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Estudio Territorial Extremadura II EL SISTEMA FISICO - NATURAL
Estudio Territorial Extremadura II EL SISTEMA FISICO - NATURAL ESTUDIO TERRITORIAL EXTREMADURA II TOMO I EL SISTEMA FÍSICO - NATURAL DICIEMBRE 1.996 Estudio Territorial Extremadura II EL SISTEMA FISICO - NATURAL INDICE TOMO I 1. INTRODUCCION. EL ESTUDIO TERRITORIAL EXTREMADURA II 1 2. LAS GRANDES UNIDADES MORFOESTRUCTURALES DE EXTREMADURA 6 2.1. SIERRA DE GATA - LAS HURDES 10 2.2. TERMINACIÓN ORIENTAL DEL MACIZO DE GREDOS 10 2.3. LLANURA DEL ALAGÓN 10 2.4. CAMPO ARAÑUELO (EL TAJO) 11 2.5. LAS VILLUERCAS 12 2.6. LA MESETA CACEREÑA 13 2.7. ALINEACIÓN DE LA SIERRA DE SAN PEDRO, SIERRA DE MONTÁNCHEZ 13 2.8. VEGAS DEL GUADIANA 14 2.9. OSSA MORENA OCCIDENTAL: SIERRAS DE JEREZ - UMBRAL DE ZAFRA 15 2.10. OSSA MORENA ORIENTAL: LLANOS Y SIERRAS DE LLERENA 15 2.11. LA SERENA 16 3. GEOLÓGÍA 17 3.1. INTRODUCCION Y ENCUADRE GEOLOGICO 17 3.1.1. LAS GRANDES UNIDADES TECTONOESTRATIGRÁFICAS 17 3.1.1.1. Zona Centro - Ibérica 18 3.1.1.2. Zona de Ossa Morena 19 3.1.1.3. Propuesta de síntesis geológica del suroeste ibérico 19 3.2. ESTRATIGRAFIA 24 3.2.1. PRECÁMBRICO 24 3.2.1.1. Terreno de Valencia de las Torres - Cerro Muriano 24 3.2.1.2. Terreno de Sierra Albarrana 26 3.2.1.3. Depósitos sinorogénicos finiprecámbricos 27 3.2.2. PALEOZOICO 30 3.2.2.1. Cámbrico 30 3.2.2.2. Paleozoico inferior - medio 33 3.2.2.3. Carbonífero 37 Estudio Territorial Extremadura II EL SISTEMA FÍSICO - NATURAL 3.2.3. NEÓGENO - CUATERNARIO 39 3.2.3.1. -
Social Science
3 Social Science Social Science Learning Lab is a collective work, conceived, designed and created by the Primary Educational department at Santillana, under the supervision of Teresa Grence. WRITERS Natalia Gómez María More ILLUSTRATIONS Dani Jiménez Esther Pérez-Cuadrado SCIENCE CONSULTANT Raquel Macarrón EDITOR Sara J. Checa EXECUTIVE EDITOR Peter Barton BILINGUAL PROJECT COORDINATION Margarita España Do not write in this book. Do all the activities in your notebook. Contents Get started! .............................. 6 1 The relief of Spain ................ 8 2 Our rivers ............................ 22 Learning Lab game ............. 36 3 We live in Europe ................ 38 4 Our world ........................... 52 Learning Lab game ............. 66 5 Studying the past ............... 68 6 Discovering history ............. 82 Learning Lab game ............. 96 Key vocabulary ................... 98 three 3 UNIT CONTENTS RAPS MINI LAB / BE A GEOGRAPHER! FINAL TASK 1 • Inland and coastal landscape features • Main features of the relief of Spain The relief rap • Compare landscapes Expedition to an autonomous community The relief of Spain • Parts of a mountain • Highest mountains and mountain • Mountain presentation ranges in Spain • Relief maps • How do you read a relief map? 2 • Types of rivers • River maps The river rap • How are watersheds similar Expedition on a river Our rivers • Parts of a river • Cantabrian rivers • How do you read a watershed map? • Features of a river • Atlantic rivers • Spanish rivers • Mediterranean rivers -
Capítulo 7 LIBRO GEOLOGÍA DE ESPAÑA Sociedad Geológica De España Instituto Geológico Y Minero De España
Capítulo 7 LIBRO GEOLOGÍA DE ESPAÑA Sociedad Geológica de España Instituto Geológico y Minero de España 1 Índice Capítulo 7 7- Estructura Alpina del Antepaís Ibérico. Editor: G. De Vicente(1). 7.1 Rasgos generales. G. De Vicente, R. Vegas(1), J. Guimerá(2) y S. Cloetingh(3). 7.1.1 Estilos de deformación y subdivisiones de las Cadenas cenozoicas de Antepaís. G. De Vicente, R. Vegas, J. Guimerà, A. Muñoz Martín(1), A. Casas(4), N. Heredia(5), R. Rodríguez(5), J. M. González Casado(6), S. Cloetingh y J. Álvarez(1). 7.1.2 La estructura de la corteza del Antepaís Ibérico. Coordinador: A. Muñoz Martín. A. Muñoz-Martín, J. Álvarez, A. Carbó(1), G. de Vicente, R. Vegas y S. Cloetingh. 7.2 Evolución geodinámica cenozoica de la Placa Ibérica y su registro en el Antepaís. G. De Vicente, R. Vegas, J. Guimerà, A. Muñoz Martín, A. Casas, S. Martín Velázquez(7), N. Heredia, R. Rodríguez, J. M. González Casado, S. Cloetingh, B. Andeweg(3), J. Álvarez y A. Oláiz (1). 7.2.1 La geometría del límite occidental entre África y Eurasia. 7.2.2 La colisión Iberia-Eurasia. Deformaciones “Pirenaica” e “Ibérica”. 7.2.3 El acercamiento entre Iberia y África. Deformación “Bética”. 7.3 Cadenas con cobertera: Las Cadenas Ibérica y Costera Catalana. Coordinador: J. Guimerá. 7.3.1 La Cadena Costera Catalana. J. Guimerà. 7.3.2 La Zona de Enlace. J. Guimerà. 7.3.3 La unidad de Cameros. J. Guimerà. 7.3.4 La Rama Aragonesa. J. Guimerà. 7.3.5 La Cuenca de Almazán. -
