Готові списки джерел за темами / Karsts – Aegean Sea Region

Добірка наукової літератури з теми "Karsts – Aegean Sea Region"

Автор: Grafiati

Опубліковано: 12 червня 2021

Оновлено: 1 лютого 2022

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Статті в журналах з теми "Karsts – Aegean Sea Region":

Damyanova, Evelina, and Aleksey Benderev. "Characterization of the Karst water regime in the Danube catchment area (Bulgaria)." Glasnik Srpskog geografskog drustva 96, no. 1 (2016): 11–25. http://dx.doi.org/10.2298/gsgd1601011d.

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The purpose of study is to estimate the role of karst springs in the formation of the flow of the Bulgarian rivers that are right tributaries of the Danube River. The study area includes the region from the Danube River to the main ridge of the Balkan (Stara Planina), representing a major water divide that separates the Black Sea catchment area from the Aegean one. The eastern border represents the watershed between the Danube and the Black Sea hydrological zones. From a geological point of view, the northern part of the area is located on the Moesian platform and the southern part belongs to the Fore Balkan and Balkan areas where various types of rocks of different geologic age outcrop. In some of them, there are conditions for the formation of karst water. In the northern part of the area they form distinct aquifers that gradually sink to the north; this is so called "platform" type of karst. In the southern mountainous part there are numerous karst basins. The most significant of karst springs are included in the national groundwater monitoring network. The hydrographs of karst springs are analyzed in view of the specific features of karstification. To classify the studied springs with respect to their regime, several indicators are used. Furthermore, the role of karst waters in the river runoff of the Bulgarian tributaries of the Danube River is assessed.

Papadopoulos, Vassilis P., Aristides Bartzokas, Themistoklis Chronis, Dimitris Georgopoulos, and George Ferentinos. "Factors Regulating the Air–Sea Heat Fluxes Regime over the Aegean Sea." Journal of Climate 25, no. 2 (January 15, 2012): 491–508. http://dx.doi.org/10.1175/2011jcli4197.1.

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Abstract The authors examine the impact of low-frequency atmospheric forcings on the air–sea heat fluxes over the Aegean Sea. The correlation between the air–sea heat flux components and three established [North Atlantic Oscillation (NAO), east Atlantic–western Russian pattern (EAWR), and North Sea–Caspian pattern (NCP)] and two testing climatic indices of potential effect over the eastern Mediterranean Sea region underlines significant discrepancies between the radiative (shortwave and longwave radiation) and the turbulent (sensible and latent heat) components. The NAO index affects the air–sea heat fluxes over the Aegean Sea region much less than the two innovative indices, the “Mediterranean index” and the “Eastern Europe index,” which play more effective roles. Moreover, the influence of the sea level atmospheric pressure (SLP) variability over an extended area (Europe and North Africa) on surface fluxes regime is investigated. The SLP anomalies are corroborated as a prominent regulating factor of the air–sea heat fluxes over the Aegean Sea region, especially during the cold season of the year. The analysis of the extreme values in the heat exchange anomalies for the period 1958–2001 highlights the role of SLP field on determining the air–sea heat fluxes regime, mainly during winter, when, occasionally, large amounts of heat loss from the sea surface trigger the mechanism of intermediate- and deep-water formation. It is suggested that wind regime and turbulent components are the modulators of the net air–sea heat flux anomalies throughout the year.

Seeliger, Martin, Anna Pint, Peter Frenzel, Nick Marriner, Giorgio Spada, Matteo Vacchi, Sait Başaran, et al. "Mid- to late-Holocene sea-level evolution of the northeastern Aegean sea." Holocene 31, no. 10 (June 28, 2021): 1621–34. http://dx.doi.org/10.1177/09596836211025967.

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We combined biostratigraphical analyses, archaeological surveys, and Glacial Isostatic Adjustment (GIA) models to provide new insights into the relative sea-level evolution in the northeastern Aegean Sea (eastern Mediterranean). In this area, characterized by a very complex tectonic pattern, we produced a new typology of sea-level index point, based on the foraminiferal associations found in transgressive marine facies. Our results agree with the sea-level history previously produced in this region, therefore confirming the validity of this new type of index point. The expanded dataset presented in this paper further demonstrates a continuous Holocene RSL rise in this portion of the Aegean Sea. Comparing the new RSL record with the available geophysical predictions of sea-level evolution indicates that the crustal subsidence of the Samothraki Plateau and the North Aegean Trough played a major role in controlling millennial-scale sea-level evolution in the area. This major subsidence rate needs to be taken into account in the preparation of local future scenarios of sea-level rise in the coming decades.

ZERVAKIS, V., and D. GEORGOPOULOS. "Hydrology and circulation in the North Aegean (eastern Mediterranean) throughout 1997 and 1998." Mediterranean Marine Science 3, no. 1 (June 1, 2002): 5. http://dx.doi.org/10.12681/mms.254.

