266 Final Proposal for a DECISION of the EUROPEAN PARLIAMENT
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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” -
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. -
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. -
On the Tectonic Origin of Iberian Topography
On the tectonic origin of Iberian topography A.M. Casas-Sainz a,?, G. de Vicente b a Departamento de Ciencias de la Tierra, Universidad de Zaragoza, Spain b Grupo de Tectonofísica Aplicada UCM. F.C. Geológicas, Universidad Complutense de Madrid, Spain a r t i c l e i n f o a b s t r a c t Article history: The present-day topography of the Iberian peninsula can be considered as the result of the MesozoicCenozoic– Received 28 January 2008 tectonic evolution of the Iberian plate (including rifting and basin formation during the Mesozoic and Accepted 26 January 2009 compression and mountain building processes at the borders and inner part of the plate, during the Tertiary, Available online xxxx followed by Neogene rifting on the Mediterranean side) and surface processes acting during the Quaternary. The northern-central part of Iberia (corresponding to the geological units of the Duero Basin, the Iberian Chain, Keywords: and the Central System) shows a mean elevation close to one thousand meters above sea level in average, some Iberia Planation surface hundreds of meters higher than the southern half of the Iberian plate. This elevated area corresponds to (i) the Landscape top of sedimentation in Tertiary terrestrial endorheic sedimentary basins (Paleogene and Neogene) and Meseta (ii) planation surfaces developed on Paleozoic and Mesozoic rocks of the mountain chains surrounding the Crustal thickening Tertiary sedimentary basins. Both types of surfaces can be found in continuity along the margins of some of the Tectonics Tertiary basins. The Bouguer anomaly map of the Iberian peninsula indicates negative anomalies related to thickening of the continental crust. -
Estructuras De Unidades Sedimentarias Recientes En La Plataforma Continental De Galicia (NW De España)
Cuaderno Lab. Xeolóxico de Laxe Coruña. 1987. Vol. 12, pp. 35-45 Estructuras de unidades sedimentarias recientes en la plataforma continental de Galicia (NW de España) Structure of recent sedimentary units in the Galician continental shelf REY,]. and DIAZ DEL RIO, V. Los 'perfiles·· de sísmica de reflexión de alta resolución en la plataforma continental gallega nos permiten conocer la estratigrafía de los sedimentos holocenos. De techo a muro se distinguen: - Un nivel superior de limos holocenos marinos con interestratificaciones de arena. - Un reflector basal que aflora hacia ~·ra zona Inedia y externa de la plataforma continental y formado por varias superficies erosionales debidas a lo reducido de los aportes sedimentarios en ese punto. - Un basamento acústico de naturaleza ígnea y metamórfica con una fuerte respuesta sísmica. La plataforma se caracteriza por el desarrollo de dos cuerpos de arena limosa que se extiende hacia mar abierto desde la zona interior de plataforma hacia el sur y una superficie de progradaci6n en la zona externa de la plataforma. El mapa de isopacas demuestra que los sedimentos marinos holocenos forman ... generalmente un lecho contínuo que alcanza su máximo espesor delante de las rías. Palabras clave: Galicia, plataforma continental, holoceno, cuaternario, estratigrafía, sondeos sísmicos. High-resolution seismic reflection profiles of Galician Continental Shelf show the shallow seismic stratigraphy of Holocene sediments. Three acoustic units can be distinguished from top bottom: 36 Rey & Díaz del Río - a continuous upper layer of Holocene marine muds with interstratifications of sand. - a basal reflector which outcrops towards the middle and outer continental shelf, forming several erosional surfaces due to reduced sediment supply. -
Cuaternario Y Geomorfología ISSN: 0214-1744 Y C G Issne: 2695-8589
Cuaternario y Geomorfología ISSN: 0214-1744 y C G ISSNe: 2695-8589 www.rediris.es/CuaternarioyGeomorfologia/ An exploratory study to test sediments trapped by potholes in Bedrock Rivers as environmental indicators (NW Iberian Massif) Un estudio exploratorio para testar los sedimentos atrapados por marmitas de erosión en ríos sobre roca como indicadores ambientales (NO Macizo Ibérico) Álvarez-Vázquez, M.A. (1); De Uña-Álvarez, E. (1) (1) Department of History, Art and Geography, GEAAT Research Group, Campus of Ourense, University of Vigo. As Lagoas s/n, 32004, Ourense, Spain. [email protected] Abstract The capacity of fluvial potholes to trap sediments, together with the geochemical analysis of their stored sediments for environmental assessment, is an overlooked research topic in small bedrock rivers. The present exploratory study is focused on this issue. It was