FACT SHEET: Axios River Basin
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(2019), the Vardar River As a Border of Semiosphere – Paradox Of
Geographia Polonica 2019, Volume 92, Issue 1, pp. 83-102 https://doi.org/10.7163/GPol.0138 INSTITUTE OF GEOGRAPHY AND SPATIAL ORGANIZATION POLISH ACADEMY OF SCIENCES www.igipz.pan.pl www.geographiapolonica.pl THE VARDAR RIVER AS A BORDER OF SEMIOSPHERE – PARADOX OF SKOPJE REGENERATION Armina Kapusta Urban Regeneration Laboratory Institute of Urban Geography and Tourism Studies Faculty of Geographical Sciences University of Łódź Kopcińskiego 31, 90-142 Łódź: Poland e-mail: [email protected] Abstract As suggested by its etymology, regeneration usually carries positive connotations while its negative aspects tend to be belittled. However, any renewal results in major morphological, physiognomic, functional or social changes, which imply changes in the meanings encoded in space. These transformations are not always welcome and they may lead to public discussions and conflicts. Skopje 2014 is a project within which such controversial transformations have been taking place. The area surrounding the Vardar River and its banks plays a major role here. On the river banks monumental buildings were erected, bridges over the river were modernised and new ones, decorated with monuments, were built for pedestrians. Bridges can be considered a valuable component of any urban infrastructure as they link different parts of a settlement unit (in the case of Skopje – left (northern) bank and the right (southern) bank; Albanian and Macedonian), improve transport, facilitate trade and cultural exchange. In this context, referring to Lotman’s semiosphere theory, they may become borders of semiotic space, which acts as a filter that facilitates the penetration of codes and cultural texts. Yet, in multicultural Skopje meanings attached to bridges seem to lead to social inequalities as they glorify what is Macedonian and degrade the Albanian element. -
The Statistical Battle for the Population of Greek Macedonia
XII. The Statistical Battle for the Population of Greek Macedonia by Iakovos D. Michailidis Most of the reports on Greece published by international organisations in the early 1990s spoke of the existence of 200,000 “Macedonians” in the northern part of the country. This “reasonable number”, in the words of the Greek section of the Minority Rights Group, heightened the confusion regarding the Macedonian Question and fuelled insecurity in Greece’s northern provinces.1 This in itself would be of minor importance if the authors of these reports had not insisted on citing statistics from the turn of the century to prove their points: mustering historical ethnological arguments inevitably strengthened the force of their own case and excited the interest of the historians. Tak- ing these reports as its starting-point, this present study will attempt an historical retrospective of the historiography of the early years of the century and a scientific tour d’horizon of the statistics – Greek, Slav and Western European – of that period, and thus endeavour to assess the accuracy of the arguments drawn from them. For Greece, the first three decades of the 20th century were a long period of tur- moil and change. Greek Macedonia at the end of the 1920s presented a totally different picture to that of the immediate post-Liberation period, just after the Balkan Wars. This was due on the one hand to the profound economic and social changes that followed its incorporation into Greece and on the other to the continual and extensive population shifts that marked that period. As has been noted, no fewer than 17 major population movements took place in Macedonia between 1913 and 1925.2 Of these, the most sig- nificant were the Greek-Bulgarian and the Greek-Turkish exchanges of population under the terms, respectively, of the 1919 Treaty of Neuilly and the 1923 Lausanne Convention. -
The Disaster and the Red Cross Red Crescent Response to Date
Revised Emergency Appeal The former Yugoslav Republic of Macedonia: Population Movement Revised Appeal n° MDRMK005 People to be assisted: Appeal launched 10 September 2015 First phase (until March 2016): 214,886 people1; Glide n° OT-2015-000069-MKD Second phase (until December 2016): 6,250 people2 Revision n° 2 issued 6 June 2016 193,218 Swiss francs DREF allocated Appeal ends 31 December 2016 6,095,910 Swiss francs revised Appeal budget Extended 3 months (from September 2016) 933,353 Swiss francs funding gap This Revised Emergency Appeal seeks a total of some 6,095,910 Swiss francs - a small increase from the original budget of 5,927,821 Swiss francs - to enable the IFRC to support the Red Cross of the former Yugoslav Republic of Macedonia to deliver assistance and support to some 221,136 people. The current revised appeal builds upon the previous revision, continuing the provision of basic food and non-food items, hygiene promotion, health care including First Aid, Restoring Family Links (RFL) services, and community engagement, as well as building the response capacities of the National Society through contingency stocks. With this revision, the Red Cross of the former Yugoslav Republic of Macedonia is responding to the daily needs of the beneficiaries stranded in the two camps, as well as to the needs of irregular migrants in the Detention Centre in Skopje and to those of irregular migrants crossing the border from Serbia and Greece. The National Society is adding the provision of psychosocial support and more comprehensive community engagement strategy with both the national population and the migrants, as well as the rehabilitation of their asylum centre to support the long term shelter needs of the migrants in country. -
Structural Evolution of the Vardar Root Zone, Northern Greece: Discussion and Reply
