10. Typologies of European Mountain Areas
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In Galicia, Spain (1860-1936)
Finisterra, XXXIII, 65, 1998, pp. 117-128 SUBSTATE NATION-BUILDING AND GEOGRAPHICAL REPRESENTATIONS OF ‘THE OTHER’ IN GALICIA, SPAIN (1860-1936) JACOBO GARCÍA -ÁLVAREZ 1 Abstract: The ‘social construction’ of otherness and, broadly speaking, the ideological-political use of ‘external’ socio-spatial referents have become important topics in contemporary studies on territorial identities, nationalisms and nation-building processes, geography included. After some brief, introductory theoretical reflections, this paper examines the contribution of geographical discourses, arguments and images, sensu lato , in the definition of the external socio-spatial identity referents of Galician nationalism in Spain, during the period 1860-1936. In this discourse Castile was typically represented as ‘the other’ (the negative, opposition referent), against which Galician identity was mobilised, whereas Portugal, on the one hand, together with Ireland and the so-called ‘Atlantic-Celtic nationalities’, on the other hand, were positively constructed as integrative and emulation referents. Key-words : Nationalism, nation-building, socio-spatial identities, external territorial referents, otherness, Spain, Galicia, Risco, Otero Pedrayo, Portugal, Atlantism, pan-Celtism. Résumé: LA CONSTRUCTION D ’UN NATIONALISME SOUS -ETATIQUE ET LES REPRESENTATIONS GEOGRAPHIQUES DE “L’A UTRE ” EN GALICE , E SPAGNE (1860-1936) – La formation de toute identité est un processus dialectique et dualiste, en tant qu’il implique la manipulation et la mobilisation de la “différence” -
Population in the Slovak Carpathian Mountains
Monitoring protocol for the Eurasian lynx (Lynx lynx) population in the Slovak Carpathian Mountains A1. Assessment and selection of sites and lynx for live-capture from the Carpathian source population in Slovakia D1. Monitoring the effects of lynx removal for translocations on the source populations Authors: Kubala J. Smolko P. Klinga P. Tám B. & Kropil R. September 2018 Report for the implementation of action A1 and D1 Realized in the frame of action A1: Assessment and selection of sites and lynx for live-capture from the Carpathian source population in Slovakia Authors: Kubala J. Smolko P. Klinga P. Tám B. & Kropil R. Content 1. Introduction…………………………………………………………………………….5 2. Objectives and attributes……………………………………………………………….7 3. Survey areas…………………………………………………………………………....7 4. Aims and principles of monitoring……………………………………………………11 5. What will be monitored?................................................................................................11 6. Monitoring network…………………………………………………………………...14 7. Passive monitoring: Collecting a chance (opportunistic information)………………..14 8. Active monitoring: Systematic surveys and monitoring system………………………15 8.1. Snow tracking………………………………………………………………………...15 8.2. Opportunistic and standardized collection of samples for genetic analysis…………..16 8.3. Camera trapping………………………………………………………………….......16 8.3.1. Opportunistic camera trapping……………………………………………………17 8.3.2. Deterministic camera trapping………………………………………………….....18 8.4. Captures and GPS/GSM telemetry…………………………………………………...20 9. Survey, monitoring and capture time-frame…………………………………………..22 References…………………………………………………………………………………….23 Foreword The purpose of this protocol is to provide detailed information about the objectives, attributes, sampling design and data management necessary for the implementation of the actions A1 and D1 within the LIFE LYNX - LIFE16 NAT/SI/000634 Together with the protocol on the A2 action in the Romanian Carpathians - Gazzola et al. (2018) it is required by the need to ensure a technical framework for the LIFE Lynx project team. -
Guidelines for Wildlife and Traffic in the Carpathians