developed in a small river over rock, in the inland territory of Galicia (NW Iberian Peninsula). The study started from an analysis of the inventoried fluvial potholes to identify suitable forms for sampling, and the collection of sediment samples within them. After this, the determination of the grain texture, mineralogy and content of major and trace elements in sediments were carried out. Potholes with maximum vertical depth from 25 cm to 1 m, located in central and sidewall sectors of the bedrock channel, provided the best conditions for sediment sampling. The sediments collected from six potholes showed predominance of coarse-medium grain size and sand fraction. The rough contents of the major and even trace elements are related with the nature of the more refractory minerals of the bed- rock. -
Cytogenetics, Geographical Distribution, Pollen Stainability and Fecundity of five Diploid Taxa of Santolina Rosmarinifolia L
Plant Syst Evol DOI 10.1007/s00606-009-0180-x ORIGINAL ARTICLE Cytogenetics, geographical distribution, pollen stainability and fecundity of five diploid taxa of Santolina rosmarinifolia L. aggregate (Asteraceae: Anthemideae) Aixa O. Rivero-Guerra Received: 22 August 2008 / Accepted: 30 March 2009 Ó Springer-Verlag 2009 Abstract The chromosome analysis of Santolina rosma- Introduction rinifolia subsp. rosmarinifolia, S. oblongifolia, S. semiden- tata subsp. semidentata, S. semidentata subsp. melidensis, Hybridisation and the maintenance of hybrid zones have S. canescens and the hybrid complex (S. rosmarinifolia received considerable attention traditionally because of subsp. rosmarinifolia, S. oblongifolia and their putative their important contribution to the understanding of evo- hybrids) shows that all the taxa are diploids (2n = 2x = 18; lutionary patterns and processes (Barton and Hewitt 1989; 18 ? 1 or more B chromosomes, with 2n = 19, 20 only in Rieseberg 1997; Rieseberg et al. 2007; Barber et al. 2007). the hybrid complex). The results show a conserved general Hybridisation—the production of viable offspring from structure of the karyotype (14m ? 2sm ? 2st), but in interspecific matings—occurs in roughly 10% of animal S. semidentata subsp. melidensis it is variable, with species and 25% of plant species (Larson 1968 cited by 14m ? 2sm ? 2st in ten individuals, 14m ? (1m - 1sm) ? Baack and Rieseberg 2007). Studies of hybrid zones pro- (1 m - 1st) in nine individuals and 12m ? (1m - 1sm) vide insights into evolutionary and speciation processes ? (1m - 1st) ? 2st ? 1B in five individuals. Tetra- (Barton and Hewitt 1981; Harrison 1990; Rieseberg 1995; ploid individuals occurred in the diploid populations of Arnold 1997; Allendorf et al. -
10. Typologies of European Mountain Areas
Mountain Areas in Europe – Final Report 10. Typologies of European mountain areas This chapter brings together data and information presented in the previous chapters, with the aim of providing a diagnosis in the form of three typologies of the mountains of the study area, based on available quantitative information. 10.1 Principles for typology development Chapters 4, 5, 6, 7 have presented a number of profiles and trends within the mountain regions of the study area. The compilation and analysis of this information is a key element of the process to fulfil one objective of the project: to propose typologies of mountain areas in Europe. We have developed three typologies in order to have different composite perspectives on mountain areas, according to the following themes: • social and economic capital; • infrastructure, accessibility and services; • land use and land covers. The social and economic processes taking place in mountain areas are often described. As shown in Chapter 5 and discussed also in Chapter 9, these areas have to struggle with difficult demographic processes (e.g., overageing of population, migration processes) and economic situations (e.g., lack of investment, agriculture remaining as an important sector). The typology on ‘social and economic capital’ draws on data presented in Chapters 5, 6 and 7. The aim of the typology on ‘infrastructure, accessibility and services’ is to provide insight into public infrastructure supply such as universities and airports, as well as linear transport infrastructure as road and railway networks. It brings together many of the issues presented in Chapter 7. The environment is one of the most important fields of concern in mountain areas. -
The Landscapes of Inland Spain
