Spatial Diversity of Cr Distribution in Soil and Groundwater Sites in Relation with Land Use Management in a Mediterranean Region: the Case of C
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ANCIENT EUBOEA: STUDIES IN THE HISTORY OF A GREEK ISLAND FROM EARLIEST TIMES TO 404 B.C. Item Type text; Dissertation-Reproduction (electronic) Authors Vedder, Richard Glen, 1950- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 11/10/2021 05:15:39 Link to Item http://hdl.handle.net/10150/290465 INFORMATION TO USERS This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. You will find a good image of the page in the adjacent frame. -
Sarakenos Cave in Boeotia, from Palaeo Lithic to The
Eura sian Pre history, 6 (1–2): 199–231. SARAKENOS CAVE IN BOEOTIA, FROM PALAEOLITHIC TO THE EARLY BRONZE AGE Adamantios Sampson1, Janusz K. Koz³owski2, Ma³gorzata Kaczanowska3, Anna Budek4, Adam Nadachowski5, 6, Teresa Tomek6 and Barbara Miêkina6 1 Aegean Uni ver sity Rhodes, De part ment of Med i ter ra nean Ar chae ol ogy, Demokratios Ave, Rhodes, Greece 2 In sti tute of Ar chae ol ogy, Jagiellonian Uni ver sity, ul. Go³êbia 11, 31-007 Kraków, Po land, [email protected] 3 Ar chae o log i cal Mu seum, ul. Senacka 3, Kraków, Po land 4 In sti tute of Geography and Spa tial Organization, Pol ish Acad emy of Sci ence, ul. Œw. Jana 22, 31-016 Kraków, Po land 5 Departament of Palaeozoology, Zoo log i cal In sti tute, Wroc³aw Uni ver sity, Sienkiewicza 21, 50-355 Wroc³aw, Po land 6 In sti tute of System at ics and Evo lu tion of An i mals, Pol ish Acad emy of Sci ences, ul. S³awkowska 17, 31-016 Kraków, Po land Ab stract Sarakenos Cave, oc cupied since the Late Palaeolithic, is of crucial im portance for the study of the Mesolithic/Neo- lithic inter face. There is a striking contrast between the isolated Mesolithic, partic u larly Late Mesolithic occu pa tions with flake technol ogy adapted to the lo cal bad quality raw mate ri als, and with subsis tence economy based on fowling and plant gather ing, also adapted to the lo cal envi ron men tal condi tions, and the Early Neolithic groups arriv ing some 120–140 ra- diocar bon years later, with im ported raw mate ri als, macroblade technol ogy and ani mal breeding. -
Geomorpology 2006 Nileas Graben
Geomorphology 76 (2006) 363–374 www.elsevier.com/locate/geomorph Transverse fault zones of subtle geomorphic signature in northern Evia island (central Greece extensional province): An introduction to the Quaternary Nileas graben ⁎ Nikolaos Palyvos a, , Ioannis Bantekas b, Haralambos Kranis b a Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna murata 605, 00143 Rome, Italy b Faculty of Geology, Dynamic, Tectonic and Applied Geology Department, Panepistimioupolis Zografou, 157 84, Athens, Greece Received 11 March 2004; received in revised form 29 September 2005; accepted 8 December 2005 Available online 20 January 2006 Abstract Reconnaissance level geomorphological observations in the northern part of Evia (Euboea) Island, suggest that a major topographic feature, the 17 km long and 15 km wide Nileas depression (NDpr), corresponds to a previously undetected graben structure, bounded by fault zones of ENE–WSW to NE–SW general strike. These fault zones have been active in the Quaternary, since they affect the Neogene deposits of the Limni–Histiaia basin. They strike transverse to the NW–SE active fault zones that bound northern Evia in the specific area and are characterised along most of their length by subtle geomorphic signatures in areas of extensive forest cover and poor exposure. The NDpr was formed during the Early–Middle Quaternary, after the deposition of the Neogene basin fill. During the Middle– Late Quaternary, the NW–SE fault zones that bound northern Evia have been the main active structures, truncating and uplifting the NDpr to a perched position in relation to the northern Gulf of Evia graben and the submarine basin on the Aegean side of the island. -
Transverse Fault Zones of Subtle Geomorphic Signature in Northern
Geomorphology 76 (2006) 363–374 www.elsevier.com/locate/geomorph Transverse fault zones of subtle geomorphic signature in northern Evia island (central Greece extensional province): An introduction to the Quaternary Nileas graben ⁎ Nikolaos Palyvos a, , Ioannis Bantekas b, Haralambos Kranis b a Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna murata 605, 00143 Rome, Italy b Faculty of Geology, Dynamic, Tectonic and Applied Geology Department, Panepistimioupolis Zografou, 157 84, Athens, Greece Received 11 March 2004; received in revised form 29 September 2005; accepted 8 December 2005 Available online 20 January 2006 Abstract Reconnaissance level geomorphological observations in the northern part of Evia (Euboea) Island, suggest that a major topographic feature, the 17 km long and 15 km wide Nileas depression (NDpr), corresponds to a previously undetected graben structure, bounded by fault zones of ENE–WSW to NE–SW general strike. These fault zones have been active in the Quaternary, since they affect the Neogene deposits of the Limni–Histiaia basin. They strike transverse to the NW–SE active fault zones that bound northern Evia in the specific area and are characterised along most of their length by subtle geomorphic signatures in areas of extensive forest cover and poor exposure. The NDpr was formed during the Early–Middle Quaternary, after the deposition of the Neogene basin fill. During the Middle– Late Quaternary, the NW–SE fault zones that bound northern Evia have been the main active structures, truncating and uplifting the NDpr to a perched position in relation to the northern Gulf of Evia graben and the submarine basin on the Aegean side of the island. -
Euboea During the Neolithic Period: a Review of the Evidence
Euboea during the Neolithic period: A review of the evidence Vagia MASTROGIANNOPOULOU Adamantios SAMPSON Περίληψη Η Εύβοια αποτελεί μια ειδική περίπτωση της Νεολιθικής περιόδου στην Ελλάδα λόγω της γεωγραφικής της θέσης και των αρχαιολογικών καταγραφών που αφορούν σε ολόκληρη τη Νεολιθική περίοδο. Μια αναθεώρηση των καταγραφών σχετικά με τη Νεολιθική περίοδο στην Εύβοια συμβάλλει στη συζήτηση για τη Νεολιθική περίοδο στην Ελλάδα με δύο τρόπους: αποκαλύπτει τις διασυνδέσεις της ηπειρωτικής χώρας με τα νησιά του Αιγαίου και της νότιας με τη βόρεια ηπειρωτική χώρα. Σε αυτό το άρθρο εξετάζονται οι μεθοδολογικοί περιορισμοί της ‘περιφερειακής μελέτης’ και ο διαχωρισμός του ‘Αιγαίου’ με την ‘ηπειρωτική χώρα’ κατά τη Νεολιθική περίοδο. Εντοπίζοντας το χωρικό και χρονικό πλαίσιο της Εύβοιας, είναι επίσης εφικτή μια περιεκτική αναφορά της προϊστορίας της δεδομένων των νέων ανακαλύψεων που έχουν γίνει στο νησί και στην περιφέρειά του. Introduction Recently, research on the Greek Neolithic has gained momentum, with specialists isolating so- cio-cultural regions—such as Thessaly, the Cyclades and southern Greece, and Crete being considered ‘isolated’—or engaging in large-scale syntheses.1 Central Greece is overlooked both in terms of the areas to its north and to its south. Moreover, this regional segmentation has established an even more important distinction—that is, the ‘continental’ and the ‘coastal/ insular’ Neolithic. The main goal of this paper is to incorporate the Neolithic record of Euboea into this framework and also to demonstrate that the aforementioned methodological framework should always be consid- ered tentatively: Euboea is perhaps the most characteristic counter-example, as it belonged both to the Boeotian, hence continental, and the insular Neolithic. -
Ausgabe 2-2016 Privatpersonen in Hamburg, Schleswig-Holstein, Handels- Und Handwerkskammer, Diplomatische Und Mecklenburg-Vorpommern Und Niedersachsen
Das Magazin MichelBlick wird kostenlos verteilt an: konsularische Vertretungen, Landesvertretung Ham- Tourismuszentren, Theater, Museen, Galerien, Universi- burg, Berlin, Hotels, Restaurants, Werbeträger und tätsbibliotheken, Behörden, Wirtschaftsverbände, Ausgabe 2-2016 Privatpersonen in Hamburg, Schleswig-Holstein, Handels- und Handwerkskammer, diplomatische und Mecklenburg-Vorpommern und Niedersachsen Die Hauptverwaltung der Deutschen Bundesbank in Hamburg, Mecklenburg-Vorpommern und Schleswig-Holstein Seite 6 residual aus eigener Kraft an die griechischen Küsten Elementarem wie ausreichend Fingerab- geschafft haben. In Griechenland lautet druck-Scannern fehlt. Die Scanner