Wildlife and Traffic in the Carpathians Guidelines how to minimize the impact of transport infrastructure development on nature in the Carpathian countries Wildlife and Traffic in the Carpathians Guidelines how to minimize the impact of transport infrastructure development on nature in the Carpathian countries Part of Output 3.2 Planning Toolkit TRANSGREEN Project “Integrated Transport and Green Infrastructure Planning in the Danube-Carpathian Region for the Benefit of People and Nature” Danube Transnational Programme, DTP1-187-3.1 April 2019 Project co-funded by the European Regional Development Fund (ERDF) www.interreg-danube.eu/transgreen Authors Václav Hlaváč (Nature Conservation Agency of the Czech Republic, Member of the Carpathian Convention Work- ing Group for Sustainable Transport, co-author of “COST 341 Habitat Fragmentation due to Trans- portation Infrastructure, Wildlife and Traffic, A European Handbook for Identifying Conflicts and Designing Solutions” and “On the permeability of roads for wildlife: a handbook, 2002”) Petr Anděl (Consultant, EVERNIA s.r.o. Liberec, Czech Republic, co-author of “On the permeability of roads for wildlife: a handbook, 2002”) Jitka Matoušová (Nature Conservation Agency of the Czech Republic) Ivo Dostál (Transport Research Centre, Czech Republic) Martin Strnad (Nature Conservation Agency of the Czech Republic, specialist in ecological connectivity) Contributors Andriy-Taras Bashta (Biologist, Institute of Ecology of the Carpathians, National Academy of Science in Ukraine) Katarína Gáliková (National -
The Carpathian Mountains: a Refuge for Wildlife and a “Paradise” for the People of Slovakia by Ted Bailey
Refuge Notebook • Vol. 7, No. 30 • August 5, 2005 The Carpathian Mountains: A refuge for wildlife and a “paradise” for the people of Slovakia by Ted Bailey Although the fireweed was in bloom and brown half the size of state of Kentucky. It is also a relatively bears, wolves, lynx roamed the surrounding forests; new country having gained its most recent indepen- we were not hiking on the Kenai Peninsula or even in dence a mere twelve years ago after the collapse of Alaska. Despite the similarities we were thousands of the Soviet Union. And Slovakia joined the European miles away in Central Europe’s Carpathian Mountains Union in 2004 only a year ago. The huge, stark, tall and in eastern Slovakia. My wife, daughter and I had trav- gray housing complexes built in the country’s largest eled here in July to find four little villages where my cities of Bratislava and Kosice during the communist grandparents lived over a hundred years ago before era contrasted with the beautifully restored old city they emigrated at a young age to America in search centers where Gothic cathedrals and old palaces are of a better life. We eventually found the villages as attractions for visitors. we traveled by car throughout the eastern regions of One day we hiked a trail into the Slovensky Raj, Slovakia known as Spis and Zemplin. Spis is a moun- one of nine national parks and fourteen protected na- tainous region that borders the southern boundary of ture territories in Slovakia. The park was the first pro- Poland. -
266 Final Proposal for a DECISION of the EUROPEAN PARLIAMENT
EUROPEAN COMMISSION Brussels, 2.6.2017 COM(2017) 266 final Proposal for a DECISION OF THE EUROPEAN PARLIAMENT AND OF THE COUNCIL on the mobilisation of the European Globalisation Adjustment Fund following an application from Spain – EGF/2017/001 ES/Castilla y León mining EN EN EXPLANATORY MEMORANDUM CONTEXT OF THE PROPOSAL 1. The rules applicable to financial contributions from the European Globalisation Adjustment Fund (EGF) are laid down in Regulation (EU) No 1309/2013 of the European Parliament and of the Council of 17 December 2013 on the European Globalisation Adjustment Fund (2014-2020) and repealing Regulation (EC) No 1927/20061 (the ‘EGF Regulation’). 2. On 20 January 2017, Spain submitted an application EGF/2017/001 ES/Castilla y León mining for a financial contribution from the EGF, following redundancies2 in the economic sector classified under the NACE Revision 2 Division 5 (Mining of coal and lignite) in the NUTS level 2 region of Castilla y León (ES41) in Spain. 