Relevant bibliographies by topics / Pindus Mountains Region (Greece)

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  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Pindus Mountains Region (Greece)'

Author: Grafiati
Published: 28 July 2024
Last updated: 31 July 2025

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Journal articles on the topic "Pindus Mountains Region (Greece)"

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Ainalis, Apostolos. "Multitemporal Land Use Changes in a Region of Pindus Mountain, Central Greece." Agriculture, Forestry and Fisheries 4, no. 1 (2015): 18. http://dx.doi.org/10.11648/j.aff.20150401.14.

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Tasic, Nikola. "Some reflections on the migrations of palaeo-Balkan peoples in pre-roman times." Balcanica, no. 45 (2014): 15–23. http://dx.doi.org/10.2298/balc1445015t.

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In the history of the central Balkans prior to the Roman conquest migrations of people had manifold importance. The recognition of these migrations has been the basis for distinguishing between different periods of prehistory. Various analyses of the material culture offer information on the social contact between the invaders and the autochtonous populations. They reveal details of the transfer of elements of culture and technological knowledge from one region to another. Of particular significance in this respect are migrations over vast territories, sometimes from as far as the Ural mountai
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Wong, Kevin, Kathryn Draper, Linshu Feng, Philip Hawkins, Samuel Oakley, and Xiao Xu Zheng. "The geology of Mount Orliakas and the Pindos Ophiolite, Greece." Bulletin of the Geological Society of Greece 54, no. 1 (2019): 144. http://dx.doi.org/10.12681/bgsg.19376.

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The Greveniotiki Pindos Mountains of Greece showcases the tectonicsaffecting the Central Mediterranean; however no detailed geologicalmaps have been produced of the region. In this study we present a1:10000 geological map of Mount Orliakas and its surrounding areas,including westernmost parts of the Pindos Ophiolite complex and theMesohellenic basin. We also provide new lithological, structural, andpalaeontological discussions of the region and give new evidence forthe provenance of the Kranea Formation.
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Kafetzidou, Aikaterini, Eugenia Fatourou, Konstantinos Panagiotopoulos, Fabienne Marret, and Katerina Kouli. "Vegetation Composition in a Typical Mediterranean Setting (Gulf of Corinth, Greece) during Successive Quaternary Climatic Cycles." Quaternary 6, no. 2 (2023): 30. http://dx.doi.org/10.3390/quat6020030.

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The Gulf of Corinth is a semi-isolated basin in central Greece interrupting the Pindus Mountain Range, which nowadays is a biodiversity hotspot. Considering its key location, deep drilling was carried out within the International Ocean Discovery Program (IODP; Expedition 381: Corinth Active Rift Development) aiming to improve our understanding of climatic and environmental evolution in the region. Here, we present a new long pollen record from a Mediterranean setting in the southernmost tip of the Balkan Peninsula recording the vegetation succession within the Quaternary. The Corinth pollen re
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Jones, Gregory, Patrick de Wever, and Alastair H. F. Robertson. "Significance of radiolarian age data to the Mesozoic tectoni and sedimentary evolution of the northern Pindos Mountains, Greece." Geological Magazine 129, no. 4 (1992): 385–400. http://dx.doi.org/10.1017/s0016756800019488.

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AbstractRadiolarians were extracted from siliceous sediments of the northern Pindos Mountains, in an attempt to establish the chronology of tectonic and stratigraphic events related to the evolution of the Pindos ocean basin. Three separate phases of siliceous sedimentation were identified: (i) (mid-) late Triassic; (ii) mid-late Jurassic and (iii) mid-late Cretaceous. The first two phases are also known from the Pindos and Sub-Pelagonian zones of southern and central Greece, and elsewhere in the Dinarides andHellenides. However, the occurrence of Cretaceous radiolarites in the west central Te
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Hughes, P. D., J. C. Woodward, P. L. Gibbard, M. G. Macklin, M. A. Gilmour, and G. R. Smith. "The Glacial History of the Pindus Mountains, Greece." Journal of Geology 114, no. 4 (2006): 413–34. http://dx.doi.org/10.1086/504177.

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Jiménez-Mejías, Pedro, and Modesto Luceño. "Carex castroviejoi Luceño & Jiménez Mejías (Cyperaceae), a new species from North Greek mountains." Acta Botanica Malacitana 34 (December 1, 2009): 231–33. http://dx.doi.org/10.24310/abm.v34i0.6911.