sind Erste Anlaufstellen residual 2 Service - Erste Anlaufstellen 3 Kolumne von Knut Fleckenstein, der einheitliche Tenor auf die Frage nach eines der wichtigsten Arbeitsinstrumente, Polizei 110 Mitglied des Europäischen Parlaments der Grenzsicherung, dass nur die türkische denn 80 Prozent der Flüchtlinge kommen Feuerwehr und Rettungsdienst 112 4 Zu Gast beim MichelBlick: Seite dies ausreichend leisten könne. ohne Pass - sei es, weil sie ihn auf der Reise Krankenwagen 192 19 Peter Griep, Präsident, Hauptverwaltung der verloren haben oder sei es, weil sie sich Polizeikommissariat 14 / Neustadt 42 86-5 14 10 Deutschen Bundesbank in Hamburg, Mecklenburg- Kürzlich habe ich in Athen im Namen des Vorpommern und Schleswig-Holstein nicht zu erkennen geben wollen. 50 % aller ASBs fünf Krankenwagen für die Flücht- Aids-Seelsorge 280 44 62 6 Portrait der Hauptverwaltung der Deutschen Menschen, die zurzeit in Griechenland lingsarbeit in der Nordägäis und an der Aids-Hilfe 94 11 Bundesbank in Hamburg, Mecklenburg-Vorpom- anlanden sind Nordafrikaner. Grund dafür mern und Schleswig-Holstein mazedonischen Grenze übergeben. Allgemeines Krankenhaus St. Georg 28 90-11 ist die Visafreiheit der Türkei mit den Ambulanz 31 28 51 10 Uni Hamburg baut internationales Apartmenthaus Flüchtlingskrise: Fraktionsübergreifend habe ich mich mit Maghreb-Staaten. -
Assessment of Neotectonic Landscape Deformation in Evia Island, Greece, Using GIS-Based Multi-Criteria Analysis
International Journal of Geo-Information Article Assessment of Neotectonic Landscape Deformation in Evia Island, Greece, Using GIS-Based Multi-Criteria Analysis Kanella Valkanou 1,* , Efthimios Karymbalis 1 , Dimitris Papanastassiou 2, Mauro Soldati 3 , Christos Chalkias 1 and Kalliopi Gaki-Papanastassiou 4 1 Department of Geography, Harokopio University, GR-17671 Athens, Greece; [email protected] (E.K.); [email protected] (C.C.) 2 Institute of Geodynamics, National Observatory of Athens, GR-11810 Athens, Greece; [email protected] 3 Department of Chemical and Geological Sciences, University of Modena and Reggio Emilia, 41125 Modena, Italy; [email protected] 4 Department of Geography and Climatology, Faulty of Geology and Geoenvironment, University of Athens, GR-15784 Athens, Greece; [email protected] * Correspondence: [email protected] Abstract: This study deals with the assessment and mapping of neotectonic landscape deformation in the northern part of the Evia Island (Central Greece). Multi-Criteria Decision Analysis (MCDA) utilizing Analytic Hierarchy Process (AHP) and Weighted Linear Combination (WLC) procedures were conducted for the calculation of the Neotectonic Landscape Deformation Index (NLDI). The study is based on the combination of morphotectonic, geomorphological and geological parameters. The GIS-based spatial MCDA led to the classification of the study area into five classes of neotectonic deformation (from very low to very high) and to a neotectonic deformation map. The results were Citation: Valkanou, K.; Karymbalis, compared with the outputs of a relative tectonic activity classification approach based on quantitative E.; Papanastassiou, D.; Soldati, M.; geomorphic analysis at a regional scale, including site-specific field observations. Areas of high Chalkias, C.; Gaki-Papanastassiou, K. -
U-Pb and Ar-Ar Geochronological Data from the Pelagonian Basement in Evia (Greece) : Geodynamic Implications for the Evolution of Paleotethys
U-Pb and Ar-Ar geochronological data from the Pelagonian basement in Evia (Greece) : geodynamic implications for the evolution of Paleotethys Autor(en): Vavassis, I. / Bono, A. de / Stampfli, G.M. Objekttyp: Article Zeitschrift: Schweizerische mineralogische und petrographische Mitteilungen = Bulletin suisse de minéralogie et pétrographie Band (Jahr): 80 (2000) Heft 1 PDF erstellt am: 06.10.2021 Persistenter Link: http://doi.org/10.5169/seals-60948 Nutzungsbedingungen Die ETH-Bibliothek ist Anbieterin der digitalisierten Zeitschriften. Sie besitzt keine Urheberrechte an den Inhalten der Zeitschriften. Die Rechte liegen in der Regel bei den Herausgebern. Die auf der Plattform e-periodica veröffentlichten Dokumente stehen für nicht-kommerzielle