Body Height and Its Estimation Utilizing Arm Span Measurements in Macedonian Adults
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Macedonia: Not out of the Woods Yet
Update Briefing Europe Briefing N°37 Skopje/Brussels, 25 February 2005 Macedonia: Not out of the Woods Yet I. OVERVIEW the two parties forced a 7 November 2004 referendum vote on the proposed law. Prime Minister Vlado Buckovski and representatives of Although VMRO was a signatory to the original peace his government and the opposition converged in Brussels agreement, it used the pre-referendum period to question on 14 February 2005 to hand over Macedonia's response sharply the government's performance and the general to the European Commission's 3,000-item questionnaire, wisdom of power-sharing among the ethnic communities. the latest stage in the EU membership application, The government worked to reassure its supporters and which was formally submitted almost a year ago. The argued that its plans would guarantee fast track economic occasion was celebrated by a concert starring Macedonian growth, European integration and better governance. musicians at an exclusive Brussels venue. Appropriately The emergence of Albanian paramilitaries on the enough for St. Valentine's Day, the relationship with the outskirts of Skopje increased tensions and gave rise to EU had taken on a new depth, but nuptials are far from concerns that Macedonia's young and fragile multi-ethnic concluded. The considerable progress Macedonia has democracy might be at serious risk. made is still fragile. The crucial decentralisation process requires careful implementation, and the coalition A strategically-timed U.S. decision to recognise the government and its constituent parties should apply a country's official name as "Macedonia" helped to ensure number of confidence building measures. -
The Significance of the Geologic Time Factor in Metallogeny and Petrology
THE SIGNIFICANCE OF THE GEOLOGIC TIME FACTOR IN METALLOGENY AND PETROLOGY Mehmed RAMOVIÇ Natural Science Faculty, Sarajevo, Yugoslavia INTRODUCTION During the past decades metallogeny, as a new branch of geology, earned an important place in the industrial planning in many countries. Metallogeny treats the regularities of spatial distributions and temporal successions of origin of different types of mineral deposits and their relations to magmatic activities and orogenic stages. To compose useful prognostical metallogenetic maps, the co-operation is needed of many specialists, such as stratigraphers, structural geologists, petrologists, metalloge- nists, geochemists, geophysicists and others. Here we will point out the urgent need for co-ordination of metallogenetic studies of geologists of different parts of the world. The problem that metallogenists are faced with, after analyses of numerous documents (facts), is how to predict suitable regions in which to plan prospection for distinct types of mineral deposits and to choose suitable methods for their discovery. In this article we Will discuss the significance of the geologic time factor in metallogeny and petrology. Over the past ten years we have been gathering documents about different types of mineral deposits, their age, their relation to orogenic stages, the structures of the mining regions and metallogenetic belts, the character and quantitative relations between different types of accompanying magmatic rocks, about their absolute and relative geologic age determinations, and after analyses of numerous statistical data, we have established some regularities which are clearly evident in the Mediterranean countries. They could be summarized as follows : a. The metallogenetic differentiation develops gradually, and is closely related to particular geologic periods as schematically represented in Fig.1.; Fig. -
About Bulgaria
Source: Zone Bulgaria (http://en.zonebulgaria.com/) About Bulgaria General Information about Bulgaria Bulgaria is a country in Southeastern Europe and is situated on the Balkan Peninsula. To the north the country borders Rumania, to the east – the Black Sea, to the south – Turkey and Greece, and to the west – Yugoslavia and Macedonia. Bulgaria is a parliamentary republic with a National Assembly (One House Parliament) of 240 national representatives. The President is Head of State. Geography of Bulgaria The Republic of Bulgaria covers a territory of 110 993 square kilometres. The average altitude of the country is 470 metres above sea level. The Stara Planina Mountain occupies central position and serves as a natural dividing line from the west to the east. It is a 750 km long mountain range stretching from the Vrushka Chuka Pass to Cape Emine and is part of the Alpine-Himalayan mountain range. It reaches the Black Sea to the east and turns to the north along the Bulgarian-Yugoslavian border. A natural boundary with Romania is the Danube River, which is navigable all along for cargo and passenger vessels. The Black Sea is the natural eastern border of Bulgaria and its coastline is 378 km long. There are clearly cut bays, the biggest two being those of Varna and Bourgas. About 25% of the coastline are covered with sand and hosts our seaside resorts. The southern part of Bulgaria is mainly mountainous. The highest mountain is Rila with Mt. Moussala being the highest peak on the Balkan Peninsula (2925 m). The second highest and the mountain of most alpine character in Bulgaria is Pirin with its highest Mt. -
Thermotectonic Evolution of an Extensional Dome: the Cenozoic Osogovo–Lisets Core Complex (Kraishte Zone, Western Bulgaria)
Int J Earth Sci (Geol Rundsch) (2004) 93: 1008–1024 DOI 10.1007/s00531-004-0435-2 ORIGINAL PAPER A. Kounov Æ D. Seward Æ D. Bernoulli Æ J.-P. Burg Z. Ivanov Thermotectonic evolution of an extensional dome: the Cenozoic Osogovo–Lisets core complex (Kraishte zone, western Bulgaria) Received: 10 November 2003 / Accepted: 18 July 2004 / Published online: 25 September 2004 Ó Springer-Verlag 2004 Abstract The Kraishte region of Bulgaria is located at Keywords Fission track Æ Core complex Æ Heat the junction of the Balkanides and Hellenides-Dinarides transfer Æ Extension Æ Bulgaria tectonic belts. Fission-track analysis on both apatites and zircons documents the Cenozoic exhumation of a Pre- cambrian basement bounded by low-angle detachments. Late Eocene–Oligocene extension began prior to 47 Ma Introduction and was dominantly in a top-to-the-southwest direction, confirmed by the sense of younging of apatite and zircon The Alpine Mediterranean mountain system results ages. This crustal extension controlled the formation of from subduction and partial obduction of former half-graben sedimentary basins on the hanging walls of Mesozoic ocean basins during the collision of Africa, the detachments. Thermal modelling of these hanging Europe and a number of smaller intervening microplates wall units provides evidence for heat transfer across the (Dewey et al. 1973; Boccaletti et al. 1974; Stampfli et al. detachments from a relatively warm rising footwall. 1991; Ricou 1994). One of the major remaining ques- From 32 to 29 Ma, pervasive magmatic activity resulted tions on this mountain system concerns the Balkan re- in the emplacement of rhyolitic to dacitic subvolcanic gion where north- to east- (eastern Alps, Carpathians) bodies and dykes, along with intrusion of the Osogovo and south- to west-vergent (Dinarides, Hellenides) belts granite. -
Status of the Project Activities by 30Th November 2019
Status of the project activities by 30th November 2019 Reporting Period Status of the project activities by 30th November 2019 Donor EU, UNDP Country Republic of N. Macedonia Project Title Improving the Management of Protected Areas Project ID 00090466 (Atlas Award ID) Outputs 00096220 - Improving the Management of Protected Areas (Atlas Project ID and Description) 4. By 2020, individuals, the private sector and state institutions Strategic Plan and/or CPD base their actions on the principles of sustainable development, Outcomes and communities are more resilient to disasters and environmental risks. Indicative output: 4.2 Public and private actors have improved capacities to implement, monitor and evaluate policies related to environment, climate change and nature protection. Implementing Partner(s) Ministry of Environment and Physical Planning Project Start Date 01 July 2017 Project End Date 31 May 2020 2019 Annual Work Plan Budget $US 2,283,402.05 Total resources required $US 4,804,390.00 Revenue received UNDP TRAC: $US 335,190.00 $ 4,469,200.00 EU: (4,000,000.00 EURO) Government: - In-Kind: - Contingency $US 69,767.00 UNDP Contact Person Narine Sahakyan UNDP Resident Representative Email: [email protected] Tel.: 3249502 1.Grantee: Balkan Foundation for Sustainable Project title: SUSTAINABLE MANAGEMENT OF PLANT NATURAL RESOURCES IN THE PRESPA REGION Development – BFSD, Skopje Outputs Completed Activities Ongoing and Planned Activities To be completed by: Potential Risks 1. Digital map of 1. Botanical targeted plant species expeditions developed 2. Mapping of presence of wild flora species 3. Digital map of targeted plant species of 18000 ha prepared Biopotential and 1. -
