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A New Consideration About the Almopia-Paikon Boundary Based on the Geological Mapping in the Area of Nerostoma-Lakka (Central Macedonia, Greece)
Δελτίο της Ελληνικής Γεωλογικής Εταιρίας τομ. ΧΧΧΧ, Bulletin of the Geological Society of Greece vol. XXXX, 2007 2007 Proceedings of the 11th International Congress, Athens, May, Πρακτικά 11ou Διεθνούς Συνεδρίου, Αθήνα, Μάιος 2007 2007 A NEW CONSIDERATION ABOUT THE ALMOPIA-PAIKON BOUNDARY BASED ON THE GEOLOGICAL MAPPING IN THE AREA OF NEROSTOMA-LAKKA (CENTRAL MACEDONIA, GREECE) Tranos M. D. \ Plougarlis A. P.!, and Mountrakis D. Μ.l 1 Aristotle University of Thessaloniki, School of Geology, Department of Geology, GR-54124 Thessaloniki, Greece, [email protected], [email protected], [email protected] Abstract Geological mapping along the boundary of Almopia and Paikon zone in the 'Nerostoma' region, NNW of Lakka village defines mafic volcanogenic rocL·, meta-pelites and radiolarites, thick-bedded to massive micritic limestones and flysch meta-sediments that dip mainly towards SW. Middle-Late Cretaceous fossiliferous limestones overlie unconformably the flysch meta-sediments and are characterised only by a primary foliation SO that dips at shallow angles to the NNW-N. Secondary foliations SI (sub-parallel to SO) and S2 are observed in the meta-clastic rocks. A Dl event caused Fl and progressively F2 folds to which S2 is the axial plane schistosity dipping to SW. This event which has not affected the fossiliferous limestones is related to an oblique convergence or inclined transpression during the Late Jurassic-Early Cretaceous. A D2 event dated in Early Tertiary caused an intense NE-thrusting and S-C cataclastic fabric defining top-to-the NE sense-of-shear. At many parts, the unconformity contact between the fossiliferous limestones and the underlying flysch is obliterated by this thrusting event. -
For Municipal Solid Waste Management in Greece
Journal of Open Innovation: Technology, Market, and Complexity Article Description and Economic Evaluation of a “Zero-Waste Mortar-Producing Process” for Municipal Solid Waste Management in Greece Alexandros Sikalidis 1,2 and Christina Emmanouil 3,* 1 Amsterdam Business School, Accounting Section, University of Amsterdam, 1012 WX Amsterdam, The Netherlands 2 Faculty of Economics, Business and Legal Studies, International Hellenic University, 57001 Thessaloniki, Greece 3 School of Spatial Planning and Development, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece * Correspondence: [email protected]; Tel.: +30-2310-995638 Received: 2 July 2019; Accepted: 19 July 2019; Published: 23 July 2019 Abstract: The constant increase of municipal solid wastes (MSW) as well as their daily management pose a major challenge to European countries. A significant percentage of MSW originates from household activities. In this study we calculate the costs of setting up and running a zero-waste mortar-producing (ZWMP) process utilizing MSW in Northern Greece. The process is based on a thermal co-processing of properly dried and processed MSW with raw materials (limestone, clay materials, silicates and iron oxides) needed for the production of clinker and consequently of mortar in accordance with the Greek Patent 1003333, which has been proven to be an environmentally friendly process. According to our estimations, the amount of MSW generated in Central Macedonia, Western Macedonia and Eastern Macedonia and Thrace regions, which is conservatively estimated at 1,270,000 t/y for the year 2020 if recycling schemes in Greece are not greatly ameliorated, may sustain six ZWMP plants while offering considerable environmental benefits. This work can be applied to many cities and areas, especially when their population generates MSW at the level of 200,000 t/y, hence requiring one ZWMP plant for processing. -
Cave Radon Exposure, Dose, Dynamics and Mitigation