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The combination of two research projects offered us the opportunity to perform a comprehensive study of the seasonal evolution of the hydrological structure and the circulation of the North Aegean Sea, at the northern extremes of the eastern Mediterranean. The combination of brackish water inflow from the Dardanelles and the sea-bottom relief dictate the significant differences between the North and South Aegean water columns. The relatively warm and highly saline South Aegean waters enter the North Aegean through the dominant cyclonic circulation of the basin. In the North Aegean, three layers of distinct water masses of very different properties are observed: The 20-50 m thick surface layer is occupied mainly by Black Sea Water, modified on its way through the Bosphorus, the Sea of Marmara and the Dardanelles. Below the surface layer there is warm and highly saline water originating in the South Aegean and the Levantine, extending down to 350-400 m depth. Below this layer, the deeper-than-400 m basins of the North Aegean contain locally formed, very dense water with different θ /S characteristics at each subbasin. The circulation is characterised by a series of permanent, semi-permanent and transient mesoscale features, overlaid on the general slow cyclonic circulation of the Aegean. The mesoscale activity, while not necessarily important in enhancing isopycnal mixing in the region, in combination with the very high stratification of the upper layers, however, increases the residence time of the water of the upper layers in the general area of the North Aegean. As a result, water having out-flowed from the Black Sea in the winter, forms a separate distinct layer in the region in spring (lying between “younger” BSW and the Levantine origin water), and is still traceable in the water column in late summer.

Jönsson, L. "SeaWiFs satellite data analysis of Black Sea water discharge pattern into the Aegean Sea." Water Science and Technology 46, no. 8 (October 1, 2002): 195–202. http://dx.doi.org/10.2166/wst.2002.0180.

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Satellite data from the SeaWiFS sensor has been used to determine chlorophyll-a contents in the North Aegean Sea using SEADAS 3.3 software. The data is used to extract knowledge on water movements/flow phenomena using chlorophyll as a “tracer” but will also indicate water quality. More than 100 SeaWiFS scenes from 1998 up to 2001 have been analyzed in terms of hydrodynamic phenomena, mainly the transport and spreading pattern of Black Sea Water in the North Aegean Sea but also concerning the water quality and its seasonal and yearly variation at the mouth region of the Dardanelles. Some comparison with earlier studies using NOAA AVHRR thermal data and historical CZCS scenes is also made.

Samanidou, Victoria F. "Conference Report: Analytical chemistry in the Aegean Sea region: current status." Bioanalysis 4, no. 24 (December 2012): 2875–76. http://dx.doi.org/10.4155/bio.12.263.

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Sakellariou, D., J. Mascle, and V. Lykousis. "Strike slip tectonics and transtensional deformation in the Aegean region and the Hellenic arc: Preliminary results." Bulletin of the Geological Society of Greece 47, no. 2 (January 24, 2017): 647. http://dx.doi.org/10.12681/bgsg.11098.

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Recently acquired offshore seismic and swath bathymetry data from the Hellenic Arc, the Ionian Sea and the South and North Aegean Sea, including the Hellenic Volcanic Arc and the Cyclades plateau, along with geological and tectonic data from Plio-Quaternary basins exposed on the Hellenic Arc indicate that strike slip tectonics has played a major role in the southwestward extension of the Aegean crustal block, the development of the offshore neotectonic basins and the spatial distribution of the volcanic activity along the Volcanic Arc. Transtensional deformation, accommodated by (sinistral or dextral) strike slip zones and related extensional structures, prevail throughout Plio-Quaternary, since the North Anatolian Fault broke westwards into the North Aegean. Incipient collision of the Hellenic Forearc south of Crete with the Libyan promontory and consequent lateral escape tectonics led to the segmentation of the Hellenic Arc in distinct blocks, which move southwestwards independently from each other and are bounded by strike slip faults.

Kourafalou, V. H., and K. Barbopoulos. "High resolution simulations on the North Aegean Sea seasonal circulation." Annales Geophysicae 21, no. 1 (January 31, 2003): 251–65. http://dx.doi.org/10.5194/angeo-21-251-2003.

