DOCSLIB.ORG

3. Case Studies and Practical Experiences Greece 3.1

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
3. Case Studies and Practical Experiences Greece 3.1 3. CASE STUDIES AND PRACTICAL EXPERIENCES GREECE 3.1. Sarigkiol basin 3.1.1 Vulnerability assessment 3.1.1.1 Short description Sarigkiol basin is located in the north­eastern part of Kozani Prefecture, Western Macedonia region, Greece, covering an area of 423 km 2. The mean altitude of the basin is about 952 m. The alluvial aquifer of the Sarigkiol basin covers an area of 60 km 2 and its maximum depth reach at 110 m below ground surface. In alluvial deposits a phreatic aquifer superimposed on successive confined aquifers is developed. Despite the documented heterogeneities however, it is suggested that on a regional scale a uniform aquifer may be considered. 3.1.1.2 Available data Data concerning required parameters were collected from previous studies, MSc and PhD thesis: a) Hydrogeological, hydrometeorologic and geological data. b) Drilling data including geological and hydrogeological information (depth and type of geological formations, aquifer, depth of unsaturated zone etc). c) Static water levels measurements d) Pumping test data to calculate the hydraulic parameters. The data collected are analytically presented in report on the Hydrometeorologic and geological data (Deliverable 3.1). 3.1.1.3 Results­ Elaboration of the vulnerability map Depth to groundwater (D) The water level map of the Sarigkiol basin was obtained from previous hydrogeological studies (Koumantakis 1999; Patsios, 2006). The depth to groundwater in the alluvial aquifer of Sarigkiol basin ranges from less than 7 to more than 75 m below ground surface (Fig. 1). Programme INTEREG IIIB ARCHIMED: WATER MAP Fig. 1: Depth to groundwater rating curve and water level sites position (above) and the depth to water table rating map (below). Net recharge (infiltration) (R) The variable R was calculated from rainfall data and the coefficients of infiltration of geological formations. The annual rainfall is 643 mm. Fig. 2: Net annual recharge rating curve (above) and the recharge rating map (below). Aquifer material or media (A) Aquifer media have been identified from the borehole data and 179 lithological profiles. Based on these profiles, the aquifer media was classified as: 1) Gravel, 2) Sand and Gravel, 3) Sandstone and conglomerate, 4) Sand, 5) Sand, gravel and clay, 6) Clay, sand and gravel. 1 Programme INTEREG IIIB ARCHIMED: WATER MAP Fig. 3: Aquifer media rating map. Soil media (S) The variable S (Soil type) was obtained from soil classification maps (IGME). The density of soil samples was 5 samples / Km 2 and the depth 0­30 cm from the ground surface. Based on results from soil analyses, the predominant soil types are: Clay, Silty­clay, Sandy­clay, Sandy­loam, Silty, Silty­loam, Loamy. 2 Programme INTEREG IIIB ARCHIMED: WATER MAP Fig. 4: Sampling soil position (above) and the soil media rating map (below). Topography (T) The variable T (Topography) was obtained from elevation points, using the triangulation method in ARC/INFO system (Fig. 5). The topography of the Sarigkiol basin is for the most part a flat plain, slope being generally low (1­3%), whereas a small area in the northern part of the basin reaches almost 10%. Fig. 5: Slop rating map. Impact of the vadose zone (I) The evaluation of variable I was based on data from lithological profiles. The vadose zone rating map is presented in Fig. 6. The existence of clay materials is recorded in the southern part of the basin, which result in low vulnerability values. 3 Programme INTEREG IIIB ARCHIMED: WATER MAP Fig. 6: Vadose zone rating map. Hydraulic conductivity (C) The variable C was calculated from pumping test data and bibliography data based on the properties of the aquifer materials, as well as from pumping test analyses. The hydraulic conductivity rating map is presented in Fig. 7. Fig. 7: Hydraulic conductivity rating map. DRASTIC index vulnerability The vulnerability index values were calculated using the formula 2.2.1 (Table 2). The final vulnerability DRASTIC map was produced using the international colour code and GIS (Fig. 8). 