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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. -
Dinámica De La Vegetación Durante El Holoceno En La Sierra De Gredos (Sistema Central Español)
Bol. R. Soc. Esp. Hist. Nat. Sec. Geol., 105 (1-4), 2011, 109-123. ISSN: 0583-7510 Publicado en formato electrónico el día 10 de noviembre de 2011. Dinámica de la vegetación durante el Holoceno en la Sierra de Gredos (Sistema Central Español) Dynamics of vegetation in the Sierra de Gredos (Spanish Central System) during the late Holocene Maria Blanca Ruiz-Zapata1, Rosa M. Carrasco2, María José Gil-García1, Javier de Pedraza3; Laura Razola3, David Domínguez-Villar1 & José Luis Gallardo2 1. Departamento de Geología. Edificio de Ciencias. Universidad deAlcalá. 28871 Alcalá de Henares. [email protected], [email protected], [email protected] 2. Departamento de Ingeniería Geológica y Minera, Universidad de Castilla-La Mancha, Avda. Carlos III, s/n, 45071 Toledo. [email protected]. [email protected] 3. Departamento de Geodinámica, Universidad Complutense, C/ José Antonio Novais, nº 2, 28040, Madrid. [email protected], [email protected] Palabras clave: Polen, Holoceno, Sierra de Gredos, Sistema Central Español. Keywords: Pollen, Holocene, Sierra de Gredos, Spanish Central System. Resumen Se presentan los datos polínicos procedentes de tres secuencias (CH, PD y CbN), localizadas en la Sierra de Gredos (Sistema Central Español), que registran la evolución de la vegetación a partir de los 7000 BP. Los hechos más destacables se resumen en el dominio del pinar, y en el cambio en la composición del bosque local; así, los bosques de Betula y Corylus, desarrollados hasta el 3000 BP son sustituidos por los de Quercus caducifolio y perennifolio. En este momento y solo en la secuencia CH, se detectan presencias de Cedrus y en menor medida de Fagus. -
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. -
GREDOS Definitivo.Qxd
LIBRO DEL PARQUE REGIONAL DE LA SIERRA DE GREDOS PROGRAMA PARQUES NATURALES DE CASTILLA Y LEÓN LIBRO DEL PARQUE REGIONAL DE LA SIERRA DE GREDOS PROGRAMA PARQUES NATURALES DE CASTILLA Y LEÓN Los trabajos de campo realizados para la elaboración del inventario han sido llevados a cabo por alumnos de la Facultad de Ciencias Ambientales de la Universidad de Salamanca y técnicos de la Sección de Espacios Naturales de la provincia de Ávila. Análisis de los datos demográficos: Carlos Gabriel Morales Rodríguez y Pedro Caballero Fernández - Rufete. Dpto. de Geografía de la Universidad de Valladolid. Cartografía: Sara Echevarría Cabezuelo. Ejecución de los trabajos: EXPOGRAFIC, S.A. / TRAGSA Coordinación del trabajo: SERVICIO DE ESPACIOS NATURALES Octubre 2003 ÍNDICE GENERAL 1. INTRODUCCIÓN: PROGRAMA PARQUES NATURALES DE CASTILLA Y LEÓN...................................................2-4 2. EL PARQUE REGIONAL DE LA SIERRA DE GREDOS.....................5-27 3. RESULTADOS DE LA SESIÓN DE PARTICIPACIÓN PÚBLICA........28-37 4. ALGUNAS ACTUACIONES PREVISTAS EN EL PARQUE REGIONAL DE LA SIERRA DE GREDOS.........................................38-48 5. PRINCIPALES FUENTES DE INFORMACIÓN.................................49-50 2 1 INTRODUCCIÓN: Tipología de Términos Municipales PROGRAMA PARQUES NATURALES DE CASTILLA Y LEÓN Antecedentes Generales Densidad de Población El 98% del territorio de la Comunidad de Castilla y León es rural y sus poblaciones están sufriendo, en general, un rápido proceso de envejecimiento y despoblación. Con el fin de afrontar esta situación, se están buscando fór- mulas y modelos que permitan incrementar la calidad de vida en el medio rural de nuestra Comunidad, de forma que se asegure el bienestar de sus poblaciones y se evite el abandono progresivo de nuestros pueblos. -
Nivicolous Myxomycetes from the Sierra De Gredos (Central Spain)