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Abstract. The seasonal characteristics of the circulation in the North Aegean Sea are examined with the aid of a climatological type simulation (three-year run with perpetual year forcing) on a fine resolution grid (2.5 km by 2.5 km). The model is based on the Princeton Ocean Model with a parameterisation of plume dynamics that is employed for the input of waters with hydrographic properties that are different than the properties of basin waters, as the Black Sea Water (BSW) outflow through the Dardanelles Strait and riverine sources. The model is nested with a sequence of coarser regional and basin-wide models that provide for the long-term interaction between the study area and the Eastern Mediterranean at large. The results are employed to discuss the response of the North Aegean to the important circulation forcing mechanisms in the region, namely wind stress, heat and salt fluxes, buoyancy due to rivers and the BSW outflow (which is low in salinity and occasionally low in temperature) and the interaction with the Southern Aegean. The high resolution allows for the detailed representation of the complicated topography that presides in the region. This helps produce a rich eddy field and it allows for variability in the pathways of BSW that has implications in the basin hydrography and circulation.Key words. Oceanography: general (continental shelf processes; numerical modeling)

Poulos, Serafim E., George Ghionis, and Hampik Maroukian. "Sea-level rise trends in the Attico–Cycladic region (Aegean Sea) during the last 5000 years." Geomorphology 107, no. 1-2 (June 2009): 10–17. http://dx.doi.org/10.1016/j.geomorph.2007.05.022.

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Jolivet, Laurent, Romain Augier, Claudio Faccenna, François Negro, Gaetan Rimmele, Philippe Agard, Cécile Robin, Federico Rossetti, and Ana Crespo-Blanc. "Subduction, convergence and the mode of backarc extension in the Mediterranean region." Bulletin de la Société Géologique de France 179, no. 6 (November 1, 2008): 525–50. http://dx.doi.org/10.2113/gssgfbull.179.6.525.

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Abstract 30-35 Ma ago a major change occurred in the Mediterranean region, from a regionally compressional subduction coeval with the formation of Alpine mountain belts, to extensional subduction and backarc rifting. Backarc extension was accompanied by gravitational spreading of the mountain belts formed before this Oligocene revolution. Syn-rift basins formed during this process above detachments and low-angle normal faults. Parameters that control the formation and the kinematics of such flat-lying detachments are still poorly understood. From the Aegean Sea to the Tyrrhenian Sea and the Alboran Sea, we have analysed onshore the deformation and P-T-t evolution of the ductile crust exhumed by extension, and the transition from ductile to brittle conditions as well as the relations between deep deformation and basin formation. We show that the sense of shear along crustal-scale detachments is toward the trench when subduction proceeds with little or no convergence (northern Tyrrhenian and Alboran after 20 Ma) and away from the trench in the case of true convergence (Aegean). We tentatively propose a scheme explaining how interactions between the subducting slab and the mantle control the basal shear below the upper plate and the geometry and distribution of detachments and associated sedimentary basins. We propose that ablative subduction below the Aegean is responsible for the observed kinematics on detachments (i.e. away from the trench). The example of the Betic Cordillera and the Rif orogen, where the directions of stretching were different in the lower and the upper crust and changed through time, is also discussed following this hypothesis.

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Дисертації з теми "Karsts – Aegean Sea Region":

Wyers, Gerard Paul. "Petrogenesis of calc-alkaline and alkaline magmas from the southern and eastern Aegean Sea, Greece /." The Ohio State University, 1987. http://rave.ohiolink.edu/etdc/view?acc_num=osu148758688918709.

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Raptis, Konstantinos. "Climatological Factors Affecting Electromagnetic Surface Ducting in the Aegean Sea Region." Thesis, Monterey, California. Naval Postgraduate School, 2012. http://hdl.handle.net/10945/6857.

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We have studied the conditions that affect atmospheric electromagnetic surface ducts in the Aegean Sea region and how those conditions are related to regional and global scale climate variations. As a primary source for our calculations, we used radiosonde soundings from three different stations situated around the Aegean Sea, analyzing a 20-year period, from 1991 to 2010. We derived statistics on ducting parameters and correlated them with the seasonal means of selected climate system variables. We focused on seasonal and interannual variations in surface ducting frequency, height, and strength gradient. We found that variations in low level atmospheric moisture were a dominant factor governing variations in surface ducting conditions. The moisture variations were mainly associated with fluctuations in (1) moisture advection associated with mid-latitude cyclones in winter; and (2) local and regional evaporation in summer. The frequency of surface ducts in the summer was twice that for the winter due to larger amounts of atmospheric moisture in the summer. Variations in large-scale subsidence did not seem to significantly affect surface ducting variations. From an interannual perspective, the years that were characterized by increased moisture amounts also tended to exhibit stronger and more frequent ducting conditions for both winter and summer. We found significant correlations between Aegean surface ducting conditions and (1) local and regional moisture(r = 0.85 with significance level p = 99%); and,(2) climate variations that affect local and regional moisture, such as those associated with the Arctic Oscillation (AO), North Atlantic Oscillation (NAO), and south Asian monsoon conditions (r 0.60 with p 95%). As a by-product, we also discovered significant correlations (ranging from r = 0.67 to r = 0.96 with p 95%) between ducting parameters and the vertical resolution of the radiosonde data, indicating that differences in data collection procedures need to be accounted for when conducting ducting analyses based on radiosonde data.

