW striking Eskişehir Fault Zone constitutes the western to central part of the system. Toward the southeast, this system splays
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Dissertations / Theses on the topic "Anatolian Plateau"

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Radeff, Giuditta. "Geohistory of the Central Anatolian Plateau southern margin (southern Turkey)." Phd thesis, Universität Potsdam, 2014. http://opus.kobv.de/ubp/volltexte/2014/7186/.

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The Adana Basin of southern Turkey, situated at the SE margin of the Central Anatolian Plateau is ideally located to record Neogene topographic and tectonic changes in the easternmost Mediterranean realm. Using industry seismic reflection data we correlate 34 seismic profiles with corresponding exposed units in the Adana Basin. The time-depth conversion of the interpreted seismic profiles allows us to reconstruct the subsidence curve of the Adana Basin and to outline the occurrence of a major increase in both subsidence and sedimentation rates at 5.45 – 5.33 Ma, leading to the deposition of al
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Radeff, Giuditta [Verfasser], and Domenico [Akademischer Betreuer] Cosentino. "Geohistory of the Central Anatolian Plateau southern margin (southern Turkey) / Giuditta Radeff. Betreuer: Domenico Cosentino." Potsdam : Universitätsbibliothek der Universität Potsdam, 2014. http://d-nb.info/1058741004/34.

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Albino, Irene <1985&gt. "Thermochronological evolution of the Eastern Pontides and the Eastern Anatolian Plateau and NW Lesser Caucasus (Turkey, Georgia, Armenia)." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2013. http://amsdottorato.unibo.it/5505/.

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The analysis of apatite fission tracks is applied to the study of the syn- and post-collisional thermochronological evolution of a vast area that includes the Eastern Pontides, their continuation in the Lesser Caucasus of Georgia (Adjara-Trialeti zone) and northern Armenia, and the eastern Anatolian Plateau. The resulting database is then integrated with the data presented by Okay et al. (2010) for the Bitlis Pütürge Massif, i.e. the western portion of the Bitlis-Zagros collision zone between Arabia and Eurasia. The mid-Miocene exhumation episode along the Black Sea coast and Lesser Caucasus o
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Biltekin, Demet. "Vegetation and climate of north anatolian and north aegean region since 7 Ma according to pollen analysis." Phd thesis, Université Claude Bernard - Lyon I, 2010. http://tel.archives-ouvertes.fr/tel-00720892.

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This study concerns a long marine section (DSDP Site 380: Late Miocene to Present) and onshore exposed sections from the Late Miocene and/or Early Pliocene. The main target of this study is to reconstruct vegetation and climate in the North Anatolia and North Aegean region for the last 7 Ma. Two vegetation types were alternately dominant: thermophilous forests and open vegetations including Artemisia steppes. During the Late Miocene, most of the tropical and subtropical plants declined because of the climatic deterioration. However, some of them survived during the Late Pliocene, such as those
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Dogan, Guray. "Comparison Of The Rural Atmosphere Aerosol Compositions At Different Parts Of Turkey." Master's thesis, METU, 2005. http://etd.lib.metu.edu.tr/upload/12605844/index.pdf.

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Long term data generated at four rural stations are compared to determine similarities and differences in aerosol compositions and factors contributing to observed differences at different regions in Turkey. The stations used in this study are located at Mediterranean coast (20 km to the west of Antalya city), Black Sea coast (20 km to the east of Amasra town), Central Anatolia (&Ccedil<br>ubuk, Ankara) and Northeastern part of the Anatolian Plateau (at Mt. Uludag). Data used in comparisons were generated in previous studies. However, some re-analysis of data were also performed<br>(1) to imp
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Tatar, Orhan. "Neotectonic structures in the east central part of the North Anatolian Fault Zone, Turkey." Thesis, Keele University, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.283263.