Structural evolution of the Vardar root zone, northern Greece: Discussion and reply Discussion C. M. BARTON"' Department of Geology, Sedgwick Museum, Downing Street, Cambridge CB2 3EQ, England Zimmerman and Ross (1976) presented an interpretation of suggested in their abstract. Such well-documented stratigraphic Greek geology in which Vardar ocean crust was eliminated in two ages provide compelling evidence that ophiolite emplacement oc- successive directions (their Fig. 6). Their contribution is welcome, curred significantly before Late Cretaceous time, probably soon although it included a number of points that require clarification. after the first deformation of the Othris margin. A metamorphism First, it is generally agreed that northeast Greece has an ex- of about the same age (Early Cretaceous) is widespread in adjacent tremely complex post-Triassic (Alpine) history. However, in their Pelagonian rocks (Mercier, 1973b). "regional tectonic model" Zimmerman and Ross did not once Because both the direction and age of thrusting associated with specify the approximate dates of tectonism. Second, the Vardar the Othris zone ophiolites are fundamental to any tectonic model of zone is only one of two parallel belts in Greece which contain mafic the Hellenides, their position in Figure 6 of Zimmerman and Ross and ultramafic rocks interpreted as ophiolites. Fragments of similar needs clarifying. Certainly, no fragments of the Othris ocean (the oceanic affinity occur farther west in the Othris (= sub-Pelagonian) Vourinos, Pindos, or Othris ophiolites) could have been derived zone. If the authors' assertion is correct and the Othris zone from an area east of Olympos before Tertiary time, because the ophiolites are rooted farther east, then existing data from this zone Olympos platform records continuous Mesozoic shallow-water (which includes Zimmerman's own [1972] account of the Vourinos sedimentation. -
World Bank Document
E2120 EMP Checklist for Construction and Rehabilitation Activities General Guidelines for use of EMP checklist: For low-risk topologies, such as school and hospital rehabilitation activities, the ECA Public Disclosure Authorized safeguards team developed an alternative to the current EMP format to provide an opportunity for a more streamlined approach to preparing EMPs for minor rehabilitation or small-scale works in building construction, in the health, education and public services sectors. The checklist-type format has been developed to provide “example good practices” and designed to be user friendly and compatible with safeguard requirements. The EMP checklist-type format attempts to cover typical core mitigation approaches to civil works contracts with small, localized impacts. It is accepted that this format provides the key elements of an Environmental Management Plan (EMP) or Environmental Management Framework (EMF) to meet World Bank Environmental Assessment requirements under OP 4.01. The intention of this checklist is that it would be applicable as guidelines for the small works contractors and constitute an Public Disclosure Authorized integral part of bidding documents for contractors carrying out small civil works under Bank-financed projects. The checklist has three sections: Part 1 includes a descriptive part that characterizes the project and specifies in terms the institutional and legislative aspects, the technical project content, the potential need for capacity building program and description of the public consultation process. This section could be up to two pages long. Attachments for additional information can be supplemented when needed. Part 2 includes an environmental and social screening checklist, where activities and potential environmental issues can be checked in a simple Yes/No format. -
Political and International Implications of Integrated Water Resources Management of Transboundary River Basins: the Case of Axios/Vardar River Basin”
View metadata, citation and similar papers at core.ac.uk brought to you by CORE UNIVERSITY OF MACEDONIA DEPARTMENT OF BALKAN, SLAVIC AND ORIENTAL STUDIES MASTER PROGRAMME IN “POLITICS AND ECONOMICS OF CONTEMPORARY EASTERN AND SOUTHEASTERN EUROPE” DISSERTATION “Political and International implications of integrated water resources management of transboundary river basins: The case of Axios/Vardar River basin” MICHAIL I.TSAVDARIDIS Graduate of Political Sciences Thessaloniki 2013 Abstract Abstract The political rivalries over the water resources are highly increased due to their scarcity, several types of pollution, increasing water consumption and several environmental shifts. These tensions are a result of the great number of transboundary river basins worldwide (261). The international institutions promote a remarkable legal framework in order to regulate those dimensions amongst the riparian states. The new EU Water Framework Directive 2000/60 and the decisions of Helsinki convention could be the road map for integrated water resources management (IWRM). In Greece the main renewable resources are “imported” and for this reason the necessity of an IWRM is obvious and a hard task at the same time. This dissertation focuses on the Axios/Vardar river basin and examines the possibility of a possible transnational cooperation in respect of the international law framework. i Table of Contents Table of Contents Abstract ......................................................................................................................... -
Analysis of the 2014 Summer Season for Macedonia Compared to 1981-2010 Base Period
Analysis of the 2014 summer season for Macedonia compared to 1981-2010 base period Temperature Average summer (June, July and August) air temperatures in Macedonia were mainly around normal value for the 1981-2010 base period. During summer 2014, mean air temperature ranged between 15.6.°C in Lazaropole and 25.6°C in Gevgelija. The departure of the mean temperature from the normal for the 1981-2010 base period ranged from -0.6°C in Kriva Palanka to 0.3°C in Gevgelija and Bitola. Station Departure (°C) June July August Summer OHRID -0.4 -0.8 0.8 -0.1 BEROVO -0.2 -0.4 0.4 -0.1 D.KAPIJA -1.0 -0.1 0.4 -0.2 GEVGELIJA 0.1 0.0 0.8 0.3 K.PALANKA -0.7 -0.9 -0.2 -0.6 LAZAROPOLE -0.3 -1.3 0.5 -0.4 PRILEP -0.4 -0.4 0.0 -0.3 SKOPJE -0.8 -0.6 0.1 -0.4 STIP -0.9 -0.6 0.3 -0.4 STRUMICA -0.5 -0.3 0.3 -0.2 BITOLA -0.2 0.1 0.9 0.3 Table 1. Departure of the mean temperature (°C) from the normal for the 1981-2010 base period Three-month course of the mean, maximum and minimum daily air temperature in Kriva Palanka, Gevgelija and Bitola during summer 2014 is shown in figures 1, 2 and 3. Figure 1. Three-month course of the mean, maximum and minimum daily air temperature in Kriva Palanka during summer 2014 Figure 2. -