4 Programme INTEREG IIIB ARCHIMED: WATER MAP Table 2: DRASTIC index worksheet (not all sites are included). X Y DrxDwTrxTwArxAw SrxSw IrxIw CrxCw RrxRw DRASTIC 316398.744 4472665.938 40 10 12 4 4 18 6 94 316479.421 4471011.955 20 9 8 4 4 15 6 70 317426.791 4470922.928 30 9 8 8 8 15 6 84 315585.998 4471989.000 10 10 16 2 2 21 6 77 314441.005 4471462.000 5 9 12 4 4 21 6 69 313385.033 4473472.839 20 9 12 2 2 18 6 79 312072.378 4474147.961 20 9 10 12 12 15 15 89 310915.305 4473669.457 5 6 14 6 6 18 6 67 310212.055 4476978.515 40 6 8 8 8 15 6 107 308738.289 4477028.339 5 6 8 10 10 15 6 78 324183.456 4471655.376 20 10 12 4 4 18 6 90 323352.360 4471719.099 40 9 12 8 8 18 6 109 322811.001 4470114.730 10 6 10 10 10 15 6 65 322097.354 4472368.593 30 9 12 6 6 21 6 100 323104.107 4473249.190 40 8 14 6 6 24 6 130 322603.000 4473938.626 10 8 14 4 4 24 6 94 321414.315 4474388.865 10 8 10 8 8 15 6 65 Fig. 8: Vulnerability map of the Sarigkiol basin. The highest vulnerability values in the Sarigkiol basin are associated with shallow aquifers without great depth of the vadose zone. Low and very low values of vulnerability are located in the southern part of the basin in which the aquifer has great depth of vadose zone with layers of clay and silt and great depth to groundwater level (Fig. 9). 5 Programme INTEREG IIIB ARCHIMED: WATER MAP 3.2. Florina basin Florina basin is located in the central part of Florina Prefecture, Western Macedonia region, Greece, covering an area about of 319 km 2. The mean altitude of the basin is about 620 m and the mean slope 1.5%. In the area developed two aquifer systems, one alluvial aquifer covering an area about 180 km 2 and a second one in neogene deposits covering an area about 149 km 2 . 3.2.1 Elaboration of the vulnerability map Depth to groundwater (D) The depth to groundwater in the alluvial aquifer of Florina basin ranges from 0 to more than 25 m below ground surface (Fig. 9). Fig. 9: Depth to water table rating map. In general, the deeper the water levels are, the longer the pollutant takes to reach the groundwater table. Net recharge (infiltration) (R) The variable R was calculated from rainfall data and the coefficients of infiltration of geological formations. The annual rainfall is 643 mm. 6 Programme INTEREG IIIB ARCHIMED: WATER MAP Fig. 10: Net annual recharge rating curve and the recharge rating map. Aquifer material or media (A) Aquifer media have been identified from the borehole data and 85 lithological profiles. Based on these profiles, the aquifer media was classified as (Fig. 11): 1) Gravel, 2) Sand and Gravel, 3) Sandstone and conglomerate, 4) Sand, 5) Sand, gravel and clay, 6) Clay, sand and gravel. Fig. 11: Aquifer media rating map. Soil media (S) The variable S (Soil type) was obtained from soil classification maps (IGME). The density of soil samples was 5 samples / Km 2 and the depth 0­30 cm from the ground surface. Based 7 Programme INTEREG IIIB ARCHIMED: WATER MAP on results from soil analyses, the predominant soil types are: Clay, Silty­clay, Sandy­clay, Sandy­loam, Silty, Silty­loam, Loamy. Fig. 12: Soil media rating map (below). Topography (T) The variable T (Topography) was obtained from elevation points, using the triangulation method in ARC/INFO system (Fig. 13). The topography of the Florina basin is for the most part a flat plain, slope being generally low (0­3%), whereas a small area in the central part of the basin reaches almost 10%. Fig. 13: Slop rating map. 8 Programme INTEREG IIIB ARCHIMED: WATER MAP Impact of the vadose zone (I) The vadose zone is the zone of subsoil above the water table, which is unsaturated. The characteristics of the vadose zone determine the pathway and concentration of a pollutant. The evaluation of variable I was based on data from lithological profiles (Fig. 14). The vadose zone rating map is presented in Fig. 15. Fig. 14: Litholog of one representative borehole in Florina basin. Fig. 15: Vadose zone rating map. 9 Programme INTEREG IIIB ARCHIMED: WATER MAP Hydraulic conductivity (C) The variable C was calculated from pumping test data and bibliography data based on the properties of the aquifer materials, as well as from pumping test analyses. Fig. 16: Hydraulic conductivity rating map. DRASTIC index vulnerability The final vulnerability DRASTIC map was produced using the international colour code (Fig. 17). The highest vulnerability values in the Florina basin are associated with shallow aquifers without great depth of the vadose zone. Low and very low values of vulnerability are located in the center of the basin in which the aquifer has great depth of vadose zone with layers of clay and silt and great depth to groundwater level. Regional assessment of groundwater vulnerability is a useful tool for groundwater resources management and protection zoning. The results provide important information and the vulnerability maps could be used by local authorities and decision makers. The proposed methodology will be applied in other areas with similar characteristics. 10 Programme INTEREG IIIB ARCHIMED: WATER MAP Fig. 17: Vulnerability map of the Florina basin. 11 Programme INTEREG IIIB ARCHIMED: WATER MAP 3.3 Mouriki basin Mouriki basin is located in the North part of Kozani Prefecture,Western Macedonia region, Greece, covering an area of 133.6 km 2 (Fig.18).