Official Journal CE 364, 20/12/2001, P
20.12.2001 EN Official Journal of the European Communities C 364 E/145 Answer given by Mr Bolkestein on behalf of the Commission (26 July 2001) Acting on the complaint to which the Honourable Member refers, the Commission studied the relevant legislation and asked the French authorities for further information, following which they were sent a letter of formal notice. The French legislation categorically rules out discharge of withholding tax at the special rate (taux du prélèvement libératoire) where income is derived from investments or policies under Articles 125-0 and Article 125 A of the Code Général des Impôts (CGI) and the person liable is not resident or established in France. The Commission considers this to be incompatible with Articles 49 (ex 59) and 56 (ex 73B) of the EC Treaty. In the light of the French authorities’ reply to the letter the Commission will shortly decide whether to issue a reasoned opinion under Article 226 (ex 169) of the EC Treaty. (2001/C 364 E/160) WRITTEN QUESTION E-1554/01 by María Rodríguez Ramos (PSE) to the Commission (28 May 2001) Subject: A thermal power plant to be built in Tordesillas, Spain The American multinational ENRON wants to build an 800 megawatt natural gas and diesel oil power plant on the outskirts of Tordesillas which, according to data supplied by the company, will release 2 540 000 tonnes of carbon dioxide (the main cause of climate change), 2 100 tonnes of nitrogen oxides, 191 tonnes of sulphur dioxide, 545 tonnes of carbon monoxide and other pollutants into the atmosphere every year. -
A Typological Calssification Os Spanish Precious Metals Deposits
Caderno Lab. Xeolóxico de Laxe Coruña. 1995. Vol. 20, pp. 253-279 A typological classification ofSpanish precious metals deposits Clasificación tipológica de los yacimientos españoles de metales nobles CASTROVIE]O, R. Last decade's intensive exploration for precious metals in Spain led to a new understanding ofvarious types ofdeposits and prospects. A summary review of recent progress is presented, allowing the systematic (typological) classification ofthe Spanish precious metals deposits shown in Table 1: 19 types are defined in the framework ofthe Iberian Geology, their exploration significance being also considered. Hypogene deposits in the Hercynian Hesperian Massif, and epithermal gold deposits in the Neogene calc-alcaline Volcanic Province ofSE Spain have been very much explored and are therefore emphasized, although their mining production is by far not to compare with the precious metals output the SWIPB (SW Iberian Pyrite Belt). IntheHesperian Massif, different metalloterts have beendemonstrated tobe related toattractiveconcentrations ofgold, bound to Hercynianshear-zones, inGalicia, in Extremadura, etc.; other concentrations (e. g., in Galicia and Asturias) are related to granite or porphyry intrusions (Salave) and skarn formations (Carlés). PGE or Platinum elements (± chromite) have been found in ophiolitic thrust complexes occurring in N Galicia, e. g. the HerbeiraMassifofthe Cabo Ortegal Complex, as had been in the 1940's in N orthern Portugal(Bragan\aand Morais complexes). Exploration for silver has demonstrated a small orebody in Fuenteheridos (Aracena, SW Spain), not minable under severe environmental constraints, but none ofthe classic Spanish silver producing districs (vein-Type deposits, e. g. Guadalcanal or Hiendelaencina) has recovered activity. Most ofthe EU (European Union) gold and silver production is won from only two types ofdeposits in the Spanish Hesperian Massif: the masive sulphides of the SWIPB, in which precious metals are won as by-products, and the related gossan deposits. -
Simulations of Mesoscale Circulations in the Center of the Iberian Peninsula for Thermal Low Pressure Conditions