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Crespin, Anne-Sophie Pelon Olivier. "Le plateau anatolien de la fin de l'empire hittite aux invasions cimmeriennes, XIIe-VIIe siècle avant J.-C." [S.l.] : [s.n.], 2001. http://demeter.univ-lyon2.fr/sdx/theses/lyon2/2001/crespin_as.

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Crespin, Anne-Sophie. "Le plateau anatolien de la fin de l'empire hittite aux invasions cimmeriennes, XIIe-VIIe siècle avant J. -C." Lyon 2, 2001. http://theses.univ-lyon2.fr/documents/lyon2/2001/crespin_as.

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Pour aborder les problèmes de la transition entre l'âge du Bronze et celui du Fer et de l'apparition ensuite de nouvelles entités politiques sur le plateau anatolien, nous avons fait en premier lieu une présentation de la géographie de la région. Le second chapitre traite de l'historique des recherches sur le sujet avant et après la seconde guerre mondiale. Un sous chapitre est consacré à la présentation des dernières données. Les sources écrites classiques, égyptiennes, assyriennes, bibliques, cunéiformes et hiéroglyphiques et phrygiennes ont fourni des renseignements provenant de secteurs gé
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Biryol, Cemal Berk. "COMPLEX RUPTURE PROCESSES OF THE SOLOMON ISLANDS SUBDUCTION ZONE EARTHQUAKE AND SUBDUCTION CONTROLLED UPPER MANTLE STRUCTURE BENEATH ANATOLIA." Diss., The University of Arizona, 2009. http://hdl.handle.net/10150/194681.

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This dissertation explores subduction zone-related deformation both on short time scales in the form of subduction zone earthquakes and over larger time and geographical scales in the form of subduction rollback or detachment of the subducting lithosphere. The study presented here is composed of two parts. First, we analyzed the source-rupture processes of the April 1, 2007 Solomon Islands Earthquake (Mw=8.1) using a body-wave inversion technique. Our analysis indicated that the earthquake ruptured approximately 240 km of the southeast Pacific subduction zone in two sub-events.In the second pa
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Delph, Jonathan, and Jonathan Delph. "Crustal and Upper Mantle Structure of the Anatolian Plate: Imaging the Effects of Subduction Termination and Continental Collision with Seismic Techniques." Diss., The University of Arizona, 2016. http://hdl.handle.net/10150/622908.

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The neotectonic evolution of the eastern Mediterranean is intimately tied to interactions between the underthrusting/subducting slab along the southern margin of Anatolia and the overriding plate. The lateral variations in the subduction zone can be viewed as a temporal analogue of the transition between continuous subduction and subduction termination by continent-continent collision. By investigating the lateral variations along this subduction zone in the overriding plate, we can gain insight into the processes that precede continent collision. This dissertation summarizes the results of th
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Books on the topic "Anatolian Plateau"

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Koromila, Marianna. Pontos-Anatolia: Northern Asia Minor and the Anatolian plateau east of the Upper Euphrates : images of a journey. Lucy Braggiotti, 1989.

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D'agostino, Anacleto, Valentina Orsi, and Giulia Torri, eds. Sacred Landscapes of Hittites and Luwians. Firenze University Press, 2016. http://dx.doi.org/10.36253/978-88-6655-904-7.

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This book contains studies on the symbolic significance of the landscape for the communities inhabiting the central Anatolian plateau and the Upper Euphrates and Tigris valleys in the 2nd-1st millennia BC. Some of the scholars who attended to the international conference Sacred Landscapes of Hittites and Luwians held in Florence in February 2014, present here contributions on the religious, symbolic and social landscapes of Anatolia between the Late Bronze Age and Iron Age. Archaeologists, hittitologists and historians highlight how the ancient populations perceived many elements of the enviro
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The development and traditions of pottery in the Neolithic of the Anatolian plateau: Evidence from Çatalhöyük, Süberde and Erbaba. Archaeopress, 2012.