Chris L. Waring, Stuart I. Hankin, Stephen B. Solomon, Stephen Long, Andrew Yule, Robert Blackley, Sylvester Werczynski, and Andrew C. Baker. Cave radon exposure, dose, dynamics and mitigation. Journal of Cave and Karst Studies, v. 83, no. 1, p. 1-19. DOI:10.4311/2019ES0124 CAVE RADON EXPOSURE, DOSE, DYNAMICS AND MITIGATION Chris L. Waring1, C, Stuart I. Hankin1, Stephen B. Solomon2, Stephen Long2, Andrew Yule2, Robert Blackley1, Sylvester Werczynski1, and Andrew C. Baker3 Abstract Many caves around the world have very high concentrations of naturally occurring 222Rn that may vary dramatically with seasonal and diurnal patterns. For most caves with a variable seasonal or diurnal pattern, 222Rn concentration is driven by bi-directional convective ventilation, which responds to external temperature contrast with cave temperature. Cavers and cave workers exposed to high 222Rn have an increased risk of contracting lung cancer. The International Commission on Radiological Protection (ICRP) has re-evaluated its estimates of lung cancer risk from inhalation of radon progeny (ICRP 115) and for cave workers the risk may now (ICRP 137) be 4–6 times higher than previously recognized. Cave Guides working underground in caves with annual average 222Rn activity 1,000 Bq m3 and default ICRP assumptions (2,000 workplace hours per year, equilibrium factor F 0.4, dose conversion factor DCF 14 µSv 3 1 1 d13 (kBq h m ) could now receive a dose of 20 mSv y . Using multiple gas tracers ( C CO2, Rn and N2O), linked weather, source gas flux chambers, and convective air flow measurements a previous study unequivocally identified the external soil above Chifley Cave as the source of cave222 Rn. -
CV Karkanas 2018.Pdf
PANAGIOTIS (TAKIS) KARKANAS CURRICULUM VITAE May 2018 Malcolm H. Wiener Laboratory for Archaeological Science American School of Classical Studies 54 Soudias, 10676 Athens, Greece Tel.: (30) 2130002400x224 Fax: (30) 2107294047 E-mail: [email protected] Personal Web Pages: https://www.researchgate.net/profile/Panagiotis_Karkanas https://ascsa.academia.edu/PanagiotisKarkanas EDUCATIONAL BACKGROUND 1994: Ph.D. in Geology (Specialty: mineralogy, petrology, geochemistry), Department of Geology, University of Athens. 1990: Postgraduate Seminar (300 hours) in Geology of sedimentary basin and energy resources. EU funded Research Seminar for Geologists, Department of Geology, University of Athens. 1986: B.Sc. in Geology, Department of Geology, University of Athens. AREAS OF INTEREST Geoarchaeology: site formation processes (stratigraphy, micromorphology, post-depositional chemical alterations) palaeoenvironmental reconstructions, paleoclimate, methods and techniques (dating, petrography, mineralogy, sedimentary analysis, provenance analysis). PROFESSIONAL APPOINTMENTS 2014-: Director, Malcolm H. Wiener Laboratory of Archaeological Science, American School of Classical Studies at Athens, Greece. 1994-2014: Senior Geologist, Ephoreia of Palaeoanthropology-Speleology (EPS), Ministry of Culture, Greece. 2004-2013: Adjunct Lecturer, Department of Geography, Harokopio University of Athens. OTHER PROFESSIONAL AND LABORATORY EXPERIENCE 1995-2003 (approx. one month per year): Visiting research scientist, Kimmel Center for Archaeological Sciences, -
Travertine Caves in Almopia, Greece
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/320310627 Travertine caves in Almopia, Greece Article in Cave and Karst Science · October 2017 CITATIONS READS 0 169 3 authors, including: Georgios Lazaridis Konstantinos Trimmis Aristotle University of Thessaloniki Cardiff University 29 PUBLICATIONS 47 CITATIONS 14 PUBLICATIONS 1 CITATION SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Using LEGO to explore Archaeology and acquire Modern Greek Vocabulary View project Exploring Archaeology in Museums through the 3E method View project All content following this page was uploaded by Konstantinos Trimmis on 10 October 2017. The user has requested enhancement of the downloaded file. Cave and Karst Science, Vol.44, No.2, (2017) 58–63 © British Cave Research Association 2017 Transactions of the British Cave Research Association ISSN 1356-191X Travertine caves in Almopia, Greece Georgios LAZARIDIS 1, Konstantinos P TRIMMIS 2 and Spyridoula PAPPA 3 1 Department of Geology, Laboratory of Geology and Palaeontology, Aristotle University of Thessaloniki, 54124, Thessaloniki, Greece. E-mail: [email protected] 2 Department of Archaeology and Conservation, Cardiff University, Cardiff, Wales, UK. E-mail: [email protected] 3 Department of Earth Sciences, The Natural History Museum, Cromwell Road, London, SW7 5BD, UK. E-mail: [email protected] Abstract: Seven caves have been explored and surveyed within two travertine terraces (Aspri Petra and Baina) in the Almopia region, Greece. The Aspri Petra terrace is less faulted than the Baina and the caves of each terrace demonstrate differences that could be related to the degree of faulting. -