Load more

Recommended publications
  • The Shaping of the New Macedonia (1798-1870)
    VIII. The shaping of the new Macedonia (1798-1870) by Ioannis Koliopoulos 1. Introduction Macedonia, both the ancient historical Greek land and the modern geographical region known by that name, has been perhaps one of the most heavily discussed countries in the world. In the more than two centuries since the representatives of revolutionary France introduced into western insular and continental Greece the ideas and slogans that fostered nationalism, the ancient Greek country has been the subject of inquiry, and the object of myth-making, on the part of archaeologists, historians, ethnologists, political scientists, social anthropologists, geographers and anthropogeographers, journalists and politicians. The changing face of the ancient country and its modern sequel, as recorded in the testimonies and studies of those who have applied themselves to the subject, is the focus of this present work. Since the time, two centuries ago, when the world’s attention was first directed to it, the issue of the future of this ancient Greek land – the “Macedonian Question” as it was called – stirred the interest or attracted the involvement of scientists, journalists, diplomats and politicians, who moulded and remoulded its features. The periodical cri- ses in the Macedonian Question brought to the fore important researchers and generated weighty studies, which, however, with few exceptions, put forward aspects and charac- teristics of Macedonia that did not always correspond to the reality and that served a variety of expediencies. This militancy on the part of many of those who concerned themselves with the ancient country and its modern sequel was, of course, inevitable, given that all or part of that land was claimed by other peoples of south-eastern Europe as well as the Greeks.
    [Show full text]
  • The Case of “Young Gegides” of Emporio, Eordaia
    ISSN 2039-2117 (online) Mediterranean Journal of Vol 9 No 2 ISSN 2039-9340 (print) Social Sciences March 2018 Research Article © 2018 Karepidis K. Ioakeim. This is an open access article licensed under the Creative Commons Attribution-NonCommercial-NoDerivs License (http://creativecommons.org/licenses/by-nc-nd/3.0/). New Year’s Initiation Processions of Teenagers: The Case of “Young Gegides” of Emporio, Eordaia Karepidis K. Ioakeim Msc. in “Folklore” Doi: 10.2478/mjss-2018-0029 Abstract The social coming of age is an issue in many – if not in all – cultures through the procedures of initiations. Such ceremonies have always existed since in the traditional societies the biological adulthood happens through the society – community. The fact that these ceremonies are old is proven through totem worships that have survived until today. Obviously in our era the conceptual core of these ceremonies has transformed since the adulthood is no longer a social issue but a legal one. So these processions have a new form adjusted to the social – historical and cultural circumstances. This article deals with this adjustment observing the ancient issue of initiation processions of teenagers (agermos) through a modern point of view. Specifically, with the excuse of the custom “Young Gegides” of Emporio, Eordaia, that takes place on New Year’s Day, the article studies the way that these processions happen now in this community, their functionality and the meaning that is attributed to them not only by those who take part but also by the community. It also studies the reasons – the triggering events that led through time to these changes and finally to the adjustments and the way that these innovations became assimilated in the local community.