880 JOURNAL OF APPLIED METEOROLOGY VOLUME 40 Simulations of Mesoscale Circulations in the Center of the Iberian Peninsula for Thermal Low Pressure Conditions. Part I: Evaluation of the Topography Vorticity-Mode Mesoscale Model FERNANDO MARTIÂN,SYLVIA N. CRESPIÂ, AND MAGDALENA PALACIOS Departmento de Impacto Ambiental de la EnergõÂa, Centro de Investigaciones EnergeÂticas, Medioambientales y TecnoloÂgicas, Madrid, Spain (Manuscript received 27 September 1999, in ®nal form 10 August 2000) ABSTRACT The Topography Vorticity-Mode Mesoscale (TVM) model has been evaluated for four different cases of thermal low pressure systems over the Iberian Peninsula. These conditions are considered to be representative of the range of summer thermal low pressure conditions in this region. Simulation results have been compared with observations obtained in two intensive experimental campaigns carried out in the Greater Madrid Area in the summer of 1992. The wind ®elds are qualitatively well simulated by the model. Detailed comparisons of the time series of simulations and observations have been carried out at several meteorological stations. For wind speed and direction, TVM results are reasonably good, although an underprediction of the daily thermal oscillation has been detected. The model reproduces the observed decoupled ¯ow in the nighttime and early morning along with the evolution of mixing layer ¯ow during the day. In addition, the model has simulated speci®c features of the observed circulations such as low-level jets and drainage, downslope, upslope, and upvalley ¯ows. The model also simulates the formation of hydrostatic mountain waves in the nighttime in some cases. 1. Introduction mal low dominates summer atmospheric conditions. In spite of the high frequency of this mesoscale pressure The Greater Madrid Area is located in a 700-m high system in the south of Europe and in other parts of the plateau at the center of the Iberian Peninsula. -
El Glaciarismo En La Península Ibérica
EL GLACIARISMO EN LA PENÍNSULA IBÉRICA EL FENÓMENO GLACIAR CUATERNARIO EN LA PENÍNSULA IBÉRICA Quaternary Glaciation in the Iberian Peninsula Eduardo Acaso Deltell (*) RESUMEN Se describe el fenómeno glaciar pleistoceno que afectó a las principales cadenas montañosas de la península. Se define el glaciarismo como de montaña con formación de glaciares de valle (donde son abundantes los aparatos de decenas de Km de longitud) y formas menores así como glaciares rocosos y, en algún caso, de montera. El mayor desarrollo se produjo en los Pirineos en donde aún existen glaciares funcionales. El modelo de evolución consta de un máximo (en torno a 70.000-38.000 BP para la cadena pirenaica) y un período de estabilización a partir del cual se da un retroceso generalizado en donde, en la mayoría de los macizos, puede hablarse de un episodio de glaciares de valle, otro de glaciares de circo y un Tardiglaciar (entre 17.300 y 9.000 BP) definido por glaciares residuales. Finalmente, en algunas ca- denas se detecta una reactivación del fenómeno glaciar durante la Pequeña Edad del Hielo (siglos XIII- XIX). ABSTRACT This is a description of the glacial processes that affected the Iberian Peninsula along the Quaternary. Mountain glaciers (valley, cirque and rock-glacier) can be identified. The maximum development was concentrated in the Pyrenees (where still survive some active glaciers) and this maximum happened ap- proximately between 70000 and 38000 years BP. Later, a retreat period affect most areas of the Iberian Peninsula, leaving a period of valley glaciers, a period of cirque glaciers and a late-glacial period (17300-9000 y BP) with only residual glaciers. -
Six Rer11i Nders ; ··· ·' F.!5 Tra~ Vellers ...· R"I
Ricardo Castto ~ t' I l .,l "t :: lar, ; I ; six rer11i nders ; ··· ·' f.!5 tra~ vellers ...· r"i. ~ >~,· ; . ;r. :,I 26 The Fifth Column Ricar<Jo Castro Dl WACKISE £T lDIT 0 0 volume eight, nwnber three on the rood .. 