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Bulletin of the Geological Society of Greece XLIII/2
Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, 2010 Bulletin of the Geological Society of Greece, 2010 Πρακτικά 12ου Διεθνούς Συνεδρίου Proceedings of the 12th International Congress Πάτρα, Μάιος 2010 Patras, May, 2010 REMARKS ON THE KARSTIFICATION IN THE WIDER AREA OF THE UPPER MESSINIA CLOSED HYDROGEOLOGICAL BASIN (SW PELOPONNESUS, GREECE) I. Mariolakos and E. Spyridonos National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironmetn, Department of Dynamic Tectonic & Applied Geology, GR-15784 Panepstimioupolis Zografou, Athens - Greece, [email protected], [email protected] Abstract The Upper Messinia Basin is part of the Kalamata - Kyparissia graben structure, defined by two fault zones, one of E-W direction to the north and one of N-S direction to the east. The Tripolis and the Pindos alpidic units build up the basement of the region, and are covered by post-alpidic Pleis- tocene and quaternary deposits. The Basin is a closed hydrogeological system. In the upper creta- ceous Pindos limestones, we observe two different karst types, according to drilling results. In the western part of the basin, where the limestones appear on the surface, the merokarst type is ob- served and water flow is limited in separated karstic conduits. On the contrary, in the central part of the basin, where the limestones underlie the clastic post-alpidic formations, the holokarst type is observed and a rich karstic aquifer is developed. This is explained by the closed hydraulic condi- tions. In the western part of the basin the karstic aquifer is unconfined, while in the central part it is confined, due to the overlying impermeable post-alpidic sediments and the overall closure of un- derground flow to the south. -
Remarks on the Karstification in the Wider Area of the Upper Messinia Closed Hydrogeological Basin (Sw Peloponnesus, Greece)
Bulletin of the Geological Society of Greece Vol. 43, 2010 REMARKS ON THE KARSTIFICATION IN THE WIDER AREA OF THE UPPER MESSINIA CLOSED HYDROGEOLOGICAL BASIN (SW PELOPONNESUS, GREECE) Mariolakos I. National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironmetn, Department of Dynamic Tectonic & Applied Geology Spyridonos E. http://dx.doi.org/10.12681/bgsg.11364 Copyright © 2017 I. Mariolakos, E. Spyridonos To cite this article: Mariolakos, I., & Spyridonos, E. (2010). REMARKS ON THE KARSTIFICATION IN THE WIDER AREA OF THE UPPER MESSINIA CLOSED HYDROGEOLOGICAL BASIN (SW PELOPONNESUS, GREECE). Bulletin of the Geological Society of Greece, 43(4), 1785-1791. doi:http://dx.doi.org/10.12681/bgsg.11364 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 16/08/2019 02:10:16 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, 2010 Bulletin of the Geological Society of Greece, 2010 Πρακτικά 12ου Διεθνούς Συνεδρίου Proceedings of the 12th International Congress Πάτρα, Μάιος 2010 Patras, May, 2010 REMARKS ON THE KARSTIFICATION IN THE WIDER AREA OF THE UPPER MESSINIA CLOSED HYDROGEOLOGICAL BASIN (SW PELOPONNESUS, GREECE) I. Mariolakos and E. Spyridonos National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironmetn, Department of Dynamic Tectonic & Applied Geology, GR-15784 Panepstimioupolis Zografou, Athens - Greece, [email protected], [email protected] Abstract The Upper Messinia Basin is part of the Kalamata - Kyparissia graben structure, defined by two fault zones, one of E-W direction to the north and one of N-S direction to the east. The Tripolis and the Pindos alpidic units build up the basement of the region, and are covered by post-alpidic Pleis- tocene and quaternary deposits. -