    [Show full text]
  • BIOGAS POTENTIAL from LIVESTOCK and POULTRY WASTES in the REGION of WESTERN MACEDONIA, GREECE Goula Ma., Bereketidou Oa,B., Econ
    16th European Biomass Conference & Exhibition, 2-6 June 2008, Valencia, Spain BIOGAS POTENTIAL FROM LIVESTOCK AND POULTRY WASTES IN THE REGION OF WESTERN MACEDONIA, GREECE Goula Ma., Bereketidou Oa,b., Economopoulos Ca., Charisiou Na. aPollution Control Technologies Department, Technological Educational Institute of Western Macedonia, Koila, Kozani, 50100, Greece, b Department of Engineering and Management of Energy Resources, University of Western Macedonia, Bakola & Sialvera, Kozani, 50100, Greece *Corresponding author. Tel: +302461068296, Fax : +302461039682, email:[email protected] ABSTRACT: Animal wastes constitute a high proportion of biomass in the region of Western Macedonia, Greece, and are able to play an important role towards the satisfaction of heat and/or energy and related material supply, with respect to environmental protection targets. Significantly, such wastes could be a significant source of energy if conventional energy prices continue to rise. This paper describes anaerobic digestion as a potential animal waste exploitation method. The aim of the present work is to strengthen the interest in animal waste potential for energy production in the region, through a methodology for the feasibility of utilization of those kinds of wastes as renewable energy resources. A combination of technical, economic and environmental issues is presented here. This study estimates the economically recoverable energy potentially available from livestock and poultry wastes in the region of Western Macedonia, Greece for the base year 2000. Anaerobic digestion of dairy cow, fed beef, goat, sheep and laying hen manures could have produced approximately 129,084 m3/d or 47x106 3 6 m /year of biogas, containing approximately 61.5 x 10 KWh/year that could result at a reduction in CO2 of over 80 x 103 tonnes per year and significant economic savings.
    [Show full text]
  • Print Sheet Remote1
    Отдалечени места към Зона I, II и III П.Код Населено място П.Код Населено място П.Код Населено място П.Код Населено място 11361 KICELI 27100 KERAMIDIA 44015 LAGKADA 70004 KSEROKABOS 12351 AGIA VARVARA 27100 MONI FRAGKOPIDIMATOS 44015 LIKORRAXI 70004 PERVOLA 13561 AGII ANARGIRI 27100 TRAGANO 44015 OKSIA 70004 PEFKOS 13672 PARNITHA 27200 AGIA MARINA 44015 PLAGIA 70004 SKAFIDIA 13679 AGIA TRIADA PARNITHAS 27200 ANALICI 44015 PLIKATI 70004 STAFRIA 13679 KSENIA PARNITHAS 27200 ASTEREIKA 44015 PIRSOGIANNI 70004 SIKOLOGOS 14451 METAMORFOSI 27200 PALEOLANTHI 44015 XIONADES 70004 SINDONIA 14568 KRIONERI 27200 PALEOXORI 44017 AGIA VARVARA 70004 TERTSA 15342 AGIA PARASKEFI 27200 PERISTERI 44017 AGIA MARINA 70004 FAFLAGKOS 18010 AGIA MARINA 27300 AGIA MAFRA 44017 VEDERIKOS 70004 XONDROS 18010 AGKISTRI 27300 KALIVIA 44017 VERENIKI 70004 CARI FORADA 18010 EGINITISSA 28080 AGIOS NIKOLAOS 44017 VROSINA 70005 AVDOU 18010 ALONES 28080 GRIZATA 44017 VRISOULA 70005 ANO KERA 18010 APONISOS 28080 DIGALETO 44017 GARDIKI 70005 GONIES 18010 APOSPORIDES 28080 ZERVATA 44017 GKRIBOVO 70005 KERA 18010 VATHI 28080 KARAVOMILOS 44017 GRANITSA 70005 KRASIO 18010 VATHI 28080 KOULOURATA 44017 DIXOUNI 70005 MONI KARDIOTISSAS 18010 VIGLA 28080 POULATA 44017 DOVLA 70005 MOXOS 18010 VLAXIDES 28080 STAVERIS 44017 DOMOLESSA 70005 POTAMIES 18010 GIANNAKIDES 28080 TZANEKATA 44017 ZALOGO 70005 SFENDILI 18010 THERMA 28080 TSAKARISIANOS 44017 KALLITHEA 70006 AGIA PARASKEFI 18010 KANAKIDES 28080 XALIOTATA 44017 KATO VERENIKI 70006 AGNOS 18010 KLIMA 28080 XARAKTI 44017 KATO ZALOGO
    [Show full text]
  • Cambridge History of Christianity, Volume 5