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Mazzoni, Stefania, and Franca Pecchioli, eds. The Uşaklı Höyük Survey Project (2008-2012). Firenze University Press, 2016. http://dx.doi.org/10.36253/978-88-6655-902-3.

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This book presents the results of the survey conducted by the University of Florence, in the years 2008-2012, at the site and in the surrounding territory of U&amp;#351;akl&amp;#305; Höyük on the central Anatolian plateau in Turkey. Geological, geomorphological, topographic and geophysical research have provided new information and data relating to the environment and the settlement landscape, as well as producing new maps of the area and indicating the presence of large buried buildings on the site. Analysis of the rich corpus of pottery collected from the surface indicates that the site and
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Schoop, Ulf-Dietrich. The Chalcolithic on the Plateau. Edited by Gregory McMahon and Sharon Steadman. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780195376142.013.0007.

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This article outlines the present state of knowledge about the Chalcolithic sequence on the Anatolian plateau and in western Anatolia. Because archaeological knowledge is not represented continuously over the whole area, it will be treated in the context of seven larger regions: the central Anatolian Plain (including Cappadocia, with occasional references to Cilicia), the southwest Anatolian Lake District (a mountainous region around the city of Burdur), the Aegean coast (extending north into the Troad), the area around the Sea of Marmara, the Porsuk region (around the city of Eskişehir), the
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Seeher, Jürgen. The Plateau: The Hittites. Edited by Gregory McMahon and Sharon Steadman. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780195376142.013.0016.

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This article presents data on the Hittites, who, during the second millennium BCE, established the first empire in what was later called Anatolia and then Asia Minor. From the beginning, the Hittite kings followed an active settlement policy on the Anatolian plateau. Sites in disparate areas show a remarkable uniformity in architecture and material culture, and thus document a strong system, with well-organized structures of production and distribution. Basically inland oriented, the Hittite state maintained close connections to the coast only in southern Asia Minor, which meant access to the
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Kealhofer, Lisa, and Peter Grave. The Iron Age on the Central Anatolian Plateau. Edited by Gregory McMahon and Sharon Steadman. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780195376142.013.0018.

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This article presents data on the Iron Age of central Anatolia. After describing the geographical context of the Anatolian plateau, it outlines advances and constraints in the development of a regional chronological framework. The current understanding of the Iron Age is then explored based on recent excavations of Iron Age levels at four sites: Gordion, Boğazköy, Kaman–Kalehöyük, and Çadır Höyük. Recent work at Kerkenes Dağ and Dorylaion/Eskişehir, as well as regional surveys, provide some additional shape to this still-fragmentary picture. The evidence from the sites suggests occupational co
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Özbaşaran, Mihriban. The Neolithic on the Plateau. Edited by Gregory McMahon and Sharon Steadman. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780195376142.013.0005.

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This article compiles data on the ninth-to-sixth-millennium-BCE communities of the central Anatolian plateau, underscoring the distinctive features of each of them in chronological order and deliberately avoiding the traditional phase terminology of the Neolithic. The data presently display local adaptations of central Anatolian Neolithic communities to their diverse habitats. In the ninth and early eighth millennia BCE, sedentism and a heavy reliance on naturally occurring resources constituted the way of life on the plateau. Full farming villages developed toward the second half of the eight
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1952-, Hopkins David C., ed. Across the Anatolian plateau: Readings in the archaeology of ancient Turkey. American Schools of Oriental Research, 2002.

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Steadman, Sharon. The Early Bronze Age on the Plateau. Edited by Gregory McMahon and Sharon Steadman. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780195376142.013.0010.

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This article presents data on the Early Bronze Age (EBA) of the Anatolian plateau. The EBA on the plateau has been identified as a period of “urbanization,” or at least the age in which complex society emerged, including the rise of an extensive trade network, established by the second half of the third millennium BCE. Chalcolithic period interregional trade with regions as far afield as Transcaucasia and possibly southeastern Europe was strengthened by connections ranging across the plateau, stretching into the Aegean, and southeastward to northern Mesopotamia and beyond. Monumental architect
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Book chapters on the topic "Anatolian Plateau"

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Bachhuber, Christoph. "The Anatolian Plateau." In A Companion to the Archaeology of the Ancient Near East. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781444360790.ch30.

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Baird, Douglas. "The Late Epipaleolithic, Neolithic, and Chalcolithic of the Anatolian Plateau, 13,000-4000 BC." In A Companion to the Archaeology of the Ancient Near East. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781444360790.ch23.

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Şaroğlu, Fuat, and Yıldırım Güngör. "Fairyland in the Erzurum High Plateau, Eastern Anatolia." In World Geomorphological Landscapes. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-03515-0_25.

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Palermo, Rocco. "From the Anatolian plateau to the steppe." In On the Edge of Empires. Routledge, 2019. http://dx.doi.org/10.4324/9781315648255-2.

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Howard-Johnston, James. "Climax of the War." In The Last Great War of Antiquity. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780198830191.003.0009.

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The initiative swung back to the Persians in 626. Two Persian armies attacked, Shahrbaraz driving Heraclius from Lake Van back to the Anatolian plateau, Shahen advancing across Transcaucasia. Shahrbaraz pressed on to the Bosporus, for a planned joint attack with the Avars on Constantinople. In the event, the Persian contingent was intercepted on the Bosporus, which left siege operations entirely in Avar hands. The huge host which they had assembled assaulted the city for ten days (29 July–7 August), deploying a full array of siege engines by land and Slav naval forces on the Golden Horn, but they could not breach the defences and withdrew on 8 August. Meanwhile, the Turks had invaded the Persian north-west across the Caucasus, and Heraclius, who had veered north on reaching Anatolia, had intercepted and destroyed Shahen’s army.
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Barazangi, Muawia, Eric Sandvol, and Doğan Seber. "Structure and tectonic evolution of the Anatolian plateau in eastern Turkey." In Postcollisional Tectonics and Magmatism in the Mediterranean Region and Asia. Geological Society of America, 2006. http://dx.doi.org/10.1130/2006.2409(22).

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Barker, Graeme. "The ‘Hearth of Domestication’? Transitions to Farming in South-West Asia." In The Agricultural Revolution in Prehistory. Oxford University Press, 2006. http://dx.doi.org/10.1093/oso/9780199281091.003.0009.

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The principal focus of this chapter is the classic zone of early farming research from the 1960s onwards, the so-called ‘hilly flanks of the Fertile Crescent’ in South-West Asia (Fig. 4.1). This region is normally defined as the arc of hill country to the west of the Syrian desert and to the north and east of the Tigris and Euphrates valleys. The western side of the arc begins east of the Nile in the Sinai and the Gulf of Arabah on the southern border of Israel and Jordan; it continues northwards as the hill country on either side of the Jordan rift valley in Israel, Palestine, Lebanon, western Jordan, and western Syria (the so-called ‘Levantine corridor’); and extends westwards to the Mediterranean littoral. The northern sector is formed by the Taurus mountains along the southern edge of the Anatolian plateau, which curve eastwards from the Mediterranean coast in northern Syria to form the present-day Syrian–Turkish border. The eastern sector consists of the Zagros mountains, running south-eastwards from eastern Turkey and north-west Iran to the Persian Gulf, forming the Iraq–Iran border for most of their length, and continuing in south-west Iran beyond the Persian Gulf towards the Straits of Hormuz. The region also embraces adjacent zones: the alluvial plains of the Tigris and Euphrates rivers and the vast tracts of steppe and desert country separating them from the Levantine, Taurus, and Zagros upland systems; the Anatolian plateau to the north of the Taurus, within modern Turkey; and the Iranian plateau east of the Zagros, within modern Iran. The archaeological literature commonly uses the term Near East to describe the main region of interest, with the Levant for its western side (a term also used in this chapter), and South-West Asia for the eastern side, but the entire region is more correctly termed South-West Asia. The upland areas of the region mostly receive more than 200 millimetres of rainfall a year, which is the minimum required for growing cereals without irrigation. Rainfall decreases drastically moving out into the steppe and desert zones.
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Wainwright, John. "Weathering, Soils, and Slope Processes." In The Physical Geography of the Mediterranean. Oxford University Press, 2009. http://dx.doi.org/10.1093/oso/9780199268030.003.0018.