After the War Was Over Mark Mazower
After the War Was Over Mark Mazower Published by Princeton University Press Mazower, M.. After the War Was Over: Reconstructing the Family, Nation, and State in Greece, 1943-1960. Princeton: Princeton University Press, 2016. Project MUSE., https://muse.jhu.edu/. For additional information about this book https://muse.jhu.edu/book/47927 Access provided by Yale University Library (30 Mar 2017 18:23 GMT) EIGHT Red Terror: Leftist Violence during the Occupation Stathis N. Kalyvas This chapter aims to question, and help revise, one of the central, indeed hegemonic, assumptions in the study of the Greek civil war: that the Left (the National Liberation Front—EAM—and the Communist Party of Greece—KKE) has been the main (or even the only) victim of violence. The emergence and domination of such a view should come as no surprise. On the one hand, defeat in a civil war tends to be total; hence supporters of the defeated side suffer disproportionately. Indeed, most descriptions of the violence suffered by the supporters of the Left usu- ally focus either on the period immediately following the end of the occupation—often described as the period of the “white terror” (1945– 1947), or on the final phase of the civil war (1947–1949) and its after- math. On the other hand, references to left-wing terror, as plentiful as they were vague, became a key weapon in the ideological arsenal of the Greek Right. The collapse, in 1974, of the ideological hegemony of the Right erased all references to leftist terror. Indeed, recent scholarly his- torical research has tended to overlook,1 minimize,2 or whitewash3 leftist terror.4 Even serious scholarship has tended to minimize leftist terror in a variety of subtle and implicit ways—including the choice of a skewed vocabulary. -
Bulletin of the Geological Society of Greece
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by National Documentation Centre - EKT journals Bulletin of the Geological Society of Greece Vol. 43, 2010 REMARKS ON THE KARSTIFICATION IN THE WIDER AREA OF THE UPPER MESSINIA CLOSED HYDROGEOLOGICAL BASIN (SW PELOPONNESUS, GREECE) Mariolakos I. National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironmetn, Department of Dynamic Tectonic & Applied Geology Spyridonos E. https://doi.org/10.12681/bgsg.11364 Copyright © 2017 I. Mariolakos, E. Spyridonos To cite this article: Mariolakos, I., & Spyridonos, E. (2010). REMARKS ON THE KARSTIFICATION IN THE WIDER AREA OF THE UPPER MESSINIA CLOSED HYDROGEOLOGICAL BASIN (SW PELOPONNESUS, GREECE). Bulletin of the Geological Society of Greece, 43(4), 1785-1791. doi:https://doi.org/10.12681/bgsg.11364 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 20/02/2020 23:34:43 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, 2010 Bulletin of the Geological Society of Greece, 2010 Πρακτικά 12ου Διεθνούς Συνεδρίου Proceedings of the 12th International Congress Πάτρα, Μάιος 2010 Patras, May, 2010 REMARKS ON THE KARSTIFICATION IN THE WIDER AREA OF THE UPPER MESSINIA CLOSED HYDROGEOLOGICAL BASIN (SW PELOPONNESUS, GREECE) I. Mariolakos and E. Spyridonos National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironmetn, Department of Dynamic Tectonic & Applied Geology, GR-15784 Panepstimioupolis Zografou, Athens - Greece, [email protected], [email protected] Abstract The Upper Messinia Basin is part of the Kalamata - Kyparissia graben structure, defined by two fault zones, one of E-W direction to the north and one of N-S direction to the east. -