    the cambridge history of EASTERN CHRISTIANITY This volume brings together in one compass the Orthodox churches of the ecumenical patriarchate – the Russian, Armenian, Ethiopian, Egyptian and Syrian churches. It follows their fortunes from the late Middle Ages until modern times – exactly the period when their history has been most neglected. Inevitably,this empha- sises differences in teachings and experience, but it also brings out common threads, most notably the resilience displayed in the face of alien and often hostile political regimes. The central theme of this volume is the survival against the odds of Orthodoxy in its many forms into the modern era. The last phase of Byzantium proves to have been surprisingly important in this survival. It pro- videdOrthodoxywiththeintellectual,artisticandspiritualreserves to meet later challenges. The continuing vitality of the Orthodox churches is evident for example in the Sunday School Movement in Egypt and the Zoe¨ brotherhood in Greece. Michael Angold is a Fellow of the Royal Historical Society and is Professor Emeritus of Byzantine History at the Univer- sity of Edinburgh. His most recent publications include The Fourth Crusade: Event and Context (2003), Byzantium: The Bridge from Antiq- uity to the Middle Ages (2001) and Church and Society in Byzantium under the Comneni, 1081–1261 (1995). Cambridge Histories Online © Cambridge University Press, 2008 Cambridge Histories Online © Cambridge University Press, 2008 the cambridge history of CHRISTIANITY The Cambridge History of Christianity offers a comprehensive chronological account of the development of Christianity in all its aspects–theological,intellectual,social,political,regional,global– from its beginnings to the present day. Each volume makes a sub- stantial contribution in its own right to the scholarship of its period and the complete History constitutes a major work of academic reference.
    [Show full text]
  • Download (2MB)
    ! ∀ !∀∀# ∃%%& ∋ ( ∃%%) ∗%+ ∋ ∃%% ∋,− ./0% !∀∀# INHALTSVERZEICHNIS 1 EINLEITUNG 6-10 KAPITEL I: DIE ORIENTKRISE UND DIE MAKEDONISCHE FRAGE BIS ZUM BERLINER KONGRESS (1876-1878) 1. Die Revolution in Bosnien und Herzegowina und der russisch-türkisch Krieg. 11-13 2. Der San Stefano Vertrag und der Berliner Kongress. 13-15 3. Die Interessen der Balkanvölker in den europäischen Provinzen des Osmanischen Reiches. 15-17 4. Der europäische Imperialismus und die Makedonische Frage. 17-25 5. Resümee. 25-26 KAPITEL II: DIE VORBEREITUNGSPHASE DES MAKEDONISCHEN KAMPFES 1. Die Problematik der ethnisch-konfessionellen Heterogenität in den europäischen Provinzen des Osmanischen Reiches. 28-34 2. Der Kirchen- und Schulkampf in der Folgezeit der Gründung des bulgarischen Exarchats. 34-37 3. Die Auswirkung des Schulkampfes: die Gründung slawischer Organisationen außerhalb Makedoniens. 37-44 4. Die Aktivitäten und Beziehungen zwischen VMRO und VMOK und die Frage der makedonischen Identität. 44-58 INHALTSVERZEICHNIS 2 5. Die Verknüpfung der Kretischen mit der Makedonischen Frage: Die griechische Außenpolitik und die Aktivität der “Ethniki Etairia” vom griechisch-türkischen Krieg (1897) bis zum Ilinden-Aufstand (1903). 58-68 6. Die Aktivierung des griechischen Patriarchats in der Vorzeit des griechisch- türkischen Krieges bis zum Ilinden-Aufstand. 68-77 7. Resümee. 78-81 KAPITEL III: DER MAKEDONISCHE KAMPF BIS ZUR JUNG-TÜRKISCHEN REVOLUTION 1. Das Wiener Reformkonzept und der Weg zum Ilinden-Aufstand 82-97 2. Die Organisation des “Makedonischen Kampfes” in West-Makedonien im Jahr 1904 97-108 3. Der Verlauf des “Makedonischen Kampfes” in West-Makedonien im Jahr 1905 und seine Erweiterung auf Zentral- und Ost-Makedonien. 108-120 4. Die griechisch-bulgarischen Partisanenkriege im Jahr 1906.