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Carex castroviejoi Luceño & Jiménez Mejías (Cyperaceae), una especie nueva de las montañas del norte de GreciaPalabras clave. Grupo de Carex flava, Grecia, Montes Pindo, serpentinas, endemismo.Key words. Carex flava group, Greece, Pindus mountains, serpentines, endemic.
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Lewin, John, Mark G. Macklin, and Jamie C. Woodward. "Late Quaternary Fluvial Sedimentation in the Voidomatis Basin, Epirus, Northwest Greece." Quaternary Research 35, no. 1 (1991): 103–15. http://dx.doi.org/10.1016/0033-5894(91)90098-p.

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AbstractDetailed morpho- and lithostratigraphic investigations, allied with radiometric dating, in the Voidomatis basin, Epirus, northwest Greece, have identified four Quaternary terraced alluvial fills that range from middle Pleistocene to historic in age. Major-periods of alluviation during the late Quaternary were associated with valley glaciation (ca. 26,000–20,000 yr B.P.) and subsequent deglaciation (ca. 20,000–15,000 yr B.P.) in the Pindus Mountains during Late Würmian times, and more recently linked to overgrazing sometime before the 11th century AD. The late Quaternary alluvial strati
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Hughes, P. D., P. L. Gibbard, and J. C. Woodward. "Middle Pleistocene glacier behaviour in the Mediterranean: sedimentological evidence from the Pindus Mountains, Greece." Journal of the Geological Society 163, no. 5 (2006): 857–67. http://dx.doi.org/10.1144/0016-76492005-131.

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ŠLENKER, MAREK, MARIÁN PERNÝ, JUDITA ZOZOMOVÁ-LIHOVÁ, and KAROL MARHOLD. "Taxonomic position and circumscription of Cardamine barbaraeoides (Brassicaceae), a systematically challenging taxon from the Balkan Peninsula." Phytotaxa 502, no. 2 (2021): 111–32. http://dx.doi.org/10.11646/phytotaxa.502.2.1.

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The Balkan Peninsula, and the territory of Greece in particular, is a significant biodiversity hotspot in the Mediterranean that is rich in endemic plants. The focal species of this study, Cardamine barbaraeoides, is a narrow Greek endemic that has been confused taxonomically since its original description. Based on a detailed multivariate morphometric study, we provide here a set of morphological characters that enables the reliable identification of this species. In addition, we present an identification key to C. barbaraeoides and related taxa. We have revised herbarium specimens and litera
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Dissertations / Theses on the topic "Pindus Mountains Region (Greece)"

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Hughes, Philip David. "Quaternary glaciation in the Pindus Mountains, Northwest Greece." Thesis, University of Cambridge, 2004. https://www.repository.cam.ac.uk/handle/1810/273442.

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Geomorphological and geological evidence for former Quaternary glaciation has been mapped n the Pindus Mountains of Northwest Greece. the dynamics and chronology of glaciation in this area has been established through sedimentological analysis, soil analysis and Uranium-series dating. Four glacial events are recorded in the sedimentological and geomorphological records. The more extensive recorded glaciation pre-dates 350,000 years BP and was characterised by extensive valley glaciers and ice-fields. A second glaciation occurred prior to the last interglacial, before <i>ca</i>. 127,000 years B
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Books on the topic "Pindus Mountains Region (Greece)"

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Provopoulos, Ēlias G. Oreinē patrida. Ekdosē tēs Dieurymenēs Koinotētas Neraïdas Trikalōn, 2007.

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Greece) Hieros Naos tēs Hagias Marinas Kissou (Pelion Mountains Region. Ho naos tēs Hagias Marinas Kissou: Historia, poleodomia, architektonikē, eikonographia. Dēmos Mouresiou, 2009.

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Book chapters on the topic "Pindus Mountains Region (Greece)"

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Hughes, Philip, and Jamie Woodward. "Glacial and Periglacial Environments." In The Physical Geography of the Mediterranean. Oxford University Press, 2009. http://dx.doi.org/10.1093/oso/9780199268030.003.0024.