27 Ricardo Casrro SIX REMINDERS FOR TRAVELLERS. Canals, Spanish canals, particularly the Canal de Castilla. Spain is engraved with canals. Transport, (exchange of goods, displacement of people) and irrigation, (movernem or dispersion of water) are, separately or combined, the two main drivmg forces for the construction of canals. A variety of minor works and utopian projects were begun and promoted as early as the first part of the sixteenth century, a time during which Spain began its political consolidation undec the Catholic Kings. A few years later, between 1548 and 1550, during the reign of Maximillian of Austria interest in fluvial navigation in Spain became a renewed imperative. It is from this time, for instance, that the first Spanish extant drawing of a revolving lock: which closed with the aid of the current, comes to us•. But it is only in the mid- eighteenth century, during the reign of Ferdinand VI, that the first major navigable-irrigation waterworks, the Canal de Castilla and the Imperial Canal of Arag6n, were bwlL Both canals, among the most extraordinary hydraulic monuments of Spain, fonn part of the extensive series of public works including roads, dams, docks, bridges, silos, hospitals, schools and even bullfight rings, initiated and promoted during the Spanish Enlightenment (La Uustraci6n Espai'lola). They would play a more significant role during the nineteenth century. -
IRS 2016 Proposal Valladolid, Spain
CANDIDATE TECHNICAL DOSSIER FOR International Radiation Symposium IRS2016 In VALLADOLID (SPAIN), August 2016 Grupo de Optica Atmosférica, GOA-UVA Universidad de Valladolid Castilla y León Spain 1 INDEX I. Introduction…………………………………………………………............. 3 II. Motivation/rationale for holding the IRS in Valladolid………………....….. 3 III. General regional and local interest. Community of Castilla y León…......... 4 IV. The University of Valladolid, UVA. History and Infrastructure………….. 8 V. Conference environment …………………………………………………. 15 VI. Venue description and capacity. Congress Centre Auditorium …….…… 16 VII. Local sites of interest, universities, museums, attractions, parks etc …... 18 VIII. VISA requirements …………………………………………………….. 20 2 IRS’ 2016, Valladolid, Spain I. Introduction We are pleased to propose and host the next IRS at Valladolid, Spain, in August of 2016, to be held at the Valladolid Congress Centre, Avenida de Ramón Pradera, 47009 Valladolid, Spain. A view of the city of Valladolid with the Pisuerga river II. Motivation/rationale for holding the IRS in Valladolid Scientific Interest In the last decades, Spain has experienced a great growth comparatively to other countries in Europe and in the world, not only in the social and political aspects but also in the scientific research. Certainly Spain has a medium position in the world but it potential increases day by day. The research in Atmospheric Sciences has not a long tradition in our country, but precisely, its atmospheric conditions and geographical location makes it one of the best places for atmospheric studies, in topics as radiation, aerosols, etc…. , being a special region in Europe to analyse the impact of climate change. Hosting the IRS’2016 for the first time in Spain would produce an extraordinary benefit for all the Spanish scientific community, and particularly for those groups working in the atmospheric, meteorological and optics research fields. -
La Música Tradicional En Valladolid Y Su Papel Durante La Transición
La música tradicional en Valladolid y su papel durante la Transición Folk music in Valladolid during the Spanish transition Antonio BELLIDO BLANCO Museo Fabio Nelli Resumen Los años de la transición estuvieron marcados por la reafirmación de la identidad de las dis- tintas regiones españolas. Las tierras vallisoletanas, dentro del contexto de lo que luego sería la Comunidad Autónoma de Castilla y León, no fueron ajenas a esta situación. Una de sus manifestaciones fue la exaltación de su música tradicional. A través de este trabajo analiza- remos la implicación que tuvieron, en este momento histórico, la mayoría de grupos folklóri- cos en la actividad de distintas formaciones políticas regionales. Palabras clave: Transición política; Música folkórica; Valladolid. Abstract During the transition’s years the reaffirmation of the identity were accentuated in the Spanish regions. The province of Valladolid, within the context of the former Autonomy of Castilla y León, wasn’t strange to this situation. One of its demonstrations was the folk music’s exalta- tion. In this study we look into the involvement of the most of folk music bands with the activi- ties of regional political parties in this historical time. Keywords: Political Transition; Folk Music; Valladolid. La música es una relevante manifestación cultural en todas las épocas y en to- dos los lugares. Se imbrica en las celebraciones religiosas y festivas, pero tam- bién en las labores cotidianas, así como en la vida pública y en la intimidad familiar. Su presencia constante ha sido, tal vez, lo que ha propiciado su estu- dio, por más que se centre por lo general en figuras concretas (compositores o intérpretes) o en lo que rodea a fiestas determinadas. -