Smith, Andrew David. "Late Quaternary tectonics, sedimentation and sea-level changes in the North Aegean region." Thesis, University of Cambridge, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.321021.

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Dominey-Howes, Dale Tim Maurice. "The geomorphology and sedimentology of five tsunamis in the Aegean Sea region, Greece." Thesis, Coventry University, 1996. http://curve.coventry.ac.uk/open/items/d00a4bee-398c-0e07-0aec-c4e0dd09e7b1/1.

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This dissertation presents the detailed results of investigations of the geomorphological and sedimentary processes associated with five Holocene tsunamis reported to have occurred in the Aegean Sea region of Greece. This research considers the effects of the widely quoted and archeologically important Minoan tsunami of the 17th century B.C.; the central southern Aegean tsunami of 66 A.D.; a hugely destructive tsunami reported to have followed a massive earthquake on the 21st July 365 A.D.; a tsunami of volcanic origin which affected the island of Thira on 29th September 1650 A.D.; and the destructive southern Aegean tsunami of 9th July 1965 A.D. The last account is believed to be the first systematic investigation of the geomorphology and sedimentology of a modern Aegean tsunami. This research is primarily concerned with the investigation of Holocene coastal sedimentary sequences in order to identify any geological traces of the former tsunamis and it is hoped that this evidence can be used to supplement the fragmentary historic accounts. This dissertation also considers whether microfossils can be used in the identification of individual stratigraphic horizons associated with tsunami-deposited sediments and investigates whether it is possible to determine the generative origins of individual tsunamis on the basis of the sediments associated with them. Whilst the findings of this research are not intended to provide a definitive account of the tsunamis considered, they do provide important evidence where the prevailing geological conditions of the Aegean Sea region would otherwise combine to limit the data available. Furthermore, it is believed that the results of this investigation do contribute to existing knowledge and will be of value to archaeologists seeking to explore the relationships between archaeological sites, landscape evolution and environmental change.

Merriman, Kristine Roberta. "The context of organic residues in archaeological vessels of ceramic and Bronze." Thesis, University of Oxford, 2014. https://ora.ox.ac.uk/objects/uuid:40bef755-49f0-4c51-ad13-41bf7bec55df.

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Since the 1970s, the study of molecular organics preserved in archaeological ceramics, commonly referred to as organic residue analysis, has been used to infer vessel use and study dietary, economic, and ritual activities in the past. The purpose of this project is to analyse organic residues from a variety of ancient vessels and attempt to understand further the relationship between molecular organic preservation and vessel characteristics. It has been previously assumed that the absorption of these organics in the ceramic matrix is predominantly responsible for their preservation. The clarification of this or other preservative mechanisms and the further understanding of the relationships of vessels with their contents has a direct impact on the interpretation of organic residues and vessel use. The first section addresses the preservation of molecular organics in pottery vessels from Tel Kabri, Israel; Tel Megiddo, Israel; and Lefkandi, Greece. The one hundred and thirty-three samples from these three sites represent vessels used in domestic, burial, ritual, and elite contexts from the Early Bronze Age through the Iron Age Eastern Mediterranean. The focus of the study is the quantification of residue yields and identification of potential links with vessel properties and characteristics of the ceramic samples. Sequential extractions using two methods, conventional chloroform/methanol solvent extraction and direct FAME extraction/derivatisation, were applied to the sherds to test the absorption and adsorption of organics into ceramic materials. The majority of samples were tested non-destructively, enabling the comparison of residue yields to certain vessel properties and characteristics displayed in the same sherds. Where available, data concerning vessel form, sampling location on the vessel profile, thickness measurements were recorded, and XRF measurements were taken, with this in mind. The second section investigates the question of whether bronze and copper alloy vessels have the capability to preserve molecular organics within their corrosion products. Twenty-two samples of corrosion and associated material from five Early Roman bronze vessels found in cremation burials during the A2 Pepperhill to Cobham project in County Kent, United Kingdom were studied for organic material. These samples provide some of the first evidence that the residues of original content are preserved in copper alloy vessels either through entrapment in or reactions with copper corrosion.

Hay, Anne Persida. "Physical and metaphysical zones of transition : comparative themes in Hittite and Greek Karst landscapes in the Late Bronze and Early Iron ages." Diss., 2021. http://hdl.handle.net/10500/27463.