Zwecke in Lehre und Forschung sowie für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und den korrekten Herkunftsbezeichnungen weitergegeben werden. Das Veröffentlichen von Bildern in Print- und Online-Publikationen ist nur mit vorheriger Genehmigung der Rechteinhaber erlaubt. Die systematische Speicherung von Teilen des elektronischen Angebots auf anderen Servern bedarf ebenfalls des schriftlichen Einverständnisses der Rechteinhaber. Haftungsausschluss Alle Angaben erfolgen ohne Gewähr für Vollständigkeit oder Richtigkeit. Es wird keine Haftung übernommen für Schäden durch die Verwendung von Informationen aus diesem Online-Angebot oder durch das Fehlen von Informationen. Dies gilt auch für Inhalte Dritter, die über dieses Angebot zugänglich sind. Ein Dienst der ETH-Bibliothek ETH Zürich, Rämistrasse 101, 8092 Zürich, Schweiz, www.library.ethz.ch http://www.e-periodica.ch SCHWEIZ. MINERAL. PETROGR. MIEL 80. 21-48, 2000 U-Pb and Ar-Ar geochronological data from the Pelagonian basement in Evia (Greece): geodynamic implications for the evolution of Paleotethys b\ I. -
The Cr(VI) Stability in Contaminated Coastal Groundwater: Salinity As a Driving Force
minerals Review The Cr(VI) Stability in Contaminated Coastal Groundwater: Salinity as a Driving Force Ioannis-Porfyrios D. Eliopoulos 1, George D. Eliopoulos 2 and Maria Economou-Eliopoulos 3,* 1 Department of Pharmacy, School of Health Sciences, National University of Athens, GR-15771 Zografou, Greece; [email protected] 2 Department of Chemistry, University of Crete, GR-70013 Heraklion, Greece; [email protected] 3 Department of Geology and Geoenvironment, National University of Athens, GR-15784 Athens, Greece * Correspondence: [email protected] Abstract: Chromium concentrations in seawater are less than 0.5 µg/L, but the Cr(VI) in contaminated coastal groundwater affected by Cr-bearing rocks/ores and/or human activities, coupled with the intrusion of seawater may reach values of hundreds of µg/L. A potential explanation for the stability of the harmful Cr(VI) in contaminated coastal aquifers is still unexplored. The present study is an overview of new and literature data on the composition of coastal groundwater and seawater, aiming to provide potential relationships between Cr(VI) with major components in seawater and explain the elevated Cr(VI) concentrations. It is known that the oxidation of Cr(III) to Cr(VI) and the subsequent back-reduction of Cr(VI) processes, during the transport of the mobilized Cr(VI) in various aquifers, facilitate the natural attenuation process of Cr(VI). Moreover, the presented positive trend between B and Cr(VI) and negative trend between δ53Cr values and B concentration may suggest that seawater components significantly inhibit the Cr(VI) reduction into Cr(III), and provide insights on the role − of the borate, [B(OH)4] ions, a potential buffer, on the stability of Cr(VI) in coastal groundwater. -
Project Screens
AD671 DESIGN: STUDIO PROJECT 4: FINAL PORTFOLIO SUBMISSION FINAL PROPOSAL: EVIA’S STONE AND STORIES STUDENT NAME: ENRICO FOCARDI STUDENT NO. 18841734 TUTOR NAME: STEPHEN RYAN CONTENTS: Page 3- 9: SITE Page 10- 27: 1ST PROGRAMME Page 28 - 50: 2ND PROGRAMME Page 51: PRECEDENCE STUDY Page 52 - 58: MORE DEVELOPING Page 59 - 79: FINAL DECISIONS/ PLANS/ SECTIONS/ RENDERS Page 80: SUMMARY LOCATING THE ISLAND MUNICIPALITY LOCAL - SITE SITE Euboea or Evia is the second-largest Greek island in area and population, The site is located in a Municipality by the name of Dirfys Messapia. It is mainly located in The site is located in a densely vegetated area at an elevation of 250m above after Crete. In general outline it is a long and narrow island; it is about 180 km the central part of the island with a total area of 800km². The municipality borders to the sea level. The sea can be viewed from site if facing anywhere from North East (110 mi) long, and varies in breadth from 50 km (31 mi) to 6 km (3.7 mi). Its northwest with the Municipality of Mantoudi Limni Agia Anna , to the south with to West. The largest village close to site is Politika - Πολιτικά - (4km away) - as geographic orientation is from northwest to southeast, and it is traversed the Municipality of Chalkida , to the southeast with the Municipality of Eretria and to the shown on the site map above. The last recorded population was taken in 2011 throughout its length by a mountain range. Euboea was believed to have northeast with the Municipality of Kymi Aliveri. -