3. Following its assessment of this application, the Commission has concluded, in accordance with all applicable provisions of the EGF Regulation, that the conditions for awarding a financial contribution from the EGF are met. SUMMARY OF THE APPLICATION EGF application EGF/2017/001 ES/Castilla y León mining Member State Spain Region(s) concerned (NUTS3 level 2) Castilla y León (ES41) Date of submission of the application 20 January 2017 Date of acknowledgement of receipt of the 20 January 2017 application Date of request for additional information 3 February 2017 Deadline for provision of the additional 17 March 2017 information Deadline for the completion of the assessment 9 June 2017 Intervention criterion Article 4(2) of the EGF Regulation Sector(s) of economic activity Division 5 (Mining of coal and (NACE Revision 2 Division)4 lignite) Number of enterprises concerned 5 Reference period nine months: 1 February 2016 - 1 November 2016 Total number of redundancies 339 Total number of eligible beneficiaries 339 1 OJ L 347, 20.12.2013, p. -
Saving the Green Heart of Europe
© WILD WONDERS OF E UROPE / CORNELIA ANNUA ANNUAL REVIEW D OERR / WW L REVIE DCP F W 2013 2013 SAVING WW THE GREEN HEART F . PAN OF EUROPE D A WWF Danube-Carpathian Programme . ORG July 2012–June 2013 FY2013 Annual Review – WWF Danube-Carpathian Programme FY2013 Annual Review – WWF Danube-Carpathian Programme A STRUGGLE FOR 15 YEARS THE GREEN HEART OF EUROPE IN THE REGION ”Last year, thousands of Bulgarians poured into the streets in The Danube River basin is the most international river basin protest over amendments to the Forest Law. Now, thousands of in the world, draining 18 countries on its 2,800 km journey Romanians are thronging the streets of Bucuresti and other from the Black Forest in Germany to the Black Sea. From cities outraged over the Romanian government’s abrupt approval the largely untamed middle and lower stretches of the river of gold mining at Rosia Montana. to the spectacular Danube Delta at its mouth, the Danube is home to some of the richest wetland areas in Europe and the The protests at Eagle’s Bridge in Sofia finally convinced the government to amend world. legislation that would have opened the country’s protected forests to development and facilitated corruption; it is still unclear what effect the protests in Romania will have on The Carpathian Mountains, arching across seven countries the Parliament’s final decision regarding gold mining with cyanide in a valuable area of from the Czech Republic across Poland, Slovakia, Ukraine the Carpathian Mountains. “Our goal is to work The two incidents brought into sharp focus a struggle over the future of the re- with others to secure the and Hungary, and down to Romania and the tip of Serbia, gion’s natural riches and the close link to good governance. -
Iberian Forests
IBERIAN FORESTS STRUCTURE AND DYNAMICS OF THE MAIN FORESTS IN THE IBERIAN PENINSULA PABLO J. HIDALGO MATERIALES PARA LA DOCENCIA [144] 2015 © Universidad de Huelva Servicio de Publicaciones © Los Autores Maquetación BONANZA SISTEMAS DIGITALES S.L. Impresión BONANZA SISTEMAS DIGITALES S.L. I.S.B.N. 978-84-16061-51-8 IBERIAN FORESTS. PABLO J. HIDALGO 3 INDEX 1. Physical Geography of the Iberian Peninsula ............................................................. 5 2. Temperate forest (Atlantic forest) ................................................................................ 9 3. Riparian forest ............................................................................................................. 15 4. Mediterranean forest ................................................................................................... 17 5. High mountain forest ................................................................................................... 23 Bibliography ..................................................................................................................... 27 Annex I. Iberian Forest Species ...................................................................................... 29 IBERIAN FORESTS. PABLO J. HIDALGO 5 1. PHYSICAL GEOGRAPHY OF THE IBERIAN PENINSULA. 1.1. Topography: Many different mountain ranges at high altitudes. Two plateaus 800–1100 m a.s.l. By contrast, many areas in Europe are plains with the exception of several mountain ran- ges such as the Alps, Urals, Balkans, Apennines, Carpathians, -
28 Unit 2 Extra Activities