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English, Afrikaans and Zulu summaries
While there is increasing interest in the effect of landscape on ancient imagination, less attention has been paid to the impact of restless karst hydrology on ancient beliefs. By identifying shared themes, this study compares and contrasts the way Hittites and Aegean people in the Late Bronze and Early Iron Ages reshaped peripheral karst landscapes into physical and imagined transitional zones. Karst geology underpins much of the Aegean and Anatolian landscape, allowing subterranean zones to be visible and accessible above ground via caves, springs, sinking streams, sinkholes and other unusual natural formations. In both cultures, certain dynamic landscapes were considered to be sacred porous points where deities, daemons, heroes and mortals could transit between cosmic realms. Evidence suggests that Hittites and Aegean people interpreted dramatic karst landscapes as liminal thresholds and spaces situated between the world of humans and the world of deities. Part One investigates physical zones of transition via the karst ecosystems of rural sanctuaries. Part Two considers the creative interpretation in myth and iconography of karst phenomena into metaphysical zones of transition. The examples reveal the way in which Hittites and Aegean people built their concept of the sacred on the extraordinary characteristics of karst geology. Numinous karst landscapes provided validity and a familiar reference point for the creation of imagined worlds where mortal and divine could connect.
Vandag is daar toenemende belangstelling in die effek van die landskap op die verbeelding van die mensdom in die oudheid - maar minder aandag word bestee aan die impak van die rustelose karst landskap op die mens se gelowigheid in die oudheid. Deur die identifisering van sekere gemene temas, vergelyk hierdie verhandeling die manier waarop die Hetiete en die Egeïese volkere in die Laat Brons- en vroeë Ystertydperke die omliggende karstlandskap herskep het in fisiese en denkbeeldige oorgangszones. Die Egeïese en Anatoliese landskap bestaan grotendeels uit karst geologie, met tot gevolg dat ondergrondse zones bo die grond sigbaar en toeganklik is in die vorm van grotte, bronne, sinkgate en ander uitsonderlike natuurlike formasies. In beide bogenoemde kulture is sekere landskapstonele beskou as heilige en poreuse punte waar gode, demone, helde en sterwelinge tussen die kosmiese zones kon beweeg. Die getuienis van die tyd suggereer dat die Hetiete en die Egeïese volkere die dramatiese karst landskappe as grense of drempels tussen hulle wêreld en dié van die gode beskou het. Deel Een ondersoek die fisiese oorgangszones deur te kyk na die karst ecostelsels waarin plattelandse heiligdomme hulle bevind het. Deel Twee beskou die kreatiewe gebruik van karst verskynsels as voorstellings van metafisiese oorgangszones in die gekrewe bronne en ikonografie. Die geselekteerde voorbeelde dui aan die manier waarop die Hetiete en Egeïese volke hulle konsepte van heiligdom gebaseer het op die buitengewone verskynsels van karst geologie. Numineuse karst landskappe het hulle idees gestaaf en ‘n bekende verwysingspunt uitgemaak waar die menslike en die goddelike met mekaar in kontak kon kom.
Ngenkathi intshisekelo ekhulayo yethonya lokwakheka komhlaba emcabangweni wasendulo, kunakwe kancane umthelela we-karst hydrology engenazinkolelo ezinkolelweni zasendulo. Ngokukhomba izingqikithi okwabelwana ngazo, lo mqondo uqhathanisa futhi uqhathanise indlela amaHeti nabantu base-Aegean kweLate Bronze kanye ne-Early Iron Ages abuye abuye abumbe kabusha imigwaqo ye-karst yomngcele ibe yizingxenye zesikhashana zomzimba nezicatshangwe. I-Karst geology isekela kakhulu indawo yezwe i-Aegean ne-Anatolian evumela ukuthi izindawo ezingaphansi komhlaba zibonakale futhi zifinyeleleke ngaphezu komhlaba ngemigede, iziphethu, imifudlana ecwilayo, imigodi yokushona nokunye ukwakheka okungokwemvelo okungajwayelekile. Kuwo womabili amasiko izindawo ezithile eziguqukayo zazithathwa njengezindawo ezingcwele zokungena lapho onkulunkulu, amademoni, amaqhawe nabantu abafayo bengadlula phakathi kwezindawo zomhlaba. Ubufakazi bukhombisa ukuthi amaHeti nabantu base-Aegean bahumusha imidwebo emangazayo yekarst njengemikhawulo yemikhawulo nezikhala eziphakathi komhlaba wabantu nezwe lonkulunkulu. Ingxenye yokuqala iphenya izindawo eziguqukayo zomzimba ngokusebenzisa imvelo ye-karst yezindawo ezingcwele zasemakhaya. Ingxenye Yesibili ibheka ukutolikwa kokudala kunganekwane nakwizithonjana zezinto ze-karst kube izingxenye eziguqukayo zenguquko. Izibonelo ziveza indlela abantu abangamaHeti nabantu base- Aegean abawakha ngayo umqondo wabo ongcwele ngezimpawu ezingavamile ze-karst geology. Amathafa amahle we-karst ahlinzeka ngokusebenza kanye nephuzu elijwayelekile lesethenjwa lokwakhiwa kwamazwe acatshangelwe lapho abantu abafayo nabaphezulu bangaxhuma khona.
Biblical and Ancient Studies
M. A. (Ancient Near Eastern Studies)

Pluta, Kevin Michael. "Aegean Bronze Age literacy and its consequences." Thesis, 2011. http://hdl.handle.net/2152/ETD-UT-2011-08-4003.