    [Show full text]
  • Settlements and Dwellings in the Early and Middle Neolithic of Central and Western Macedonia
    Settlements and dwellings in the Early and Middle Neolithic of Central and Western Macedonia Ploutarchos Mitsakos SCHOOL OF HUMANITIES A thesis submitted for the degree of Master of Arts (MA) in the Classical Archaeology and the Ancient History of Macedonia January 2020 Thessaloniki – Greece Student Name: Mitsakos Ploutarchos SID: 2204180004 Supervisor: Prof. Duska Urem-Kotsou I hereby declare that the work submitted is mine and that where I have made use of another’s work, I have attributed the source(s) according to the Regulations set in the Student’s Handbook. January 2020 Thessaloniki - Greece 2 Preface This study is the completion of the postgraduate course of MA in the Classical Archaeology and the Ancient History of Macedonia at the International University of Thessaloniki. Here I would like to express my gratitude to some people of whom the contribution was vital for the completion of this study. Firstly, I would like to thank Prof. Duska Urem-Kotsou for accepting to supervise my thesis and for aiding me during all its stages. She was always available to guide me and clarify any questions or concerns about the work. Secondly, I would also like to thank Prof. Nikos Efstratiou of the Aristotle University of Thessaloniki for the discussion and the information he provided me during my study. Lastly, I would like to express my gratitude to Prof. Nikos Akamatis who helped me whenever clarifications were needed. 3 Contents Preface……………………………………………………………………………………..3 Contents…………………………………………………………………………………...4 Introduction……………………………………………………………………………….6 A. Chapter 1: Defining the region under study…………………………………………8 A.1. The prehistoric research in Macedonia.....…...……...…………………………….8 A.2.
    [Show full text]
  • 3 Sustainable Development and Tourism
    SCHOOL OF SOCIAL SCIENCES Master in Business Administration (MBA) Dissertation “The Development of Alternative Tourism in West Macedonia. Case study for Sustainable Regional Tourism Development” “Thaleia Rizou” Supervisor: “Ioannis Pollalis” Patras, Greece, “March” “2018” © Hellenic Open University, 2018 The content of this thesis/dissertation along with its results is owned by the Hellenic Open University and his/her author, where each of them has the sole and exclusive right to use, reproduce, and publish it (totally or partially) for educational or research purposes, with the obligation to make reference to the thesis’s title, the author’s name and to the Hellenic Open University where the thesis / dissertation was written. “The Development of Alternative Tourism in West Macedonia. Case study for Sustainable Regional Tourism Development” “Thaleia Rizou” Supervising Committee Supervisor: Co-Supervisor: “Ioannis Pollalis” “Ioannis Spanos” “1st Supervisor” “2nd Supervisor” Patras, Greece, “March” “2018” “The Development of Alternative Tourism in West Macedonia. Case study for Sustainable Regional Tourism Development” “Acknowledgments” I would like to express my appreciation to my supervisor Dr I. Pollalis (Professor of Strategic Management) for his assistance and support during the writing of this dissertation. Last, but not least, I wish to express my truly thanks to my family for their patience throughout this unique learning experience. Thaleia Rizou iv “The Development of Alternative Tourism in West Macedonia. Case study for Sustainable Regional Tourism Development” Abstract The paper elaborates on the development of Alternative tourism in a Sustainable way in the region of Western Macedonia which is described as an area of Economic isolation but of richness in natural and cultural resources.