Unit 2 The Earth’s relief Extra activities: Name: Class: Group: Date: 1. Listen to the audio recording, answer the questions and complete the text with the following words: Asia, Pangaea, drift, continent, period, Africa. a) What was Pangaea? What happened to it in the secondary period? b) How did continents appear? c) Explain the continental drift to your partner. d) There was only one in the beginning. It was called . In the secondary continents started to move apart. In the beginning India was attached to but in quaternary it became part of . 2. How many layers make up the Earth? Which one is the outermost? And the innermost? Complete this table and then check your answers with your partner. Layer Subdivisions Depth Melted/Half melted/ Not Melted 3. What are tectonic plates? On which layer are they moving? How do they move? 4. Answer the following questions and then check your answers with your partner. a) How many continents are there in the Eurasian plate? b) Locate Australia on a tectonic plate. c) Which tectonic plate does Argentina belong to? And Brazil? d) Are there many earthquakes in Japan? Why so? 5. What is/are your favourite sport/s? What type of sports could you practise in the following locations? a) The Pyrenees in winter. b) The Pyrenees in summer. c) The Canary Islands any time of the year. 6. Order from highest to smallest the following peaks: Torre Cerredo, Puig Major, Las Villuercas, Mulhacén, Veleta, Teide, Teleno, Aneto, Moncayo. algaida editores, S.A. Authorized photocopiable material. photocopiable Authorized S.A. -
Background and Introduction
Chapter One: Background and Introduction Chapter One Background and Introduction title chapter page 17 © Libor Vojtíšek, Ján Lacika, Jan W. Jongepier, Florentina Pop CHAPTER?INDD Chapter One: Background and Introduction he Carpathian Mountains encompass Their total length of 1,500 km is greater than that many unique landscapes, and natural and of the Alps at 1,000 km, the Dinaric Alps at 800 Tcultural sites, in an expression of both km and the Pyrenees at 500 km (Dragomirescu geographical diversity and a distinctive regional 1987). The Carpathians’ average altitude, how- evolution of human-environment relations over ever, of approximately 850 m. is lower compared time. In this KEO Report, the “Carpathian to 1,350 m. in the Alps. The northwestern and Region” is defined as the Carpathian Mountains southern parts, with heights over 2,000 m., are and their surrounding areas. The box below the highest and most massive, reaching their offers a full explanation of the different delimi- greatest elevation at Slovakia’s Gerlachovsky tations or boundaries of the Carpathian Mountain Peak (2,655 m.). region and how the chain itself and surrounding areas relate to each other. Stretching like an arc across Central Europe, they span seven countries starting from the The Carpathian Mountains are the largest, Czech Republic in the northwest, then running longest and most twisted and fragmented moun- east and southwards through Slovakia, Poland, tain chain in Europe. Their total surface area is Hungary, Ukraine and Romania, and finally 161,805 sq km1, far greater than that of the Alps Serbia in the Carpathians’ extreme southern at 140,000 sq km. -
Contemporary Geomorphic Processes in the Polish Carpathians Under Changing Human Impact
21 by Adam Lajczak1, Wlodzimierz Margielewski2, Zofia Raczkowska3 Jolanta Swiechowicz4 Contemporary geomorphic processes in the Polish Carpathians under changing human impact 1 Pedagogical University, Institute of Geography, 2 Podchorazych Str., 30-084 Cracow, Poland. E-mail: [email protected] 2 Polish Academy of Sciences, Institute of Nature Conservation, 33 A. Mickiewicza Ave., 31-120 Cracow, Poland 3 Polish Academy of Sciences, Institute of Geography and Spatial Organization, 22 Sw. Jana Str., Cracow, Poland 4 Jagiellonian University in Krakow, Institute of Geography and Spatial Management, 7 Gronostajowa Str., 30-387 Cracow, Poland The paper presents activity of contemporary The Polish Carpathians are relatively densely populated (127 2 geomorphic processes in the Polish Carpathians, taking persons/km ), and more than 65% of the population live in rural areas (Dlugosz and Soja, 1995). For this reason man exerts a strong into account human impact on relief transformation in influence on the course of geomorphic processes, but recent processes the past several centuries. and their