Description of Ozyptila Balcanica Sp. N. from the Balkan Peninsula and Its Comparison with the Closely Related O
ACTA ZOOLOGICA BULGARICA Systematics and Phylogenetics Acta zool. bulg., 68 (4), 2016: 483-490 Research Article Description of Ozyptila balcanica sp. n. from the Balkan Peninsula and its Comparison with the closely related O. umbraculorum Simon, 1932 (Araneae: Thomisidae) Christo Deltshev1, Gergin Blagoev2, Marjan Komnenov3 & Stoyan Lazarov1 1 National Museum of Natural History, Bulgarian Academy of Sciences, Sofia, Bulgaria; E-mail:[email protected] m; [email protected] 2 Centre for Biodiversity Genomics, University of Guelph, Guelph, Canada; E-mail: [email protected] 3 Macedonian Museum of Natural History, Skopje, FYR Macedonia; E-mail: [email protected] Abstract: Ozyptila balcanica sp. n. is described (based on both males and females) from Bulgaria (Zemen Gorge), Greece (Arkadia, Mainalo) and FYR Macedonia (Skopje Region, Osogovo Mts.). The new species re- sembles the poorly known O. umbraculorum Simon, 1932, recorded from France, Portugal and Spain, but is clearly a distinct species. Illustrations of both taxa are presented. Due to the isolated position of both species in the genus, we proposed a new species group – umbraculorum, characterised by a large inter- mediate apophysis (ITA), armed with well-developed teeth, and a long scimitar-shaped tegular apophysis. The females have similar epigynes with pan-shaped median septum. Key words: Description, comparison, Ozyptila, umbraculorum species group Introduction The crab spiders of the genus Ozyptila Simon, 1864 the text shows that he had female specimens. Later, are common in a range of ground habitats such as URONES (1985) and JIMÉNEZ -VALVER D E (2002) pre- moss, detritus and leaf litter. Currently, the genus in- sented new illustrations of female and male, respec- cludes 103 species and five subspecies, 16 of which tively, of O. -
Macedonian Production & Location Guide
MACEDONIAN PRODUCTION & LOCATION GUIDE MACEDONIAN FILM AGENCY 8 Mart No.4 1000 Skopje, Macedonia MACEDONIAN PRODUCTION & LOCATION GUIDE Let Macedonia be on your filmmaking map as a beautiful country with breathtaking landscapes, exceptional and skilled local talents and professionals, production companies that have an impressive record in domestic and international production, lowest taxes in the region and Europe and 20% production incentive. …The magic of the Republic of Macedonia is awaiting for you … Explore its beauty. CONTENT 05 INTRODUCTION 05 Macedonian Film Agency 06 Co-production Funding 08 Production incentive 09 Criteria for funding 10 WHY MACEDONIA? 12 MACEDONIA GENERAL OVERVIEW 12 Facts for Macedonia 14 Transport infrastructure 18 Accommodation 18 Communication 18 Climate 23 USEFUL INFO 23 Filming & Location Permits 23 Visas 23 Working Permits 24 Customs Regulations 24 Temporary Import of Professional Equipment 26 BRIEF OVERVIEW OF THE MACEDONIAN FILM INDUSTRY 30 LOCATION GUIDE 30 Regions 38 Urban Areas 38 Rural Areas 40 Lakes 42 Rivers 42 Waterfalls 43 Mountains & National Parks 43 Spa Resorts 45 Caves 46 Big City Island 46 Archeological Sites 47 Churches & Monasteries 4 MACEDONIAN FILM AGENCY Macedonian Film Agency is the newly founded governing film body, erators, internet providers, cinema exhibitors, distributors, entertain- legal successor of the Macedonian Film Fund which started to work in ment games and games of chance. 2014 under the new Film Industry Law. The new Agency will continue Under the new Film Industry Law, The Macedonian Film Agency will to giving its full support to development of the film industry, film tra- be the first stop for foreign companies and individuals who are pre- dition and film culture in Macedonia. -
I Macedonia and the Macedonians