The Carnivore Remains from the Sima De Los Huesos Middle Pleistocene Site
N. Garcia & The carnivore remains from the Sima de J. L. Arsuaga los Huesos Middle Pleistocene site Departamento de Paleontologia, (Sierra de Atapuerca, Spain) Facultad de Ciencias Geologicas, U.A. de Paleoantropologia & Instituto de View metadata, citation and similar papersRemain ats ocore.ac.ukf carnivores from the Sima de los Huesos sitebrought representin to you gby a t COREleast Geologia Economica, Universidad 158 adult individuals of a primitive (i.e., not very speleoid) form of Ursus Complutense de Madrid, Ciudad provided by Servicio de Coordinación de Bibliotecas de la... deningeri Von Reichenau 1906, have been recovered through the 1995 field Universitaria, 28040 Madrid, Spain season. These new finds extend our knowledge of this group in the Sierra de Atapuerca Middle Pleistocene. Material previously classified as Cuoninae T. Torres indet. is now assigned to Canis lupus and a third metatarsal assigned in 1987 to Departamento de Ingenieria Geoldgica, Panthera cf. gombaszoegensis, is in our opinion only attributable to Panthera sp. The Escuela Tecnica Superior de Ingenieros family Mustelidae is added to the faunal list and includes Maites sp. and a de Minas, Universidad Politecnica smaller species. The presence of Panthera leo cf. fossilis, Lynxpardina spelaea and de Madrid, Rios Rosas 21, Fells silvestris, is confirmed. The presence of a not very speloid Ursus deningeri, 28003 Madrid, Spain together with the rest of the carnivore assemblage, points to a not very late Middle Pleistocene age, i.e., oxygen isotope stage 7 or older. Relative frequencies of skeletal elements for the bear and fox samples are without major biases. The age structure of the bear sample, based on dental wear stages, does not follow the typical hibernation mortality profile and resembles a cata strophic profile. -
Isotopic Analysis of the Ecology of Herbivores and Carnivores from the Middle Pleistocene Deposits of the Sierra De Atapuerca, Northern Spain N
Isotopic analysis of the ecology of herbivores and carnivores from the Middle Pleistocene deposits of the Sierra De Atapuerca, northern Spain N. Garcia Gar~ia~,~,",R.S. FeranecC.*, J.L. ~rsua~a~,~,J.M. BermGdez de Castrod, E. Carbonelle 'Deportomento de Poleontologio, Focultod de Ciencior Geoldgicor, Univerridod Complutense de Modrid, Ciudod Univerritorio, 28040 Modrid, Spoin Centlo Mkt0 (UCM-ISUII) de Evolucidn y Comportomiento Humonor, CfSinerio Delgodo 4, Pob. 14, 29029 Modrid, Spoin 'New York Stote Museum. 3140 Culturol Education Center. Albonv. NY 12230. USA *centre Nocionol de Invertigoci6n robre 10 Evoluci6n Humono -?M, Avda de ia Pog 28, 09004 Burger, Spoin eInstitut Cotold de Poleoecologio Humono i Evoluci6 Sociol (IPHES), C/ Erconodor, r/n 43003 Torrogono, Spoin ABSTRACT Carbon and oxygen isotope values reveal resource partitioning among the large mammal fauna from three contemporaneous Middle Pleistocene hominid-bearing localities within the Sierra de Atapuerca (northern Spain). Carbon isotope values sampled from the tooth enamel of fauna present during Ata- ouerca Faunal Unit 6 show that a C?-dominated ecosvstem surrounded the area where fossils were preserved during this time. For the herbivores, Fallow deer isotope values are significantly different from Red deer and horses and show that this species did not forage in open environments at this locality. Red Keywords: deer and horses show similar feedine strateeies with less neeative carbon values imolvine use of more C-l3 Diet Ecology Enamel that this species is herbivorous. Special metabolic mechanisms involved in hibernation in U deningeri Mammal might also have influenced its isotope values. The carbon isotope values of remaining carnivores were 0-18 similar and suggest that each was typically a generalist carnivore, eating a wide variety of prey items. -
UCLA Electronic Theses and Dissertations