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Traditionally, glacial and periglacial geomorphology has not featured prominently in discussions about the physical geography of the Mediterranean basin. It is now clear, however, that on numerous occasions during the Pleistocene, and to a lesser extent during the Little Ice Age (LIA), glacial and periglacial activity was widespread in many of the region’s mountain ranges (Hughes et al. 2006a; Hughes and Woodward 2008). Even today, small glaciers and active periglacial features can be found on the highest peaks. Many mountain landscapes in the Mediterranean basin are therefore the product of g
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Fant, Clyde E., and Mitchell G. Reddish. "Antioch of Pisidia." In A Guide to Biblical Sites in Greece and Turkey. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195139174.003.0027.

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Although overshadowed in the New Testament by a different Antioch (Antioch on the Orontes), Antioch of Pisidia was an important city during Hellenistic and Roman times. Archaeological excavations have uncovered the remains of a thriving city, complete with theater, baths, temples, stadium, nymphaeum, paved streets, and aqueduct. Augustus had a copy of his famous Res Gestae, the list of his accomplishments, inscribed on his sanctuary in the city. Several cities in the ancient world were called Antioch, named for various members of the Seleucid dynasty who bore the name of Antiochus. Antioch of
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Fant, Clyde E., and Mitchell G. Reddish. "Tarsus." In A Guide to Biblical Sites in Greece and Turkey. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195139174.003.0047.

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Tarsus, best known as the home of the Apostle Paul, was the principal city of the eastern Cilician plain. A city renowned in antiquity as a center of culture and learning, Tarsus was visited by such figures as Julius Caesar, Mark Antony, and Cleopatra. Recent excavations have uncovered more remains of the city from Hellenistic and Roman times, including a paved, colonnaded street. Tarsus, the capital of the ancient province of Cilicia, is located near the eastern Mediterranean coast of Turkey. Situated today 10 miles inland from the sea, Tarsus served as a port city because the Cydnus River (t
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O'Brien, William. "Eastern and Central Mediterranean." In Prehistoric Copper Mining in Europe. Oxford University Press, 2014. http://dx.doi.org/10.1093/oso/9780199605651.003.0008.

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Copper objects first circulated on the Greek mainland during the fifth millennium BC and shortly after in the islands of the southern Aegean (Zachos 2007). The earliest metalwork of Late Neolithic date comprised small objects such as awls, beads, and bracelets. Metal use gradually expanded during the Chalcolithic stage that followed, with production of larger items such as axeheads. There are parallels with the development of early metallurgy in the Balkans, however there was much less copper in circulation. This may be explained by the absence of early copper mines comparable to Rudna Glava o
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Kamil, İbrahim. "Bulgaristan Diplomatik Belgelerine Göre Batı Trakya’da Fransız İdaresi (1919-1920)." In Millî Mücadelenin Yerel Tarihi 1918-1923 (Cilt 10): Edirne - Kırklareli - Tekirdağ. Türkiye Bilimler Akademisi, 2023. http://dx.doi.org/10.53478/tuba.978-625-8352-72-6.ch09.

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"The Western Thrace region, stretching from the Meriç River to Mesta-Karasu, from the Rhodope Mountains to the Aegean Sea, was taken from the Ottoman Empire and given to Bulgaria with the 1913 Bucharest Treaty signed after the Balkan Wars. The Western Thrace, which was ruled by Bulgaria until 1919, passed under the administration of the Allied Powers with the Treaty of Neuily signed after this country was defeated in World War I. French General Charpy was appointed as Governor of Western Thrace. The General-Governor established a political system called the ""Inter-Allied Thrace Government"" i
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Fant, Clyde E., and Mitchell G. Reddish. "Lystra." In A Guide to Biblical Sites in Greece and Turkey. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195139174.003.0037.

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Few visitors seek out the ancient site of Lystra. Neither its unexciting location in the Anatolian plain nor its unexcavated mound offer much enticement except to the hard-core adventurer seeking to trace the route of the Apostle Paul. The ancient city of Lystra was located near the modern village of Hatunsaray, approximately 24 miles southwest of Konya in south-central Turkey. In 1885, about a mile north of Hatunsaray, on a mound called Zoldera (or, variously, Zordula), J. R. Sitlington Sterrett discovered a stone block approximately 3.5 feet tall and 1 foot thick. On the stone was the Latin
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Crouch, Dora P. "Central Greco-Roman Cities." In Geology and Settlement. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780195083248.003.0010.

