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Dirección General De Carreteras E Infraestructuras Carreteras De La Comunidad De Madrid
DIRECCIÓN GENERAL DE CARRETERAS E INFRAESTRUCTURAS CARRETERAS DE LA COMUNIDAD DE MADRID CARRETERA DEFINICION PUNTO INICIO PUNTO FINAL LONGITUD TIPO DE RED MUNICIPIOS POR LOS QUE PASA Ajalvir Algete Alcalá de Henares De M-203 y M-300 (Alcalá de Henares) a A-1 San Sebastián de los Reyes Alcalá de Henares M-100 M-300 24,830 Principal por Cobeña A-1 Cobeña M-203 Daganzo de Arriba San Sebastián de los Reyes Patones De N-320 (Torrelaguna) a límite de provincia Torrelaguna Límite provincia Guadalajara M-102 10,750 Secundaria Torrelaguna con Guadalajara por Patones de Abajo N-320 Patones Torremocha del Jarama Algete Cobeña Cobeña Talamanca del Jarama Fuente El Saz de Jarama M-103 De M-111 a N-320 por Algete 25,790 Secundaria M-100 M-320 Paracuellos de Jarama Talamanca de Jarama Valdetorres de Jarama De A-1 (San Agustín de Guadalix) a San Agustín de Guadalix Colmenar Viejo Colmenar Viejo M-104 14,370 Secundaria M-607 (Colmenar Viejo) A-1 M-607 San Agustín de Guadalix Algete San Sebastián de los Reyes Algete M-106 De M-103 (Algete) a M-100 4,490 Secundaria M-103 M-100 San Sebastián de los Reyes Ajalvir De A-2 (Torrejón de Ardoz) a M-100 (Daganzo Torrejón de Ardoz Daganzo de Arriba M-108 8,980 Principal Paracuellos de Jarama de Arriba) A-2 M-100 Torrejón de Ardoz Algete Fuente El Saz de Jarama De M-13 (Barajas) a M-103 (Fuente el Saz de Barajas Fuente El Saz de Jarama M-111 24,480 Principal Madrid Jarama) M-13 M-103 Paracuellos de Jarama San Sebastián de los Reyes De M-123 (Alalpardo) a M-103 (Fuente el Saz Alalpardo Fuente El Saz de Jarama Fuente -
Recent Tectonic Model for the Upper Tagus Basin (Central Spain)
ISSN (print): 1698-6180. ISSN (online): 1886-7995 www.ucm.es/info/estratig/journal.htm Journal of Iberian Geology 38 (1) 2012: 113-126 http://dx.doi.org/10.5209/rev_JIGE.2012.v38.n1.39208 Recent tectonic model for the Upper Tagus Basin (central Spain) Modelo tectónico reciente de la Cuenca Alta del Tajo (parte central española) J.L. Giner-Robles*1, R. Pérez-López 2, P.G. Silva 3, A. Jiménez-Díaz 4, M.A. Rodríguez-Pascua 2 1 Dpto. Geología y Geoquímica. Facultad de Ciencias. Campus de Cantoblanco, Universidad Autónoma de Madrid. 28049- Madrid, Spain. [email protected] 2 IGME – Instituto Geológico y Minero de España. Área de Investigación y Peligrosidad en Riesgos Geológicos C/ Ríos Rosas 23, 28003 Madrid, Spain [email protected], [email protected] 3 Dpto. Geología, Escuela Politécnica Superior de Ávila, Universidad de Salamanca. Avda. Hornos Caleros, 50. 05003-Ávila.España. Email: [email protected] 4 Dpto. de Geodinámica. Facultad de Ciencias Geológicas. Universidad Complutense de Madrid. 28040 - Madrid. España (Spain). Email: [email protected] *Corresponding author Received: 08/12/2011 / Accepted: 08/03/2012 Abstract Active tectonics within the Upper Tagus Basin is related to the lithospheric flexure affecting the Palaeozoic basement of the basin. This flexure displays NE-SW trending. Besides, this structure is in agreement with the regional active stress field defined by the maximum horizontal stress with NW-SE trending. In this tectonic framework, irregular clusters of instrumental seismicity (Mw< 5.0) fade in the zone bounded by the Tagus River and the Jarama River valleys. -
Presentación De Powerpoint
Monjes del Paular en Getafe 1 ª parte PRESENTACIÓN TALLER HABLEMOS DE GETAFE – CASA DEL MAYOR TALLER HABLEMOS DE GETAFE – CASA DEL MAYOR – 19-XII- 2013 Monjes del Paular en Getafe TALLER HABLEMOS DE GETAFE – CASA DEL MAYOR – 19-XII- 2013 TALLER HABLEMOS DE GETAFE – CASA DEL MAYOR – 19-XII- 2013 TALLER HABLEMOS DE GETAFE – CASA DEL MAYOR – 19-XII- 2013 Durante sus primeros cuatro siglos y medio de existencia, El Paular, concluido en 1442 bajo el reinado de Juan II y totalmente remodelado por Juan de Guas, arquitecto de los Reyes Católicos, se convirtió en una de las cartujas más poderosas del continente europeo, hasta el punto de que en 1515 pudo permitirse el lujo de costear la construcción de la cartuja de Granada. Su importancia económica fue notable, ya que disponía, entre otras fuentes de ingresos, de una cabaña real con 86.000 ovejas merinas y de su “molino de papel”, en el que se imprimió la editio princeps del Quijote. Sus posesiones rústicas y urbanas, agrupadas en torno a la Conrería situada en Talamanca del Jarama y en el señorío de Getafe (Madrid), eran inmensas, de tal modo que alguien las tituló con el sugerente mote de “ministerio de hacienda de los cartujos”. http://monasteriopaular.com/historiacartuja2.html http://www.foroxerbar.com/viewtopic.php?t=10326 TALLER HABLEMOS DE GETAFE – CASA DEL MAYOR – 19-XII- 2013 RELACIONES HISTÓRICO-GEOGRÁFICAS-ESTADÍSTICAS DE GETAFE MANDADAS HACER POR FELIPE II, SEGÚN EL INTERROGATORIO DE 1575 “ los edificios del pueblo casi todos son iguales en obras y materiales, salvo en hacer unos altos e otros bajos. -
ESR Dating of Middle Pleistocene Archaeo-Paleontological Sites from the Manzanares and Jarama River Valleys (Madrid Basin, Spain)
Quaternary International 520 (2019) 23e38 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint ESR dating of Middle Pleistocene archaeo-paleontological sites from the Manzanares and Jarama river valleys (Madrid basin, Spain) * Davinia Moreno a, , Mathieu Duval b, Susana Rubio-Jara c, Joaquín Panera a, Jean Jacques Bahain d, Qingfeng Shao e, Alfredo Perez-Gonz alez a, Christophe Falgueres d a Centro Nacional de Investigacion sobre la Evolucion Humana (CENIEH), Paseo Sierra de Atapuerca, 3, 09002, Burgos, Spain b Australian Research Centre of Human Evolution (ARCHE), Environmental Futures Research Institute (EFRI), Griffith University, 170 Kessels Road, Nathan, QLD 4111, Australia c Instituto de Evolucion en Africa (IDEA), Museo de San Isidro, Plaza de San Andres, 2, Madrid, Spain d Departement de Prehistoire, Museum National d’Histoire Naturelle, UMR 7194, 1, