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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 GEOMORPHIC EVOLUTION OF WESTERN (PALIKI) KEPHALONIA ISLAND (GREECE) DURING THE QUATERNARY Gaki - Papanastassiou K. University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatology Karymbalis E. Harokopio University, Department of Geography Maroukian H. University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Tsanakas K. University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and http://dx.doi.org/10.12681/bgsg.11193 Copyright © 2017 K. Gaki - Papanastassiou, E. Karymbalis, H. Maroukian, K. Tsanakas To cite this article: Gaki - Papanastassiou, K., Karymbalis, E., Maroukian, H., & Tsanakas, K. (2010). GEOMORPHIC EVOLUTION OF WESTERN (PALIKI) KEPHALONIA ISLAND (GREECE) DURING THE QUATERNARY. Bulletin of the Geological Society of Greece, 43(1), 418-427. doi:http://dx.doi.org/10.12681/bgsg.11193 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 10/01/2020 22:39:34 | 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 GEOMORPHIC EVOLUTION OF WESTERN (PALIKI) KEPHALONIA ISLAND (GREECE) DURING THE QUATERNARY Gaki - Papanastassiou K.1, Karymbalis E.2, Maroukian H.1 and Tsanakas K.1 1 University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatologyy, 15771 Athens, Greece Emails: [email protected], [email protected], [email protected] 2 Harokopio University, Department of Geography, 70 El. -
Onshore Drilling Outcomes in Kefalonia Issued 16 September 2015
Onshore Drilling Outcomes in Kefalonia Issued 16 September 2015 Summary The results of the geoscientific campaign unveiled a complex geo-tectonic and geological landscape beneath the Thinia valley, the isthmus separating the western peninsula of Paliki from the rest of Kefalonia. It has superseded the simple side-wall collapse and in-fill hypothesis and has raised another possibility, that of a massive rotational slump, leading to a toe-thrust and the elevation of an ancient marine channel. The critical question then becomes one of timing: could this rotational slump have occurred recently (in the last ~3,200 years) and therefore be responsible for in-filling and displacement of a Mycenaean age marine channel? Other promising findings include the discovery of ancient beach deposits buried under land-slip infill at the northern end of the Thinia valley and evidence of an ancient marine harbour that reached the foot of Kastelli Hill and that contained radiocarbon-datable samples attributable to the Bronze Age. An anomalous late-period lakebed, now dried out, is another intriguing finding. It is also worth reiterating that Mycenaean-era sites have been previously identified on both the western peninsula (called Paliki) and the remaining part of the island of Kefalonia, confirming that this land is of considerable historical and archaeological interest dating to the period in question. The geological research sponsored by Fugro and directed by Professor John Underhill has been completed safely, successfully and with no harm to the environment. Thinia valley panorama looking east from Paliki Project Background The objective of this phase of geoscientific research has been to test the proposition that the island of Ithaca may have been accurately described in Homer’s Odyssey as the furthest west of a group of four islands off the western coast of Greece, facing dusk, the open sea and being of low elevation. -
Applicant UNESCO Global Geopark
Applicant UNESCO Global Geopark Kefalonia-Ithaca, Greece Geographical and geological summary 1. Physical and human geography The Kefalonia – Ithaca applicant UNESCO Global Geopark is located in Western Greece (SE Europe). It is an island complex (Kefalonia-Ithaca-Atokos-Arkoudi) belonging to the Heptanese (Ionian Sea). It is located 340,3 km from Athens, the capital of Greece and 165.37 and 258 km from Albania and Italy respectively. Its surface area reaches 3.006 km2 and includes 913,075 km2 of land and 2.092,9 km2 of marine area. The geopark ‘s area belongs administratively to the Ionian Islands Perfecture. Kefalonia (38°12′44′′ N 20°32′00′′ E) occupies an area of 773 km2. Its capital city is Argostoli. According