Medina D San Vicente Medina Del Campo. Fairs City N
MEDINA DDEL CAMPO. FAIRS CITY Medina del Campo, Fairs City, iis known for its Fairs all overr Europe. In the 15th and 16th centuries, the fairs broughtbrou a lot of wealth into the townown and suchsuc wealth allowed the buildinglding of beautiful religious and civil monuments thatt have contributed to makee Medina oneon of the most well-know placesaces in SpaiSpain for its historical and artisticstic heritage. Many building have been destroyed throughoutthr the centuries, such as great walls,wall gates, somes palaces, manyy churches, convents,c monasteries etc. However,owever, partpar of the magnificent architecturalctural past of the town can still be seen. The old part of the ttown became a “listed historical complex”mplex” in 1991.Thanks19 to the railway, Medina gotot itsits status oof road junction back. The service sector,ector, the agricultureagr and the wood transformationn industry hahave become the economic motor of the 19th and 220th Centuries. Medina del Campo recoveredcovered its mythical 20.000 inhabitans in the mid-eighties. Holy week was declared of Regional Tourist InterestInter in 1993, of National Tourist Interestterest in 2005 and International Tourist Interest in 2011. The Holly Week of Medina del Campo has the oldeoldest processions of Spain. Nowadays,, the Holy WWeek of Medina has about thirty pasosos and more ffifteen processional marches SANN VICENTE FERRER CULTURALAL CENTRCENTRE HUELLASLLAS DE PAPASION INTERPRETATIONION CENTRECENTR Passion Traceses InterpretatInterpretation Centre can be found in the Hermititageage of NueNuestra Señora del Amparo and in new modernsoderns building,buildi next to the Historical and a Commercialial Centre of the Village, 250 metres fron thee great Plaza Mayor de la Hispanidad PASSION TRACES INTERPRETATIONN CENTRE The propuse for this innovative sspace is to immerse the visitor in a experience of sensations wich approach them to the originorig of the Easter Week and its processions, to the Passsion week of the Village and to the religious heritage of our town. -
Comparative Chorology Between Podarcis Bocagei and P. Carbonellae
Rev. Esp. Herp. (2001) 15:85-97 85 Comparative chorology between Podarcis bocagei and P.carbonellae (Sauria: Lacertidae) in Portugal PAULO SÁ-SOUSA Lab. Biologia da Conservação Dep. Biologia, Univ. Évora P-7002-544 Évora, Portugal. e-mail: [email protected] Abstract: The geographic distributions of the Bocage’s wall lizard, Podarcis bocagei and the Carbonell’s wall lizard, P. carbonellae in Portugal were determined through extensive field surveys. The river Douro constitutes the main geographical barrier where both lizard species show nearby a zone of contact. Predictive models of probability of occurrence were developed for both species in Portugal, based on the Logistic Multiple Regres- sion (LMR) and the Overlap Analysis (OA). On a coarse scale, the best-fit model suggested that the distribution of P. bocagei in Portugal might be largely explained by macroenvironmental variables such as radiation, eva- potranspiration or type of climate. The balance between the number of frost days per year and a coefficient of aridity (Kdr = 100 × temperature/precipitation) seems important to explain the range of P. carbonellae. Howe- ver, the large overlap found between predictive areas strongly suggest that historical events (e.g. Pliocene spe- ciation, Pleistocene glacial refugia) might have been preponderant, acting the macroenvironmental factors as ultimate determinants of the present-day distribution of both species. The distribution of P. bocagei is signi- ficantly congruent with that of Chioglossa lusitanica, partially with Vipera seoanei and with Rana iberica and Lacerta schreiberi northwards the river Douro. Conversely, the contractive distribution of P. carbonellae did not share any significant pattern of congruence with the latter taxa.