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Hillslopes are the dominant landform features of the Earth’s surface. They make up the interface between the atmosphere and Earth systems, providing a substrate that supports life and thus the basis for human activities within the Mediterranean. Their location at this interface means that hillslopes evolve through a complex interaction of different processes, operating at a range of different time and spatial scales. At longer timescales, processes of weathering convert rock and other parent materials into soils. Soils allow the growth of vegetation and thus further feedbacks between atmospheric and surface processes; in some cases these feedbacks can be seen to provide relative stability, while in others the system can become more fragile (Chapter 20). The latter case often arises as a result of erosion processes of various types. Water erosion and mass movements are a significant element of Mediterranean landscape evolution, occurring in parallel with (in response to, and affecting) tectonic processes that have moulded the configuration of the Earth’s crust (see Chapter 1), producing the unique combination of environmental characteristics of the region. Since the Late Pleistocene, depending on location, human activity has led to an acceleration of many of these processes, with important consequences for the basic ‘life-support system’ of the region and for global environmental cycles. The in situ modification of near-surface materials is typically considered to take place along a continuum relating to the dominance of mechanical or chemical processes (e.g. Birkeland 1999). The simplest control may be considered to be climatic, with mechanical breakdown of particles dominating in cold, dry conditions, and chemical processes dominating in warm, wet conditions. Comparing this model to the present day climate of the Mediterranean suggests, as with other processes, something of a north–south divide in terms of the dominant weathering process. The northern part of the basin (together with the Levant and the north-facing uplands of the Maghreb) would seem to be dominated by moderate chemical weathering; exceptions being the arid areas of south-east Spain, southern Sicily, eastern Cyprus, and parts of the Anatolian plateau as well as areas where low average temperatures would also reduce rates, such as in the Alps and parts of Slovenia and Croatia.
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"Patterns of Armeno-Muslim Interchange on the Armenian Plateau in the Interstice between Byzantine and Ottoman Hegemony." In Islam and Christianity in Medieval Anatolia. Routledge, 2016. http://dx.doi.org/10.4324/9781315589886-11.

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10

Roberts, Neil, and Jane Reed. "Lakes, Wetlands, and Holocene Environmental Change." In The Physical Geography of the Mediterranean. Oxford University Press, 2009. http://dx.doi.org/10.1093/oso/9780199268030.003.0021.