UCLA UCLA Electronic Theses and Dissertations Title Cremation, Society, and Landscape in the North Aegean, 6000-700 BCE Permalink https://escholarship.org/uc/item/8588693d Author Kontonicolas, MaryAnn Emilia Publication Date 2018 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California UNIVERSITY OF CALIFORNIA Los Angeles Cremation, Society, and Landscape in the North Aegean, 6000 – 700 BCE A dissertation submitted in partial satisfaction of the requirements for the degree Doctor of Philosophy in Archaeology by MaryAnn Kontonicolas 2018 © Copyright by MaryAnn Kontonicolas 2018 ABSTRACT OF THE DISSERTATION Cremation, Society, and Landscape in the North Aegean, 6000 – 700 BCE by MaryAnn Kontonicolas Doctor of Philosophy in Archaeology University of California, Los Angeles, 2018 Professor John K. Papadopoulos, Chair This research project examines the appearance and proliferation of some of the earliest cremation burials in Europe in the context of the prehistoric north Aegean. Using archaeological and osteological evidence from the region between the Pindos mountains and Evros river in northern Greece, this study examines the formation of death rituals, the role of landscape in the emergence of cemeteries, and expressions of social identities against the backdrop of diachronic change and synchronic variation. I draw on a rich and diverse record of mortuary practices to examine the co-existence of cremation and inhumation rites from the beginnings of farming in the Neolithic period -
Pleistocene Cave Hyenas in the Iberian Peninsula: New Insights from Los Aprendices Cave (Moncayo, Zaragoza)
Palaeontologia Electronica palaeo-electronica.org Pleistocene cave hyenas in the Iberian Peninsula: New insights from Los Aprendices cave (Moncayo, Zaragoza) Víctor Sauqué, Raquel Rabal-Garcés, Joan Madurell-Malaperia, Mario Gisbert, Samuel Zamora, Trinidad de Torres, José Eugenio Ortiz, and Gloria Cuenca-Bescós ABSTRACT A new Pleistocene paleontological site, Los Aprendices, located in the northwest- ern part of the Iberian Peninsula in the area of the Moncayo (Zaragoza) is presented. The layer with fossil remains has been dated by amino acid racemization to 143.8 ± 38.9 ka (earliest Late Pleistocene or latest Middle Pleistocene). Five mammal species have been identified in the assemblage: Crocuta spelaea (Goldfuss, 1823) Capra pyre- naica (Schinz, 1838), Lagomorpha indet, Arvicolidae indet and Galemys pyrenaicus (Geoffroy, 1811). The remains of C. spelaea represent a mostly complete skeleton in anatomical semi-connection. The hyena specimen represents the most complete skel- eton ever recovered in Iberia and one of the most complete remains in Europe. It has been compared anatomically and biometrically with both European cave hyenas and extant spotted hyenas. In addition, a taphonomic study has been carried out in order to understand the origin and preservation of these exceptional remains. The results sug- gest rapid burial with few scavenging modifications putatively produced by a medium sized carnivore. A review of the Pleistocene Iberian record of Crocuta spp. has been carried out, enabling us to establish one of the earliest records of C. spelaea in the recently discovered Los Aprendices cave, and also showing that the most extensive geographical distribution of this species occurred during the Late Pleistocene (MIS4- 2). -
Proceedings VOLUME 1
16th INTERNATIONAL CONGRESS OF SPELEOLOGY Proceedings VOLUME 1 Edited by Michal Filippi Pavel Bosák 16th INTERNATIONAL CONGRESS OF SPELEOLOGY Czech Republic, Brno July 21 –28, 2013 Proceedings VOLUME 1 Edited by Michal Filippi Pavel Bosák 2013 16th INTERNATIONAL CONGRESS OF SPELEOLOGY Czech Republic, Brno July 21 –28, 2013 Proceedings VOLUME 1 Produced by the Organizing Committee of the 16th International Congress of Speleology. Published by the Czech Speleological Society and the SPELEO2013 and in the co-operation with the International Union of Speleology. Design by M. Filippi and SAVIO, s.r.o. Layout by SAVIO, s.r.o. Printed in the Czech Republic by H.R.G. spol. s r.o. The contributions were not corrected from language point of view. Contributions express author(s) opinion. Recommended form of citation for this volume: Filippi M., Bosák P. (Eds), 2013. Proceedings of the 16th International Congress of Speleology, July 21–28, Brno. Volume 1, p. 453. Czech Speleological Society. Praha. ISBN 978-80-87857-07-6 KATALOGIZACE V KNIZE - NÁRODNÍ KNIHOVNA ČR © 2013 Czech Speleological Society, Praha, Czech Republic. International Congress of Speleology (16. : Brno, Česko) 16th International Congress of Speleology : Czech Republic, Individual authors retain their copyrights. All rights reserved. Brno July 21–28,2013 : proceedings. Volume 1 / edited by Michal Filippi, Pavel Bosák. -- [Prague] : Czech Speleological Society and No part of this work may be reproduced or transmitted in any the SPELEO2013 and in the co-operation with the International form or by any means, electronic or mechanical, including Union of Speleology, 2013 photocopying, recording, or any data storage or retrieval ISBN 978-80-87857-07-6 (brož.) system without the express written permission of the 551.44 * 551.435.8 * 902.035 * 551.44:592/599 * 502.171:574.4/.5 copyright owner. -