UNIT The landscapes k 1 o o teb of inland Spain o Work in your n Landscapes Track 1 Wherever we look, we can see a landscape. A landscape is an area of land that you can see from a particular point. Elements of a landscape In a landscape, there are natural and man- made elements. Natural elements are things that are not made Natural elements by man: • Relief, such as mountains, plains and valleys. • Water, such as rivers, seas and lakes. • Vegetation, or plants, and the fauna, or all the animals. Man-made elements are the things that are made by man. These include houses, roads and train tracks. Man-made elements Changes in landscapes Over time, all landscapes change. These changes can be caused by nature or by man. • Natural causes can be earthquakes, floods and volcanic eruptions. Natural causes can destroy buildings, bridges and vegetation. • Man-made causes can be the building of roads, buildings, tunnels and bridges. Man-made causes can change the landscape a lot. 1 What are the elements of landscapes? Give two examples of each. 2 Think about the landscape where you live and answer the questions in your notebook. olcan n v o! w o 1 How has it changed? r u o y 2 Are these changes man-made or natural? e k a 3 Are these changes positive or negative? M 4 Unit 1 Interior landscapes Track 2 Mountain landscapes Mountains are the most common landform in mountain landscapes. • The highest part is called the summit. • The lowest part is called the foot. -
Los Bosques Y El Sector Forestal En España/ Los Bosques Y El Sector Forestal 00 Cubiertas Página 2 Modelo Cap 06
00_cubiertas Página 1 modelo cap 06 El objetivo de esta monografía es ofrecer una recopilación de datos acerca de las principales fuentes de información actualmente disponibles para la comprensión del estado actual de los montes en Es- Los bosques y el sector paña, la ubicación y la composición de las principales catenas que se dan en nuestras montañas y una breve información sobre las especies forestales más relevantes en cuanto a su papel a nivel de pai- saje. La lista incluye especies del género Quercus (ocho especies), el género Pinus (siete especies), el forestal en España/ género Abies (dos especies), el género Betula (dos especies), el género Fraxinus (dos especies), Fagus sylvatica, Juniperus thurifera y Olea europaea var. sylvestris. También se presenta información sobre Forest and forestry las áreas naturales protegidas, junto con algunos datos sobre la diversidad de los bosques y su im- portancia económica, así como algunas actividades de investigación relacionadas en el sector fores- in Spain tal que se ha desarrollado en el CIFOR-INIA en los últimos años. The aim of this monograph is to offer a compilation of data about the main information sources actually Jesús de Miguel available for understanding Spanish forestry, the location and composition of the forest catenae in David Sánchez de Ron Spanish mountains and brief information about forest tree species that are relevant at landscape level. Francisco Javier Auñón The species list includes genus Quercus (eight species), genus Pinus (seven species), genus Abies (two José Manuel García del Barrio especies) genus Betula (two species), genus Fraxinus (two species), Fagus sylvatica, Juniperus thurifera and Olea eurapaea var. -
Goodwood Road Racing Club Iberian Peninsula Driving Tour 23 September – 2 October 2018
GOODWOOD ROAD RACING CLUB IBERIAN PENINSULA DRIVING TOUR 23 SEPTEMBER – 2 OCTOBER 2018 Long before F1 became established at the Circuit de Catalunya near Barcelona, Spain was in love with motor racing. The first Spanish Grand Prix took place in 1913 and was run to touring car rules on a 300 kilometre route near Madrid. Thereafter, racing took place around the country, most notably at Sitges, Jarama and Jerez. When the Monte Carlo rally was in full swing in the 1960’s Spain was one of the starting points for entrants converging on Reims for the run to the South of France. We are delighted to confirm details of our 2018 European driving tour to the Iberian Peninsula. This trip has been created to provide Members and their guests with a memorable and exclusive opportunity to drive some stunning roads in the mountains and vineyards of Spain, alongside travelling down into Northern Portugal. In addition to the fabulous driving roads, we will be staying in luxury 4* and 5 * hotels situated in some fantastic locations along the route. Highlights will include the Picos Europa, the Galician Massif, the Douro Valley in Portugal and the Ribera del Duero in Spain. We will be travelling to and from Spain with Brittany Ferries. If Members would prefer to fly (and have their cars transported) we will gladly organise this if there are sufficient numbers. DATES Sunday 23 September to Monday 1 October 2018 (inclusive) returning to Portsmouth on Tuesday 2 October 2018 Day 1 – Sunday 23 September RV Time – Departure: 0800hrs – 0930hrs Check in at Brittany Ferries: 1415hrs Expected driving time: 3hrs 45mins Expected driving distance: 190 miles Ferry Departure from Plymouth: 1545hrs Members and their guests are requested to meet at The Kennels for registration and a briefing about the trip over tea and coffee.