effects also pose a threat to man. According to Slaymaker Landsliding in the flysch Carpathians is a principal (2010), human activity is a key driver in present-day landscape process in slope transformation, posing the most serious evolution in mountain areas. threat to man, both in the mountains and the foothills. The aim of this paper is to present such mutual relationships within areas showing four types of relief, indicating the most important On the other hand, unsuitable housing on slopes initiates process, type of geomorphic hazard and type and effect of human mass movements, frequently with catastrophic influence on relief transformation, as well as tendencies in these consequences. -
The Landforms of Spain
UNIT The landforms k 1 o bo ote Work in your n of Spain Spain’s main geographical features Track 1 Spain’s territory consists of a large part of the Iberian Peninsula, the Canary Islands in the Atlantic Ocean, the Balearic Islands in the Mediterranean Sea and the autonomous cities of Ceuta and Melilla, located on the north coast of Africa. All of Spain’s territory is located in the Northern Hemisphere. Peninsular Spain shares a border with France and Andorra to the north and with Portugal, which is also on the Iberian Peninsula, to the west. The Cantabrian Sea and the Atlantic Ocean border the north and west coast of the Peninsula and the Mediterranean Sea borders the south and east coast. The Balearic Islands are an archipelago in the Mediterranean Sea. The Canary Islands, however, are an archipelago located almost 1 000 kilometres southwest of the Peninsula, in the middle of the Atlantic Ocean, just north of the coast of Africa. Spain is a country with varied terrain and a high average altitude. Spain’s high average altitude is due to the numerous mountain ranges and systems located throughout the country and the fact that a high inner plateau occupies a large part of the Peninsula. The islands are also mostly mountainous and have got significant elevations, especially in the Canary Islands. Northernmost point 60°W 50°W 40°W 30°W 20°W 10°W 0° 10°E 20°E 30°E 40°E 50°E 60°N Southernmost point Easternmost point s and Westernmost point itie y iv ou ct ! a m 50°N r Estaca o S’Esperó point (Menorca), f de Bares, 4° 19’ E d ATLANTIC 43° 47’ N n a L 40°N ltar Gibra Str. -
Relief Evolution of Landslide Slopes in the Kamienne Mts (Central Sudetes, Poland) – Analysis of a High-Resolution DEM from Airborne Lidar
Contemp.Trends.Geosci., 7(1),2018,1-20 DOI: 10.2478/ctg-2018-0001 Relief evolution of landslide slopes in the Kamienne Mts (Central Sudetes, Poland) – analysis of a high-resolution DEM from airborne LiDAR Aleksandra Osika*, Małgorzata Wistuba, Ireneusz Malik Faculty of Earth Sciences, University of Silesia in Katowice, Bedzinska 60, 41-200 Sosnowiec, Poland * corresponding author: [email protected] Received: 5th November, 2017 Accepted: 9th January, 2018 Abstract The aim of the study is to reconstruct the development of landslide relief in the Kamienne Mountains (Central Sudetes, SW Poland) based on a DEM from LiDAR data. Analyses of relief and geological maps in ArcGIS 10.5 and of slope cross-sections in Surfer 14 allowed to distinguish different types of landslide relief, developed in latites and trachybasalts lying above claystones and mudstones. The types vary from small, poorly visible landslides to vast landslides with complex relief. They were interpreted as consecutive stages of geomorphic evolution of hillslope-valley topography of the study area. Two main schemes have been established which explain the development of landslide slopes in the Kamienne Mts: (1) upslope, from the base of the slope towards the mountain ridge and (2) downslope, beginning on the top of the mountain ridge. The direction of landslide development depends on the thickness of volcanic rocks in relation to underlying sedimentary rocks. When the latter appear only in the lowest part of the slope, landslides develop upslope. If sedimentary rocks dominate on the slope and volcanic rocks form only its uppermost part, landslides develop downslope. The results show that landsliding leads to significant modifications of relief of the study area, including complete degradation of mountain ridges.