The GEOLOGY of ALMOPIA SPELEOPARK
Scientific Annals, School of Geology Special volume 98 27-31 Thessaloniki, 2006 Aristotle University of Thessaloniki (AUTH) THE GEOLOGY OF ALMOPIA SPELEOPARK George ElEftHEriadis1 Abstract: The Almopia Speleopark is located on the boundary of two geological zones: the Almopia (Axios) zone eastwards and the Pelagonian zone westwards. The Almopia zone in the area of study is comprised of metamorphic rocks (schists, marbles and cipolines), ophiolites, limestones and clastic formations whereas the Pelagonian zone consist of carbonate rocks of Triassic-Jurassic age, sediments of Upper Cretaceous age and flysch of Upper Maastrictian-Lower Paleocene. In the area there are also travertine deposits of signifi- cant quantity and excellent quality. The seismicity in the area can be considered as not significant. Key words: Almopia, Speleopark, geology, volcanology, seismicity. INTRODUCTION The Almopia area geotectonicaly belongs to the Almopia zone, which together with the Peonia and Paikon zones constitute the old Axios (Vardar) zone (Μercier, 1968). The Axios zone Kossmat,( 1924) is situated between the Pelagonian massif to the west and the Serbo-Macedonian massif to the east. The Almopia and Peonia zones, con- stituting the westernmost and easternmost parts of the Axios zone, respectively, were deep-water oceans sepa- rated by the shallow ocean of the Paikon zone, consisting of thick carbonate rocks of mainly Triassic to Cretaceous age.The Almopia zone is characterized by huge masses of ophiolites (Bebien et al., 1994). The Almopia zone was deformed during two oro- genic periods: the Upper Jurassic-Lower Cretaceous and the Upper Cretaceous-Middle Eocene. During the first period the Almopia ocean closed, the Almopia zone emerged temporary until the Middle-Upper Cretaceous transgression and the ophiolitic rocks overthrusted on the Pelagonian platform westwards (Μercier, 1968). -
Wetlands Management in Northern Greece: an Empirical Survey
water Article Wetlands Management in Northern Greece: An Empirical Survey Eleni Zafeiriou 1,* , Veronika Andrea 2 , Stilianos Tampakis 3 and Paraskevi Karanikola 2 1 Department of Agricultural Development, Democritus University of Thrace, GR68200 Orestiada, Greece 2 Department of Forestry and Management of the Environment and Natural Resources, Democritus University of Thrace, GR68200 Orestiada, Greece; [email protected] (V.A.); [email protected] (P.K.) 3 School of Forestry, Department of Forestry and Natural Environment, Faculty of Agriculture, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece; [email protected] * Correspondence: [email protected]; Tel.: +30-6932-627-501 Received: 29 September 2020; Accepted: 9 November 2020; Published: 13 November 2020 Abstract: Water management projects have an important role in regional environmental protection and socio-economic development. Environmental policies, strategies, and special measures are designed in order to balance the use and non-use values arising for the local communities. The region of Serres in Northern Greece hosts two wetland management projects—the artificial Lake Kerkini and the re-arrangement of Strymonas River. The case study aims to investigate the residents’ views and attitudes regarding these two water resources management projects, which significantly affect their socio-economic performance and produce several environmental impacts for the broader area. Simple random sampling was used and, by the application of reality and factor analyses along with the logit model support, significant insights were retrieved. The findings revealed that gender, age, education level, and marital status affect the residents’ perceived values for both projects and their contribution to local growth and could be utilized in policy making for the better organization of wetland management.