I MACEDONIA AND THE MACEDONIANS The Macedonian People and Macedonian National Consciousness The development of nearly all European peoples and nations has been accompa- nied by numerous and various historical and political difficulties and upheavals. Even in the case of some of the most highly developed modern nations of the European and other continents, history has dictated situations which are not too different from those of the Macedonian people: tribes and ethnicities have become mixed, languages and names have been borrowed, territories and state boundaries have been altered, faiths and cultures have intertwined with each other… Let us take the example of France and the French. The ancient Gaul covered the territory of what is today northern Italy, France, part of Switzerland, Luxem- bourg, Belgium and the Netherlands, and was populated by Gauls, a Roman name designating Celtic tribes. In the 1st century BC Julius Caesar conquered Gaul and it remained within the borders of the Roman Empire up to the end of the 5th century AD. This was a period during which a complex process of assimilation of the Gauls and Romans took place and when Vulgar Latin became the spoken language of the population. It was from this basis that later, influenced by the vernacular of some Germanic tribes, modern French developed. The present-day name of the French derives from the state of the Franks, a group of western Germanic tribes who lived around the River Rhine in what is today Germany and who, towards the late 5th century, conquered almost the whole of ancient Gaul and, by the end of the 8th century, most of Central and Western Europe. -
Seismicity and Geodynamics of Macedonia and Surroundings
Seismicity and Geodynamics of Macedonia and Surroundings Boyko Ranguelov1, Garo Mardirosian1, Stoyan Velkosky2 1Bulgarian Academy of Sciences - Sofia 2Institute GAPE - Skopie e-mail: [email protected] Key words: seismicity, neotectonic, earthquakes, GPS measurements Introduction This is a summary of the investigations of the authors and their coauthors published during the last decade. It shows the knowledge and the common views about the seismicity and the geodynamics of the South Balkans and the Aegean region. This is not the full reflection of the previous research and results made on these areas by different authors. The aim of this study is just to show the results and possible applications to the seismic hazard assessment related to Macedonia. The area is extensively investigated by many authors and different views and interpretations have been expressed (McKenzie, 1972; Papazachos, 1966; Ranguelov, 1987; Vannicci, 2004, etc.). Our aim is just to focus on some summary results and their internal relationships. On this base conclusions about the practical applications are done. Neotectonic background The neotectonic movements of the Balkan Peninsula occurred after the last intense thrusting (Early Miocene), and after the Early – Middle Miocene planation. (Zagorchev, 1992). They were controlled by extensional collapse of the Late Alpine orogen, and by extension behind the Aegean arc, and were influenced by the complicated vertical and horizontal movements in the Pannonian region. The Balkan mountain and the Dinarian Hellenic linear neotectonic morphostructures inherited the Alpine orogenic zones and bounded the Central-Balkan neotectonic region. The linear morphostructures were tilted towards the Pannonian and Euxinian basins and the North-Aegean though. -
The Macedonian Wine Cluster (Pdf)
The Macedonian Wine Cluster Harvard Business School Microeconomics of Competitiveness, Spring 2006 Instructor: Prof. Michael E. Porter Project Group: Bartol Letica Dan Doncev Ersin Esen Nem Mijic Susanne Cassel May 5, 2006 TABLE OF CONTENTS Page I. Macedonia’s Economy and National Business Environment 3 1.0 Country overview 3 1.1. Political situation 3 1.2. Economic analysis 4 2.0 National Diamond Analysis 8 2.1. Factor Conditions 9 2.2. Context for Firm Strategy and Rivalry 9 2.3. Demand Conditions 10 2.4. Related and Supporting Industries 10 3.0 Country Strategy and recommendations 11 II. The Macedonian Wine Cluster 13 4.0 Overview of the Macedonian Wine Cluster 13 4.1 History 13 4.2 Cluster Map 14 4.3. Key Features of the Macedonian Wine Cluster 15 4.4 Winemaking in Macedonia 16 4.4.1 Grape Growing/Procurement 16 4.4.2 Crushing, Fermentation and Aging 17 4.4.3 Bottling and Packaging 18 4.4.4 Production, Sales, Marketing and Distribution 18 5.0 Cluster Diamond Analysis 20 5.1. Factor Conditions 21 5.2. Context for Firm Strategy and Rivalry 22 5.3. Demand Conditions 23 5.4. Related and Supporting Industries 24 6.0 Cluster recommendations 27 III. Bibliography and Disclosures 31 2 I. Macedonia’s Economy and National Business Environment 1. Country overview 1.1. Political situation Macedonia was proclaimed a sovereign and independent state on September 17, 1991 after a national referendum. Its history has been characterised by a centuries-long struggle of the Macedonian people for a free and independent state, symbolized by the state’s motto “liberty or death”. -