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The Mycenaeans used writing for a variety of administrative purposes. The archaeological evidence for writing suggests that it was a highly restricted technology. Mycenaeans used the Linear B script to write clay tablets, inscribe sealings, and paint on vessels. There is evidence to suggest that ephemeral documents of parchment or papyrus also were used for writing. In most of these instances, writing recorded economic transactions involving the material wealth of the state. The only exception is a small number of open-shaped vessels that are likely inscribed with personal names. The Linear B script is often blamed for the restriction of writing by the Mycenaeans. This open-syllabic script does not well represent the sound of spoken Greek, and requires the frequent use of dummy vowels and the omission of consonants at the end of syllables. Studies in literacy theory, however, suggest that script usage, reading, and writing are dictated by social factors and by need, rather than by forces supposedly inherent in the script itself. Writing was restricted because Mycenaean society dictated a restricted use. The sealings and tablets, which are found at several sites throughout mainland Greece and Crete, are small in size and are found almost exclusively in administrative contexts, in buildings that have functions in central administration. Writing is never found in public displays, as it is in the contemporary Near East. There was no intent to familiarize the Mycenaean populace with the technology of writing. Training in literacy likewise appears to have been highly restrictive, with new individuals being taught by scribes on an ad hoc, individualized basis. The loyalty of scribes to the king would have been essential. The sealings and tablets record the material wealth of the kingdom that was under the management of central administration. Furthermore, the contents of the tablets are not countermarked by seal impressions that would confirm their authenticity. Scribes would have been among the king’s closest administrators and members of the elite. The restriction of writing would ensure that all written words were legitimate, as they could only be written by the most trusted individuals in the kingdom.
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Книги з теми "Karsts – Aegean Sea Region":

European Association of Archaeologists. Meeting. The Aegean Bronze Age in relation to the wider European context: Papers from a session at the Eleventh Annual Meeting of the European Association of Archaeologists, Cork, 5-11 September 2005. Oxford: Archaeopress, 2008.

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Athanasopulos, Haralambos. Greece, Turkey, and the Aegean Sea: A case study in international law. Jefferson, N.C: McFarland, 2001.

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Jasink, Anna Margherita, Luca Bombardieri, and Maria Emanuela Alberti. Le collezioni egee del Museo archeologico nazionale di Firenze. Firenze: Firenze University Press, 2009.

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Bahcheli, Tozun. Greek-Turkish relations and U.S. foreign policy: Cyprus, the Aegean, and regional stability. Washington, DC (1550 M St., NW, Washington 20005): U.S. Institute of Peace, 1997.

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Bahcheli, Tozun. Greek-Turkish relations and U.S. foreign policy: Cyprus, the Aegean, and regional stability. Washington, DC (1550 M St., NW, Washington 20005): U.S. Institute of Peace, 1997.

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Bahcheli, Tozun. Greek-Turkish relations and U.S. foreign policy: Cyprus, the Aegean, and regional stability. Washington, DC (1550 M St., NW, Washington 20005): U.S. Institute of Peace, 1997.

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International Aegean Conference (12th 2008 University of Melbourne). Dais: The Aegean feast : proceedings of the 12th International Aegean Conference,12e Rencontre égéenne internationale, University of Melbourne, Centre for Classics and Archaeology, 25-29 March 2008. Liège: Université de Liège, Histoire de l'art et archéologie de la Grèce antique, 2008.

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Yasur-Landau, Assaf. The Philistines and Aegean migration at the end of the late Bronze Age. New York: Cambridge University Press, 2010.

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Bahcheli, Tozun. Greek-Turkish relations and U.S. foreign policy. Washington, DC (1550 M St., NW, Washington 20005): U.S. Institute of Peace, 1997.

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Bahcheli, Tozun. Greek-Turkish relations and U.S. foreign policy. Washington, DC (1550 M St., NW, Washington 20005): U.S. Institute of Peace, 1997.

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Частини книг з теми "Karsts – Aegean Sea Region":

Sakellariou, Dimitris, Vasilis Lykousis, Maria Geraga, Grigoris Rousakis, and Takvor Soukisian. "Late Pleistocene Environmental Factors of the Aegean Region (Aegean Sea Including the Hellenic Arc) and the Identification of Potential Areas for Seabed Prehistoric Sites and Landscapes." In Submerged Landscapes of the European Continental Shelf, 405–29. Oxford, UK: John Wiley & Sons, Ltd, 2017. http://dx.doi.org/10.1002/9781118927823.ch15.

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Erol, Ayşe F. "New findings on the history and archaeology of the Eastern Black Sea region of Turkey:." In The Danubian Lands between the Black, Aegean and Adriatic Seas, 453–62. Archaeopress Publishing Ltd, 2015. http://dx.doi.org/10.2307/j.ctvr43k44.64.