Top-Down Reconciliation and the Role of Time the Case of the Greek Civil War
Top-down reconciliation and the role of time The case of the Greek Civil War Authors: Dimitrios Stratakos Tutor: Manuela Nilsson Peace and Development Work Examiner: Heiko Fritz Subject: Peace and Development Level and semester: Master'sThesis Spring 2013 MASTER’S PROGRAMME IN PEACE AND DEVELOPMENT WORK Course Code: 4FU41E Top-down reconciliation and the role of time The case of the Greek Civil war Author: Dimitrios Stratakos Tutor: Manuela Nilsson 14/6/2013 School of Social Sciences ACKNOWLEDGEMENTS This report is the result of a five weeks field work on behalf of the Master’s programme in Peace and Development work of Linnaeus University, Sweden. I would like to acknowledge my gratitude to Mr. Charilaos Sismanis and Mrs. Katherine Stefatos for their assistance and advice. I also want to thank Evi and Vasilis Mitseas, as well as Tzanakaki and Giftea families for their kind support, both practical and psychological during my fieldwork; an additional thank you to Evangelos Pournaras, Antonis Bourgias and my colleague Michael Edwards for their enlightening advice. I want to thank my family and friends that have always been supportive during the whole process. I would also like to express my gratitude to all the people that accepted to take part in this research. I am grateful that I had the chance to listen to so many stories and experiences about an issue that every Greek should be aware of. Finally, I want to acknowledge my gratitude to Professor Manuela Nilsson. Her patience and guidance during the whole process were of great importance to me. It would have been impossible to conduct this study without her. -
Inhoudsopgave
Inhoudsopgave Inleiding 7 Pylos en noordelijk van Pylos 72 ROUTE 2: ACHTERGRONDEN 9 Pylos – Korifasi – paleis van Nestor – Landschap 9 Chora – Gargaliani – Filiatra – Ligging 9 Christiani – Chora – Pylos (circa 85 km) Klimaat en reistijd 11 Alternatief: vanaf Filiatra langs de kust Flora en fauna 13 naar Marathopoli – Petrachori – Het verleden 14 Gialova – Pylos (circa 95 km) 72 Mythologie 14 De eilanden in de baai van Navarino 75 Beknopte geschiedenis van de Tishli-Baba 76 Peloponnesos 17 Helonaki 76 De bevolking 22 Noordelijk van Pylos 76 Vlag en volkslied 22 Schiereiland Messenia 82 Volksfeesten 24 ROUTE 3: Taal en geloof 26 Pylos – Methoni – Finikounda – Koroni – Iets over de inrichting van het kerk- Longa – Petalidi – Rizomilos – Pylos gebouw 28 (circa 90 km) 82 Cultuur 30 Literatuur 30 De Mani 89 Bouwkunst 30 De Buiten-Mani 91 Economie 35 ROUTE 4: Kalamata – Areopoli – Githio – Sparti – PRAKTISCHE INFORMATIE 37 Kalamata (circa 200 km) 91 Van A tot Z 37 Githio – Sparta 94 Sparta 94 BEZIENSWAARDIGHEDEN 61 Sparta – Kalamata 98 Het zuidwesten 61 De Binnen-Mani 104 Kalamata en Antiek Messini 64 ROUTE 5: ROUTE 1: Areopoli – Pirgos Dirou – Kalamata – Thouria – Aris – Eva – Paliros – Kokkala – Kotronas – Valira – Mavromati – Antiek Messini – Passavas – Githio (circa 100 km) 104 Zerbisia – Meligalas – Meropi – Kalamata (circa 80 km) 66 Het zuidoosten 109 De opgravingen 68 ROUTE 6: ROUTE 1A: Geraki – Vrontamas – Skala – Molai – Thouria – Dirrachi – Leptini – Neochori – Monemvasia – Limenas Geraka – Kalamata (circa 50 km) 69 Richia – Metamorfosi – Molai – Apidia – ROUTE 1B: Geraki (150 km) 109 Messini – Kefalinos – Kopanaki – Geraki 109 Platania – Figalia – Sidirokastro – Kalo ROUTE 6A: Nero (circa 75 km) 70 Verlenging: Richia – Paralia en/of 3 RHB Peloponnesos deel 1.indd 3 29-09-15 11:04 Inhoudsopgave Monemvasia – Neapoli (circa 70 km) 112 ROUTE 12: ROUTE 7: Korinthos – kustweg tot Derveni – Geraki – Ag. -