Granitoid Formations in the Republic of Macedonia
GRANITOID FORMATIONS IN THE REPUBLIC OF MACEDONIA B. BOEV, S. LEPITKOVA and G. PETROV Faculty of Mining and Geology Stip, Goce Delcev, 89, 2000 Stip, Republic of Macedonia; [email protected] Abstract: Granitoid formations can be found in all geotectonic units in the territory of the Republic of Macedonia: the Western Macedonian zone, the Pelagonian massif, the Vardar zone and throughout the Serbo-Macedonian mass. The rocks of these formations occur in smaller or larger magmatic bodies. They are grantitic, granodioritic, syenitic and monzonitic in composition varying in age from Tertiary to Precambrian ( Fig.1). Key words: Granites, granodiorites, monzonites, syenities. Granodiorite formation in the Pelagonian massif The rocks of the formation occur as irregular magmatic bodies predominantly of N - S strike, and mainly along the axis of the Pelagonian massif (Kajmakcalan - Mt Selecka - Babuna). The bodies are forced into the gneiss-micaschists series of the Precambrian complex. The most widespread rocks of the formation are massive medium- to coarse- grained granodiorites and porphyroid granodiorites. Granites, quartz-monzonites and quartz-diorites are less developed. They are fairly abundant in quartz, plagioclases and biotite, whereas the content of potassium feldspar is variable. Apatite, titanite, hornblende, zircon, garnet, orthite and magnetite are the most common accessory minerals and those of epidote, zoisite, sericite, chlorite and kaolin occur as secondary minerals. Potassium feldspars occur as orthoclase and microcline and plagioclases as oligoclase, andesine seldom albite as well. Fig. 1. Tectonic map of the Republic of Macedonia WWZ - Western Macedonian zone, PM - Pelagonian massif, VZ - Vardar zone, SMM - Serbo-Macedonian mass, 1 - Neogene-Quaternary sediments, 2 - volcanic and volcanogene-sedimentary rocks, 3 - Paleogene sediments, 4 - granitoids, 5 - Mesozoic complex, 6 - Paleozoic complex, 7 - Riphean-Cambrian and Precambrian complexes. -
Myriapoda: Diplopoda) of the Republic of North Macedonia
Arthropoda Selecta 28(2): 191205 © ARTHROPODA SELECTA, 2019 Checklist of the millipedes (Myriapoda: Diplopoda) of the Republic of North Macedonia Êîíòðîëüíûé ñïèñîê äèïëîïîä (Myriapoda: Diplopoda) Ðåñïóáëèêè Ñåâåðíàÿ Ìàêåäîíèÿ Zvezdana S. Jovanoviæ1*, Aleksandra Cvetkovska-Gjorgjievska2, Dana Preliæ2, Dragan . Antiæ1,3, Slobodan E. Makarov1,3 Çâåçäàíà Ñ. £îâàíîâè1*, Àëåêñàíäðà Öâåòêîâñêà-îðèåâñêà2, Äàíà Ïðåëè2, Äðàãàí Æ. Àíòè1,3, Ñëîáîäàí Å. Ìàêàðîâ1,3 1 Institute of Zoology, Faculty of Biology, University of Belgrade, Studentski Trg 16, 11000 Belgrade, Serbia; E-mail: [email protected] 2 Institute of Biology, Faculty of Natural Sciences and Mathematics, Saints Cyril and Methodius University, Arhimedova 3, 1000 Skopje, North Macedonia 3 Serbian Biospeleological Society, Trg Dositeja Obradoviæa 2, 21000 Novi Sad, Serbia KEY WORDS: Diplopoda, diversity, fauna, North Macedonia, Balkan Peninsula. ÊËÞ×ÅÂÛÅ ÑËÎÂÀ: Diplopoda, ðàçíîîáðàçèå, ôàóíà, Ñåâåðíàÿ Ìàêåäîíèÿ, Áàëêàíñêèé ïîëóîñòðîâ. ABSTRACT. The millipede fauna of the Republic Introduction of North Macedonia presently includes 67 species from 33 genera, 15 families and seven orders. As many as 12 The Republic of North Macedonia occupies the and 19 species, or ca. 18% and 28% of all records, are central part of the Balkan Peninsula. It has varied relief endemic to North Macedonia and the Balkan Peninsu- structure and age, geology and soil types, a situation la, respectively. The most speciose families are Jul- resulting from its complex geotectonic evolution, which idae, with 29 species, or 43%, followed by Polydesmi- shaped the republic´s present-day rich biodiversity. The dae with 16 species, or 24%. Hirudisoma hirsutum mountains of the older Rhodopian tectonic mass (Mts (Verhoeff, 1901) and Brachydesmus cristofer Strasser, Belasica and Osogovo) and those of the younger Di- 1966 are new to the millipede fauna of North Mace- naric tectonic mass (ar Planina Mountains and Mts donia.