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The Mediterranean regions of the world are defined on the basis of their climate, with a distinct hot, dry summer season and a warm, wet winter (Grove and Rackham 2001; Chapter 3). Spring and autumn seasons are less well defined but often contribute significantly to annual precipitation. Strictly defined in this way, the Mediterranean region is confined to parts of Italy, Greece, southern France, the south and east of Spain (non-Atlantic climate), the Maghreb and Cyrenaica in North Africa, and narrow coastal strips running through the Balkans, southern and western Turkey, and the Levant (Syria, Lebanon, and Israel-Palestine). Outside these areas, climate becomes humid temperate (western Europe, Black Sea), arid (Sahara, northern Arabia), or continental (interior areas of the Balkans, Turkey and Iberia, the Zagros mountains of Iran/Iraq). Even within the strict definition are found subalpine mountain zones, so it is a difficult study region to demarcate absolutely. In a similar vein to the volume by Zolitschka et al. (2000), this chapter extends the scope to important wetlands in some neighbouring regions, and deals effectively with the circum-Mediterranean. Thus, we include lakes Ohrid and Dojran in the Balkans, wetlands of the continental interior of Turkey, north-western Iran and the Caucasus (e.g. Lakes Van, Urmia, and Sevan), the climatically dry Jordan rift valley which includes the Dead Sea, and the subalpine northern Italian lakes such as Como and Maggiore. The Mediterranean basin is geologically complex and has its origin in the progressive closure of the Sea of Tethys during the Tertiary (Laubscher and Bernoulli 1977). Plate convergence between Africa and Eurasia led to a major phase of orogenesis and the creation of fold mountains including the Atlas, Sierra Nevada, Alps, Apennines, and Taurus, and to plateau uplift in Iberia and Anatolia (Chapter 1). These mountain ranges are commonly dominated by massively deformed Mesozoic limestones that now form karst landscapes (e.g. Dinaric Alps; Ager 1980; Chapter 10). Tectonic movement also led to extensive late Cenozoic volcanism, notably in southern and central Italy, the Hellenic arc, Anatolia, and around the Jordan rift (Chapter 15).
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Conference papers on the topic "Anatolian Plateau"

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Campbell, Clay, Michael H. Taylor, Faruk Ocakoğlu, Alexis Licht, Megan A. Mueller, and Andreas Möller. "DID THE CENTRAL ANATOLIAN CANKIRI BASIN FORM AS A RESULT OF AN OLIGO-MIOCENE RAYLEIGH-TAYLOR INSTABILITY? IMPLICATIONS FOR EARLY MIOCENE PLATEAU DEVELOPMENT IN CENTRAL ANATOLIA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338731.

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2

Mulch, Andreas, Maud J. M. Meijers, Maud J. M. Meijers, et al. "LATE MIOCENE TO PLIOCENE PALEOENVIRONMENT AND SURFACE UPLIFT OF THE CENTRAL ANATOLIAN PLATEAU AND ITS SOUTHERN MARGIN (TURKEY)." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300514.

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3

Zeybek, Fatih. "Innovative Construction Methods of Osmangazi Bridge." In IABSE Symposium, Guimarães 2019: Towards a Resilient Built Environment Risk and Asset Management. International Association for Bridge and Structural Engineering (IABSE), 2019. http://dx.doi.org/10.2749/guimaraes.2019.0912.

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&lt;p&gt;Construction period of Osmangazi Bridge was around 39 months and a short period for a large multi span bridge in a marine environment.&lt;/p&gt;&lt;p&gt;The Osmangazi Bridge is situated in a very active seismic area where in 1999 the 7.6 Kocaeli earthquake occurred on the North Anatolian Fault in 1999. Therefore, the bridge is designed to resist earthquakes. The North Anatolian fault is approximately 1600 km long major right-lateral strike slip fault forming the tectonic boundary between the Eurasian Plate and Anatolian Block of the African plate.&lt;/p&gt;&lt;p&gt;Bridge Owner requir
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Esat, Korhan, Gurol Seyitoglu, Gurol Seyitoglu, et al. "THE NW CENTRAL ANATOLIAN CONTRACTIONAL AREA: A MAJOR STRIKE-SLIP FAULT ZONES INDUCED NEOTECTONIC REGION IN THE ANATOLIAN PLATE, TURKEY." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286592.

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Faccenna, Claudio, Fabio Capitanio, Fabio Capitanio, Thorsten Becker, and Thorsten Becker. "MANTLE DYNAMICS AND PLATE BOUNDARY FORMATION: THE CASE OF THE NORTH ANATOLIAN FAULT." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-336384.

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Reports on the topic "Anatolian Plateau"

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Rodgers, A. Earthquake focal parameters and lithospheric structure of the anatolian plateau from complete regional waveform modeling. Office of Scientific and Technical Information (OSTI), 2000. http://dx.doi.org/10.2172/15006169.

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