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"Turkey’s Maritime Compliance and Enforcement of International Law of the Sea, Particularly Irregular Migration in the Aegean Sea Region." In Legal Order in the World's Oceans, 409–23. Brill | Nijhoff, 2018. http://dx.doi.org/10.1163/9789004352544_022.

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Schneider, Gerwulf, and Malgorzata Daszkiewicz. "LATE HELLENISTIC AND ROMAN TABLEWARE IN THE AEGEAN AND THE BLACK SEA REGION – WHY WE NEED CHEMICAL ANALYSIS." In Rei Cretariae Romanae Fautorum: Acta 46, 429–36. Archaeopress Publishing Ltd, 2020. http://dx.doi.org/10.2307/j.ctv1gt94kk.48.

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Koutsouflakis, George, and Peter B. Campbell. "Roman and Late Roman Pontic cargoes in the Aegean:." In The Greeks and Romans in the Black Sea and the Importance of the Pontic Region for the Graeco-Roman World (7th century BC-5th century AD): 20 Years On (1997-2017), 267–79. Archaeopress Publishing Ltd, 2021. http://dx.doi.org/10.2307/j.ctv1pdrqhw.41.

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Fant, Clyde E., and Mitchell G. Reddish. "Assos." In A Guide to Biblical Sites in Greece and Turkey. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195139174.003.0028.

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With its acropolis perched on a steep hill overlooking the Aegean Sea, the city of Assos provides a spectacular view for the visitor. From the acropolis one can look down on the ruins of the ancient buildings on the slope and also see the remains of the city’s harbor in the Aegean. On a clear day the island of Lesbos is visible approximately 7 miles south across the Bay of Edremit. From this island came the first settlers of ancient Assos. The site of ancient Assos is located in the southern part of the Troad area of Turkey, on the modern highway that runs along the Aegean coast and connects the towns of Geyikli and Ayvacïk. Assos was in the ancient region of Mysia. Today the village of Behramkale occupies the site of ancient Assos. During the 7th century B.C.E. Aeolian Greeks from the town of Methymna (modern Molivos) on the island of Lesbos crossed the Edremit Bay and founded the city of Assos. During the first half of the 6th century, King Croesus of Lydia (whose capital was at Sardis) captured and controlled Assos. Lydian domination ended in 546 B.C.E., when Cyrus of Persia defeated Croesus and brought this area of Asia Minor under Persian control. During the following century Assos gained its freedom when a coalition of Greek city-states defeated the Persians. Assos then became a part of the Delian League under the leadership of Athens. One of the rulers of Assos in the 4th century was Hermias, who had been a student, along with Aristotle, of the philosopher Plato. At the invitation of Hermias, Aristotle went to Assos and lived there from 348 to 345 B.C.E., marrying Hermias’ niece. The Persians recaptured the city and killed Hermias, but their control ended with the conquests of Alexander the Great. After Alexander’s untimely death the Seleucids ruled Assos. In 241 B.C.E. the city became a part of the Pergamene kingdom and remained under the control of the kings of Pergamum until the death of Attalus III in 133 B.C.E., at which time the city passed into Roman hands.

Fitzsimons, Rodney D., and Evi Gorogianni. "Dining on the Fringe? A Possible Minoan- Style Banquet Hall at Ayia Irini, Kea and the Minoanization of the Aegean Islands." In Minoan Architecture and Urbanism. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198793625.003.0022.

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Since its excavation by John Caskey and the University of Cincinnati from 1960 to 1976, Ayia Irini has served as one of the principal catalysts for investigations into the spread of Minoan culture throughout the Aegean in the later Middle and early Late Bronze Age (Fig. 14.1). Indeed, the abundance, concentration, and range of ceramic, architectural, iconographic, technological, and administrative evidence at the site that was inspired by, adapted, and/or adopted from the Cretan cultural package suggests that it functioned as one of the key nodes in the complex web of exchange networks that facilitated the dissemination of non-local traits across the region throughout this period (Abell 2014; Berg 2006, 2007; Davis 1979; Davis and Gorogianni 2008; Dietz 1998; Graziadio 1998; Knappett and Nikolakopoulou 2005; Knappett, Evans, and Rivers 2008; Knappett 2011; Nikolakopoulou 2007; Papagiannopoulou 1991; Schofield 1982a, 1982b, 1983, 1984a). Despite the quantity, quality, and variety of such evidence at Ayia Irini, however, only a single structure in the settlement, House A, has been hitherto recognized as betraying any indication of Minoan architectural influence (e.g. Berg 2007: 114; Cummer 1980; Cummer and Schofield 1984; Hitchcock 1998: 173; Letesson 2009: 298–303; Whitelaw 2005: 56). Currently located in the south-east quadrant of the site, though originally probably closer to its centre if changes in sea level are taken into account (Caskey 1962: 266, 278; 1964: 321; 1966: 365; 1971: 362), House A underwent a series of remodellings over the course of the Late Minoan IA through LM II periods (Cummer and Schofield 1984: 30–5; or Periods VI and VII in Caskey’s local pottery terminology), the end result of which produced an interesting blend of local and Minoanizing features.