to the last census, 35.801 inhabitants were recorded living mainly in coastal settlements. Ithaca (38°23′59.28′′ N 20°41′21.11′′E) follows in size with 117 km2 surface area. Vathi is the capital city. In winter 3.084 residents are living on the island but in the summer the population is more than double. The local residents in the geopark ‘s area are mostly occupied with agriculture, fishery and tourism. Especially tourism plays an important role in the economic development of the area. Atokos (4,4 km2) and Arkoudi (4,275 km2) are small desolated islands north of Ithaca. Kefalonia includes four main peninsulas (Paliki, Erisos, Livatho and Atro). The mean altitude of the island is 358,5m. Approximately 37.5% is occupied by mountains, 42,5% is semi-mountainous and 20% is occupied by lowland areas. -
Wednesday 24 September 2014
THE GEODYNAMIC AND SEISMOTECTONIC SETTING OF CEPHALONIA (IONIAN SEA, WESTERN GREECE) AS FACTOR CONTROLLING THE DISTRIBUTION OF EARTHQUAKE ENVIRONMENTAL EFFECTS AND STRUCTURAL DAMAGE INDUCED BY THE EARLY 2014 EARTHQUAKES (JANUARY 26th and FEBRUARY 3rd, Mw 6.0) by LEKKAS, E., MAVROULIS, S., ALEXOUDI, V. National and Kapodistrian University of Athens, School of Sciences, Faculty of Geology and Geoenvironment, Department of Dynamic Tectonic Applied Geology Cephalonia is the largest of the Ionian Islands in Western Greece and is located on the tectonic front of the Hellenic thrust and fold belt developed only a few km east of the Hellenic Trench representing an active plate boundary where the Eastern Mediterranean lithosphere is being subducted beneath the Aegean one. The subduction zone terminates against the Cephalonia Transform Fault Zone connecting the subduction boundary to the continental collision between the Apulian microplate and the Hellenic foreland and playing a significant role in the region's geodynamic complexity. Historical seismic data indicate that Cephalonia has been repeatedly struck by moderate and strong, shallow earthquakes producing large seismic intensities and causing a large number of human casualties and great economic losses. One more episode in the geodynamic evolution of the island is the early 2014 earthquake sequence comprising two main shocks with the same magnitude (Mw 6.0) occurring successively in short time (January 26th and February 3rd) and space (neotectonic macrostructure of Paliki peninsula in the western part of Cephalonia). According to geological data collected in the field during our reconnaissance immediately after both earthquakes, it is concluded that each earthquake was induced by the rupture of a different pre-existing active fault zone located in Paliki peninsula. -
(Apulia, Italy) Threatened by Xylella Fastidiosa Subsp. Pauca: a Working Possibility of Restoration
sustainability Perspective The Multi-Millennial Olive Agroecosystem of Salento (Apulia, Italy) Threatened by Xylella Fastidiosa Subsp. Pauca: A Working Possibility of Restoration Marco Scortichini CREA-Council for Agricultural Research and Economics, Research Centre for Olive, Fruit and Citrus Crops, Via di Fioranello 52, I-00134 Roma, Italy; [email protected] Received: 3 July 2020; Accepted: 12 August 2020; Published: 19 August 2020 Abstract: In Salento, the olive agro-ecosystem has lasted more than 4000 years, and represents an invaluable local heritage for landscape, trade, and social traditions. The quarantine bacterium Xylella fastidiosa subsp. pauca was introduced in the area from abroad and has been widely threatening olive groves in the area. The successful eradication of quarantine phytopathogens requires a prompt identification of the causative agent at the new site, a restricted infected area, a highly effective local organization for crop uprooting and biological features of the micro-organism that would guarantee its complete elimination. However, at the time of the first record, these criteria were not met. Interdisciplinary studies showed that a zinc-copper-citric acid biocomplex allowed a consistent reduction of field symptoms and pathogen cell concentration within infected olive trees. In this perspective article, it is briefly described the implementation of control strategies in some olive farms of Salento. The protocol includes spray treatment with the biocomplex during spring and summer, regular pruning of the trees and mowing of soil between February and April to reduce the juvenile of the insect vector(s). Thus far, more than 500 ha have begun to follow this eco-friendly strategy within the “infected” and “containment” areas of Salento. -