Contamination of the Soil–Groundwater–Crop System: Environmental Risk and Opportunities
minerals Review Contamination of the Soil–Groundwater–Crop System: Environmental Risk and Opportunities Maria Economou-Eliopoulos * and Ifigeneia Megremi Department of Geology and Geoenvironment, National University of Athens, GR-15784 Athens, Greece; [email protected] * Correspondence: [email protected] Abstract: The increasing development of industries, resulting in a large volume of mining, smelting, and combustion wastes, and intense agricultural activities, due to demand for food and energy, have caused environmental hazards for food quality and ecosystems. This is a review on the contamination of the soil–groundwater–crop system and a potential reduction of the contamination by a gradual shift towards green economy within the European Union and on a worldwide scale. Available mineralogical and geochemical features from contaminated Neogene basins have shown a diversity in the contamination sources for soil and groundwater, and highlighted the need to define the contamination sources, hot spots, degree/extent of contamination, and provide ways to restrict the transfer of heavy metals/metalloids into the food chain, without the reduction of the agricultural and industrial production. Among harmful elements for human health and ecosystems, the contamination of groundwater (thousands of µg/L Cr(VI)) by industrial activities in many European countries is of particular attention. Although Cr(VI) can be reduced to Cr(III) and be completely attenuated in nature under appropriate pH and Eh conditions, the contamination by Cr(VI) of coastal groundwater Citation: Economou-Eliopoulos, M.; affected by the intrusion of seawater often remains at the hundreds µg/L level. A positive trend Megremi, I. Contamination of the − between B and Cr(VI) may provide insights on the role of the borate [B(OH)4] ions, a potential Soil–Groundwater–Crop System: buffer, on the stability of Cr(VI) in coastal groundwater. -
Articulating Landscapes in Central Greece
2 Articulating Landscapes in Central Greece Archaeology in essence then is the discipline with the theory and practice for the recovery of unobservable hominid behaviour patterns from indirect traces in bad samples. —David Clarke, “Archaeology: The Loss of Innocence” Archaeologists necessarily work with bad data derived from a variety of incon- sistent sources. Moreover, these data are not always well suited to answering the social questions of greatest interest to our discipline. A certain amount of model building is therefore necessary to fill gaps and make connections between what we can know—the hard facts of archaeological materials—and what we can infer based on these facts. This chapter presents the baseline evidence and the models drawn on in the analysis of landscape, interaction, and complexity that forms the core of this book—that is, the archaeological remains of human activity, the ques- tion of how they are distributed across the Greek landscape, and the methods used to articulate relationships between places in geographical space. I begin with some overall characterization of the archaeological dataset compiled and parsed from a number of different types of fieldwork, reports, and publications. I next provide some contextual description of the geography and history of research for each of the regions under study. Finally, I outline the analytical framework of articulat- ing relations between communities and within landscapes and regions—spatial approaches to modeling connectivity and territory. THE BASELINE EVIDENCE: SITES, COMMUNITIES, AND REGIONAL DATASETS The dataset that forms the core of this analysis is comprised of about 400 archaeo- logical sites, drawn from various types of archaeological survey and excavation data (map 3; see also appendix for a complete list and locations of all sites used in this study).