Fant, Clyde E., and Mitchell G. Reddish. "Amphipolis." In A Guide to Biblical Sites in Greece and Turkey. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195139174.003.0008.

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The modern, small village of Amphipolis belies the importance of the ancient city whose name it bears. Located strategically along the Strymon River and on the Via Egnatia, Amphipolis was one of the most important cities of Macedonia in antiquity. The site of ancient Amphipolis is located between Thessaloniki and Kavala, about 65 miles east of Thessaloniki. From highway E90 there are signs that point the way to Amphipolis. The ancient city sits on a bend on the east bank of the Strymon River, surrounded by the river on three sides. This geographical feature gave rise to the name of the city, since Amphipolis means “around the city.” The site was originally settled by Thracians, who called their settlement Ennea Hodoi, meaning “Nine Ways” or “Nine Roads,” indicating the importance of the location as a crossroads for travel and trade routes. After several failed attempts the Athenians captured the area and founded the city of Amphipolis on the site of Ennea Hodoi in 437 B.C.E. under the leadership of Hagnon. In 424 B.C.E. the city came under Spartan control. Amphipolis was an important city both because of its strategic location on the Strymon River only 3 miles from the Aegean Sea and because of its rich natural resources of agriculture (wine, oil, and wood) and precious metals (especially gold from the mines on Mt. Pangaion). In spite of repeated attempts by the Athenians to recapture the city, Amphipolis remained a free city until its capture by Philip II of Macedon in 358–357 B.C.E. During the time of Macedonian rule, Amphipolis became one of the leading cities in the region. It was one of six cities chosen by Alexander the Great where large, costly temples were built. The city also played a significant role in Alexander’s military conquests. For example, the city and the surrounding area served as the staging ground for the beginning of Alexander’s conquest of Asia. After Alexander’s death his wife Roxane and their young son, Alexander IV, were exiled to Amphipolis. After the Roman victory at Pydna in 168 B.C.E., which effectively ended Macedonian rule, Amphipolis, along with the rest of Macedonia, became a Roman possession.

Тези доповідей конференцій з теми "Karsts – Aegean Sea Region":

Zafeiratou, Eleni, Catalina Spataru, and Raimund Bleischwitz. "Wind offshore energy in the Northern Aegean Sea islanding region." In 2016 IEEE 16th International Conference on Environment and Electrical Engineering (EEEIC). IEEE, 2016. http://dx.doi.org/10.1109/eeeic.2016.7555518.

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Nomikou, P., N. Ocakoğlu, Y. Işcan Alp, D. Lampridou, and D. Papanikolaou. "Morpho-structural setting of the eastern part of the Aegean Sea (Kos-Nisyros-Tilos-Gökova region) revealed by high-resolution bathymetry." In 16th International Conference on Geoinformatics - Theoretical and Applied Aspects. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201701840.

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Gammon, Mark, Abdi Kukner, and Ahmet Alkan. "Hull Form Optimization of Performance Characteristics of Turkish Gulets for Charter." In SNAME 17th Chesapeake Sailing Yacht Symposium. SNAME, 2005. http://dx.doi.org/10.5957/csys-2005-006.

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Turkish Gulets are motor-sailors that are still being built using wooden boatbuilding traditional construction in the Aegean and Mediterranean as well as being built using steel and cold moulded techniques. They are typical of the craft used for skippered charter tours in the region and exhibit good seakeeping in the shorter steep sea of the Mediterranean and also for manoeuvring in port and in anchorages. Usually this performance is at the cost of resistance. Sailing performance and stability are surprisingly not considered due to the large beams. The hull forms of two typical gulets are used to examine the stability, resistance and coupled heave and pitch. A multi-objective evolutionary optimization methodology is used to investigate the performance of the three objectives. The evaluation of resistance uses a transom modified Michell theory in keeping with the smaller L/B ratios and large transoms of many of these vessel types. Seakeeping is evaluated using a strip motion program and the stability curve is used to provide a stability index. The multi-objective analysis is based on the optimization capabilities of genetic algorithms. Evolutionary algorithms are stochastic in nature and follow the Darwinian principle of survival of the fittest. From a given population of hull candidates, those hulls that are “fitter” by having better resistance, seakeeping and stability are selected to generate a new population. Over the course of many generations, the hulls are optimized to provide better performance. Each of the objectives requires an index to measure the performance of the candidate.