Central Balkans Cradle of Aegean Culture
ANTONIJE SHKOKLJEV SLAVE NIKOLOVSKI - KATIN PREHISTORY CENTRAL BALKANS CRADLE OF AEGEAN CULTURE Prehistory - Central Balkans Cradle of Aegean culture By Antonije Shkokljev Slave Nikolovski – Katin Translated from Macedonian to English and edited By Risto Stefov Prehistory - Central Balkans Cradle of Aegean culture Published by: Risto Stefov Publications [email protected] Toronto, Canada All rights reserved. No part of this book may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording or by any information storage and retrieval system without written consent from the author, except for the inclusion of brief and documented quotations in a review. Copyright 2013 by Antonije Shkokljev, Slave Nikolovski – Katin & Risto Stefov e-book edition 2 Index Index........................................................................................................3 COMMON HISTORY AND FUTURE ..................................................5 I - GEOGRAPHICAL CONFIGURATION OF THE BALKANS.........8 II - ARCHAEOLOGICAL DISCOVERIES .........................................10 III - EPISTEMOLOGY OF THE PANNONIAN ONOMASTICS.......11 IV - DEVELOPMENT OF PALEOGRAPHY IN THE BALKANS....33 V – THRACE ........................................................................................37 VI – PREHISTORIC MACEDONIA....................................................41 VII - THESSALY - PREHISTORIC AEOLIA.....................................62 VIII – EPIRUS – PELASGIAN TESPROTIA......................................69 -
© Hachette Tourisme 2015 TABLE DES MATIÈRES ◗ Attention ! Les Îles Grecques Et La Crète Font L’Objet De Guides À Part
© Hachette Tourisme2015 © Hachette Tourisme 2015 TABLE DES MATIÈRES ◗ Attention ! Les îles grecques et la Crète font l’objet de guides à part. LES QUESTIONS QU’ON SE POSE LE PLUS SOUVENT ...................... 10 LES COUPS DE CŒUR DU ROUTARD .................................................. 11 ITINÉRAIRES CONSEILLÉS .................................................................... 13 COMMENT Y ALLER ? G EN AVION ....................................... 14 G EN VOITURE ................................... 32 G LES ORGANISMES G EN BATEAU .................................... 32 DE VOYAGES ................................. 18 G UNITAID .......................................... 33 G EN TRAIN ....................................... 30 QUITTER LA GRÈCE G EN AVION ....................................... 34 G PAR VOIE MARITIME G EN TRAIN ....................................... 34 ET TERRESTRE ............................. 34 GRÈCE CONTINENTALE UTILE G ABC DE LA GRÈCE ........................ 35 G LANGUE ......................................... 49 G AVANT LE DÉPART ........................ 35 G LIVRES DE ROUTE ........................ 54 G ARGENT, BANQUES, CHANGE ..... 39 G MUSÉES ET SITES G ACHATS .......................................... 40 ARCHÉOLOGIQUES ...................... 57 G AVENTURE, SPORT, NATURE ....... 41 G PLAGES .......................................... 58 G BUDGET ......................................... 41 G POLICE TOURISTIQUE ................. 58 G CLIMAT ........................................... 44 G POSTE ........................................... -