    [Show full text]
  • Integrated ESIA Greece Annex 6.4.0 - Supporting Materials Cultural Heritage Baseline Page 2 of 60 Area Comp
    Integrated ESIA Greece Annex 6.4.0 - Supporting Materials Cultural Heritage Baseline Page 2 of 60 Area Comp. System Disc. Doc.- Ser. Code Code Code Code Type No. Project Title: Trans Adriatic Pipeline – TAP GPL00-ASP-642-Y-TAE-0070 Integrated ESIA Greece Annex 6.4.0 - Supporting Document Title: Rev.: 00 / at05 Materials Cultural Heritage Baseline TABLE OF CONTENTS 1 CULTURAL HERITAGE ANNEX 3 1.1 Cultural Heritage Baseline Study Methodology 3 1.1.1 Cultural Heritage Site Types 3 1.1.2 Cultural Heritage Site Importance/Quality Criteria 3 1.2 Cultural Heritage Baseline Fieldwork Methodology 4 1.3 Cultural Heritage Data Recording Forms 7 1.3.1 Daily Survey Record Form 7 1.3.2 Site Evaluation Form 8 1.3.3 Site Observation Checklist 9 1.4 General Chronology and Cultural Context for Greece with a Focus on the Region of Macedonia and Thrace 11 1.4.1 Palaeolithic Period (250,000 – 10,000 BC) 14 1.4.2 Mesolithic Period (10,000 – 6000 BC) 15 1.4.3 Neolithic Period (6000 – 3000 BC) 15 1.4.4 Bronze Age Period (3000 – 1050 BC) 16 1.4.4.1 Early Bronze Age 16 1.4.4.2 Middle Bronze Age 17 1.4.4.3 Late Bronze Age 17 1.4.5 Early Iron Age (1050 – 800 BC) 18 1.4.6 The Archaic Period (800 – 500 BC) 19 1.4.7 The Classical Period (500 – 323 BC) 19 1.4.7.1 The 5th century BC 19 1.4.7.2 The 4th Century BC 20 1.4.8 The Hellenistic Period (323 – 146 BC) 21 1.4.9 The Roman Period (146 BC – AD 330) 21 1.4.10 The Byzantine Period (AD 330 – 1453) 22 1.4.11 Ottoman Period (15th century – early 19th century) 23 1.4.11.1 Early Period (15th – 16th centuries) 23 1.4.11.2 Later Ottoman Rule(17th century – early 19th century) 25 1.4.12 Modern Period (late 19th century – Present) 26 1.5 Inventory of Cultural Heritage Resources 28 LIST OF TABLES Table 1-1 Cultural Heritage Site Importance/Quality Criteria 4 Table 1-2 General Timeline of Greek Prehistory and History with focus in the Region of Macedonia and Thrace 13 Table 1-3 Cultural Heritage Sites and Areas of High Archaeological Potential within/ in proximity to the Study Area.
    [Show full text]
  • Drama, O Agora, 27.04.2009 Platanenaue, 272 M Dra 132, KF 75.87.00, 41°08'04''N, 24°21'22’‘E Leg
    A Willing Contribution to Flora Hellenica Field records 2012 Stachys iva by Eckhard & Rita Willing Dessau March 2012 Published by BGBM Press Botanic Garden and Botanical Museum Berlin-Dahlem Freie Universität Berlin Berlin, 2013 ISBN 978-3-921800-85-0 http://dx.doi.org/10.3372/wfr2012 © Eckhard & Rita Willing, 2013 The Botanic Garden and Botanical Museum Berlin-Dahlem as publisher reserves the right not to be responsible for the topicality, correctness, completeness or quality of the information provided. The information provided is based on material identified and named by the authors. The entire collections are preserved in the Herbarium of the Botanic Garden and Botanical Museum Berlin-Dahlem, where the determinations can be reassessed. This publications should cited as: Willing E. & Willing R. 2013: A Willing contribution to Flora Hellenica. Field records 2012. – Berlin: Botanic Garden and Botanical Museum Berlin-Dahlem, stable URL: http://dx.doi.org/10.3372/wfr2012 Address of the authors: Rita und Eckhard Willing Augustenhof 14 D-06842 Dessau-Roßlau Germany [email protected] 2 1. Introduction As in past years we hereby would like to present the results of our last botanical trip for the flora Hellenica to Greece. The plants collected in 2012 now are mounted, are determined (some only up to the genus level), labeled and given into the Access databank. They all are available in the Botanical Museum of Berlin-Dahlem. After analysis of our own previous collections and of distribution maps published in Flora Hellenica Vol 1 and Vol 2 we planned to collect in 2012 mainly in the hill country around Grevena (Grevena) and around Ptolemaida (Kozanis).
    [Show full text]