Nova Hedwigia 81 3—4 371—394 Stuttgart, November 2005 Nivicolous Myxomycetes from the Sierra de Gredos (central Spain) by Carlos Lado1*, Anna Ronikier2, Michał Ronikier2, Anna Drozdowicz3 1Real Jardín Botánico (CSIC), Plaza de Murillo 2, 28014 Madrid, Spain [email protected] 2Institute of Botany, Polish Academy of Sciences, Lubicz 46, PL-31-512 Kraków, Poland [email protected], [email protected] 3Institute of Botany, Jagiellonian University, Kopernika 27, PL-31-501 Kraków, Poland [email protected] With 39 figures Lado, C., A. Ronikier, M. Ronikier, A. Drozdowicz (2005): Nivicolous Myxomycetes from the Sierra de Gredos (central Spain). - Nova Hedwigia 81: 371-394. Abstract: First data on the diversity of nivicolous myxomycetes from the Sierra de Gredos, the most important mountain range in central Spain, are reported. Twenty one species have been found in alpine grasslands and shrub communities at altitudes between 1900 and 2250 m. All records are new for the area, and three species, Comatricha cf. rigidireta Nann.-Bremek., Lamproderma splendens Meyl. and Lepidoderma carestianum (Rabenh.) Rostaf., are also recorded for the first time in Spain. Comatricha cf. rigidireta and Lamproderma arcyrioides (Sommerf.) Rostaf. are reported for the first time from nivicolous habitats. Detailed descriptions, comments on morphology, taxonomy and distribution as well as SEM photographs of the most interesting taxa are included. Key words: Distribution, ecology, Eumycetozoa, Iberian Peninsula, Mediterranean region, nivicolous species, SEM microphotographs, taxonomy. Resumen: Se aportan los primeros datos sobre la diversidad de especies quionófilas de Myxomycetes en la Sierra de Gredos, el sistema montañoso mas importante del centro de España. -
Castilla Y Leon CONTENTS
Spain Castilla y Leon Avila Burgos Leon Palencia Salamanca Segovia Soria Valladolid Zamora CONTENTS Introduction 1 A walk through the capital cities Avila 8 Burgos 11 Leon 14 Palencia 17 Salamanca 20 Dublín United Kingdom Segovia 23 Soria 26 Ireland London Valladolid 29 Zamora 32 Enjoying Castilla y Leon 35 Avila. The circus of Gredos 36 París Burgos. Heart of Castille 38 Leon. The Road to Santiago 40 France Palencia. The romanesque 42 Salamanca. The mountains 44 Segovia. The Royal Houses 46 Cantabrian Sea Soria. The lands of el Cid 48 Valladolid. Vineyards and monasteries 50 Castilla y León Zamora. Lakes of Sanabria 52 Leisure and entertainment 54 Madrid Useful information 60 Portugal Lisbon Spain Mediterranean Sea Melilla Ceuta Text: Printed by: Javier Tomé GAEZ, S.A. Translation: D.L. M-24401-2000 Alistair Louis Ross Morocco Maqueta: NIPO: 104-99-042-7 OPCIÓN K, Comunicación Visual, S.L. Printed in Spain Photographs: Archivo Turespaña 1st edition Published by © Turespaña Secretaría de Estado de Comercio y Turismo Ministerio de Economía Introduction the largest region in the European Union. TERRITORY The basic axis of the territory is the basin of the river Duero, If there is one word that sums the largest in Spain. The major up the complex reality of the communication routes region of Castilla y Leon, that between the capital Madrid and word is “monumental”. the Atlantic regions all run Everything about the geography through here. Castilla y Leon, and the culture of this Region, then, is situated in the northern strategically situated in the part of the central Spanish north-east Iberian Peninsula, is plateau. -
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. -
March Newsletter 2021
March 2021 CCAASSTTIILLLLAA YY LLEEÓÓNN [inspira] https://www.turismocastillayleon.com/turismocyl/en Río Duero y Puente Románico, Toro, Zamora THE DUERO ROUTE The Duero Route is one of the most important cultural routes in the south of Europe. This route's itinerary splits the region in two and allows tourists to experience the nature, art and gastronomy that the area has to offer. 80% of this route passes through Soria, Burgos, Valladolid, Zamora and Salamanca, 5 of the provinces making up Castilla y León. The river Duero was an important crossroads for the Peninsula in the past. During the time of the Reconquista, it became a border line. This would explain how a large number of its listed buildings, including the castles and monasteries that had been built, determined the future of the surrounding villages. The Duero Route takes tourists to areas of natural beauty that have been formed by the natural course of the river and become important environmental and fauna reserves. The river Duero is also responsible for irrigating the vineyards of southern Europe's most famous grape and wine growing area. It is also the ideal choice for aquatic activities as cruises along the river and water sports in the dams that have been constructed along the river. TOURISM IDEAS IN CASTILLA Y LEÓN CHERRY BLOSSOM BLOOMING IN THE TIÉTAR VALLEY The Tiétar Valley in the south of Ávila is a true paradise protected from the cold by the Sierra de Gredos mountain range. The differences in altitude between the peaks and the bottom of the valley favour the formation of multiple habitats rich in flora and fauna.