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Bulletin of the Geological Society of Greece Vol. 43, 2010 Contents Geological Society of Greece Geological Society of Greece https://doi.org/ Copyright © 2017 Geological Society of Greece Geological Society of Greece To cite this article: Geological Society of Greece, G. S. o. G. (2010). Contents. Bulletin of the Geological Society of Greece, 43(1), xxi-xxvii. Retrieved from http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 30/09/2021 08:26:55 | ΠΕΡΙΕΧΟΜΕΝΑ / CONTENTS = ΤΟΜΟΣ 1 / VOLUME 1 Εναρκτήρια Ομιλία / Οpening Lectures Κεντρικές και Θεματικές Ομιλίες / Special and Keynote Lectures Γενική και Τεκτονική Γεωλογία / General and Structural Geology Νεοτεκτονική και Γεωμορφολογία / Neotectonics and Geomorphology ΕΝΑΡΚΤΗΡΙΑ ΟΜΙΛΙΑ / OPENING LECTURE Zerefos C.S.: The “Anthropocene” in the Mediterranean ............................................................................................................ 2 ΚΕΝΤΡΙΚΕΣ ΟΜΙΛΙΕΣ / SPECIAL LECTURES Foscolos, A.E.: Climatic Changes: Anthropogenic Influence or Naturally Induced Phenomenon ........................ 8 Makris, J.: Geophysical studies and tectonism of the Hellenides ........................................................................................ 32 Papazachos, B.C., Karakaisis, G.F., Papazachos, C.B., Scordilis E.M.: Intermediate Term Earthquake Prediction Based on Interevent Times of Mainshocks and on Seismic Triggering .................... 46 Rausch, R., Schüth, C., Kallioras, A.: Groundwater Resources Management in Arid Countries ..................... 69 ΘΕΜΑΤΙΚΕΣ -
Ionian Sea, Greece)
EGU21-15736 https://doi.org/10.5194/egusphere-egu21-15736 EGU General Assembly 2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Upper-plate structural controls on the segmentation of the Kefalonia Fault (Ionian Sea, Greece) Emmanuel Skourtsos, Haralambos Kranis, Spyridon Mavroulis, and Efthimios Lekkas National and Kapodistrian University of Athens, Geology & Geoenvironment, Dynamic, Tectonic & Applied Geology, Athens, Greece ([email protected]) The NNE-SSW, right-lateral Kefalonia Transform Fault (KTF) marks the western termination of the subducting Hellenic slab, which is a part of the oceanic remnant of the African plate. The inception of the KTF, described as a STEP fault, is placed in the Pliocene. KTF is considered to be the most active earthquake source in the Eastern Mediterranean. During the last two decades, four significant earthquakes (M>6.0) have been associated with the KTF. These events are attributed to the reactivation of different segments of the KTF, which are (from North to South) the North Lefkada, South Lefkada, Fiskardo, Paliki and Zakynthos segments: the North Lefkada segment ruptured in the 2003 earthquake, the 2014 Kefalonia events are associated with the Paliki segment and the 2015 Lefkada earthquake with the South Lefkada (and possibly the Fiskardo) segments. The upper plate structure in the islands of Lefkada and Kefalonia is characterized by the Ionian Unit, thrusted over the Paxi (or Pre-Apulian) Unit. The Ionian Thrust, which brings the Ionian over the Paxi Unit, is a main upper-plate NNW-SSE, NE-dipping structure. It runs through the island of Lefkada, to be mapped onshore again at the western coast of Ithaki and at SE Kefalonia. -
Apulia a Journey Across All Seasons
Apulia A Journey across All Seasons Pocket Guide Mario Adda Editore Regione Puglia AreA Politiche Per lA Promozione del territorio, dei sAPeri e dei tAlenti Servizio Turismo – Corso Sonnino, 177 – cap 70121 Bari Tel. +39 080.5404765 – Fax +39 080.5404721 e-mail: [email protected] www.viaggiareinpuglia.it Text: Stefania Mola Translation: Christina Jenkner Photographs: Nicola Amato and Sergio Leonardi Drawings: Saverio Romito Layout: Vincenzo Valerio ISBN 9788880829362 © Copyright 2011 Mario Adda Editore via Tanzi, 59 - Bari Tel. e fax +39 080 5539502 www.addaeditore.it [email protected] Contents A Journey across All Seasons ....................................................pag. 7 A History ............................................................................................ 9 Buried Treasures ....................................................................................... 11 Taranto’s Treasure ........................................................................ 12 Egnazia ....................................................................................... 12 The Bronzes of Brindisi ............................................................... 13 The Vases of Ruvo ....................................................................... 13 Between Legend and Reality on the Hill of Cannae ....................... 14 Ostuni – Pre-Classical Civilizations ............................................... 14 Caves and Prayers ....................................................................... -