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Argos, situated in the southern peninsula of Greece called the Peloponnese, lies on the northwest side of the Argos Plain, backed by hills to the north and west that are the eastern edge of an extensive region of mountains and intermountain basins. A road runs northward through the valley and over the hills to Nemea and Corinth. Eastward beyond the capricious rivers lie the old Mycenaean cities of Mycenae and Tiryns on their knolls, with the port of Nauplia closing the circuit to the southeast. Beyond Nauplia is the Argolid peninsula with the ancient pilgrimage and health center of Epidauros.
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Fant, Clyde E., and Mitchell G. Reddish. "Attalia." In A Guide to Biblical Sites in Greece and Turkey. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195139174.003.0029.

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Antalya, the modern name for ancient Attalia, is a delightful city perched on the Mediterranean coast of southern Turkey. The eleventh largest city in modern Turkey, Antalya is a thriving tourist center. Although many visitors to the city use it as a base for visiting beaches along Turkey’s Mediterranean coast or archaeological sites in nearby locations, Antalya has plenty of charm and interest of its own. Attalia was a city in the region known as Pamphylia, an area bounded by the Taurus Mountains on the north and the Mediterranean Sea on the south. Situated on what is now called the Gulf of A
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Price, T. Douglas. "Centers of Power, Weapons of Iron." In Europe before Rome. Oxford University Press, 2013. http://dx.doi.org/10.1093/oso/9780199914708.003.0009.

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The introduction of iron after 1000 BC brought new tools and weapons to Europe. Smelting technology and higher furnace temperatures were likely the key to iron production, which is generally thought to have originated in Anatolia around 1400 BC among the Hittites, but there are a few earlier examples of iron artifacts as old as 2300 BC in Turkey. Iron produced sharper, more readily available implements and was in great demand. In contrast to copper and tin, whose sources were limited, iron was found in a variety of forms in many places across the continent. Veins of iron ore were exploited in
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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
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Conference papers on the topic "Pindus Mountains Region (Greece)"

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Ravet, Fabien, Damien Moureaux, Theodoros Stimaratzis, Cristian Grecco, and Etienne Rochat. "Natural Hazards Events Identification Along the Trans Adriatic Pipeline Monitoring With Geotechnical Monitoring System." In 2024 15th International Pipeline Conference. American Society of Mechanical Engineers, 2024. https://doi.org/10.1115/ipc2024-133985.

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Abstract Landslides and unstable ground conditions represent a significant hazard for pipelines since they can generate permanent ground displacement (PGD) along or across the pipeline alignment. Pipeline rupture is not uncommon in incidents caused by landslides. As such, landslide-related incidents often result in leaks that may have severe environmental impact as well as long periods of operational stoppage. Regarding pipelines running through mountainous areas, statistics show that landslides are the most common cause of pipeline rupture and as such the most significant operational risk. Th
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Valkaniotis, Sotiris, Maria Taftsoglou, George Papathanasiou, Domna Samara, Caterina Zei, and Themistoklis Chatzitheodosiou. "Development of a medicane-induced landslide inventory; case study of 2023 Cyclone Daniel, Central Greece." In 4th European Regional Conference of IAEG. University of Zagreb Faculty of Civil Engineering, 2024. https://doi.org/10.5592/co/euroengeo.2024.163.

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Cyclone (medicane) Daniel was a devastating Mediterranean tropical-like cyclone that affected Greece during September 4-8 2023. Severe rainfall in central and southern Greece led to widespread landslides and flooding that caused more than 2 billions in damages. Flooding in Thessaly region surpassed 800,000 hectares, the largest recorded flood event in recent history. The area most affected by landslides and debris flows was the mountainous part of Western Thessaly, along Pindos mountain range, where severe mass wasting was also documented during Medicane Ianos in September 2020. Using post-eve
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Dimitrov, Nikolay. "APPLICATION OF GPS FOR STUDY THE GEODYNAMIC PROCESSES IN THE REGION OF SOUTHWESTERN BULGARIA." In 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022/2.1/s09.21.

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The article summarizes the main geodetic activities performed in the region of Southwestern Bulgaria to study the modern crustal movements and clarify the geodynamic situation of the region. The study area is bounded to the north of the southern slopes of the Balkan Mountains, to the south to the southern slopes of the Rila Mountains, to the west � the western border of Bulgaria and to the east � the beginning of the Upper Thracian plain. The area has a complex geological structure with many active faults that must be studied. The region is of particular interest due to its high population den
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