Apulia Agro-Biodiversity Between Rediscovery and Conservation: the Case of the «Salento Km0» Network
Central European Journal of Geography and Sustainable Development 2021, Volume 3, Issue 1, Pages: 49-59 ISSN 2668-4322, ISSN-L 2668-4322 https://doi.org/10.47246/CEJGSD.2021.3.1.4 Apulia agro-biodiversity between rediscovery and conservation: the case of the «Salento km0» network Sara Nocco,* Department of History Society and Human Studies, University of Salento, Complesso Studium 2000, Ed. 5 - Via di Valesio, 73100 Lecce, Italy [email protected] Received: 31 March 2021; Revised: 20 May 2021; Accepted: 11 June 2021; Published online: 29 June 2021 __________________________________________________________________________________________________________________________ Abstract: Green Revolution and the birth of the current global economic system had two opposite, subsequent effects. If, initially, they led to processes of crop homogenization, seasonal adjustment, homogenization of the landscape and markets standardization, they have subsequently pushed local communities towards a recovery of endemic biodiversity at risk of extinction because of such planetary processes, as well as a fundamental element in terms of local development, food security and sovereignty and reduction of environmental impacts. Starting from these instances of recovery and protection, which are increasingly taking place in Apulia, this work will examine both projects created "from above" and initiatives "from below", being the latter the result of a new consciousness that renews social cohesion and gives new value to the territorial milieu. In this regard, the case of the «Salento km0» network will be examined: born in 2011 and now made up of 61 local subjects including producers, restaurateurs, associations, ethical purchasing groups and traditional stores, which represent a key symbol of a territory that resists and a population that has chosen to stay and innovate according to economic, social, cultural and environmental sustainability. -
Selido3 Part 1
ΔΕΛΤΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ Τόμος XLIII, Νο 3 BULLETIN OF THE GEOLOGICAL SOCIETY OF GREECE Volume XLIII, Νο 3 1 (3) ΕΙΚΟΝΑ ΕΞΩΦΥΛΛΟΥ - COVER PAGE Γενική άποψη της γέφυρας Ρίου-Αντιρρίου. Οι πυλώνες της γέφυρας διασκοπήθηκαν γεωφυ- σικά με χρήση ηχοβολιστή πλευρικής σάρωσης (EG&G 4100P και EG&G 272TD) με σκοπό την αποτύπωση του πυθμένα στην περιοχή του έργου, όσο και των βάθρων των πυλώνων. (Εργα- στήριο Θαλάσσιας Γεωλογίας & Φυσικής Ωκεανογραφίας, Πανεπιστήμιο Πατρών. Συλλογή και επεξεργασία: Δ.Χριστοδούλου, Η. Φακίρης). General view of the Rion-Antirion bridge, from a marine geophysical survey conducted by side scan sonar (EG&G 4100P and EG&G 272TD) in order to map the seafloor at the site of the construction (py- lons and piers) (Gallery of the Laboratory of Marine Geology and Physical Oceanography, University of Patras. Data acquisition and Processing: D. Christodoulou, E. Fakiris). ΔΕΛΤΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ Τόμος XLIII, Νο 3 BULLETIN OF THE GEOLOGICAL SOCIETY OF GREECE Volume XLIII, Νο 3 12o ΔΙΕΘΝΕΣ ΣΥΝΕΔΡΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ ΠΛΑΝHΤΗΣ ΓH: Γεωλογικές Διεργασίες και Βιώσιμη Ανάπτυξη 12th INTERNATIONAL CONGRESS OF THE GEOLOGICAL SOCIETY OF GREECE PLANET EARTH: Geological Processes and Sustainable Development ΠΑΤΡΑ / PATRAS 2010 ISSN 0438-9557 Copyright © από την Ελληνική Γεωλογική Εταιρία Copyright © by the Geological Society of Greece 12o ΔΙΕΘΝΕΣ ΣΥΝΕΔΡΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ ΠΛΑΝΗΤΗΣ ΓΗ: Γεωλογικές Διεργασίες και Βιώσιμη Ανάπτυξη Υπό την Αιγίδα του Υπουργείου Περιβάλλοντος, Ενέργειας και Κλιματικής Αλλαγής 12th INTERNATIONAL CONGRESS OF THE GEOLOGICAL SOCIETY OF GREECE PLANET EARTH: Geological Processes and Sustainable Development Under the Aegis of the Ministry of Environment, Energy and Climate Change ΠΡΑΚΤΙΚΑ / PROCEEDINGS ΕΠΙΜΕΛΕΙΑ ΕΚΔΟΣΗΣ EDITORS Γ.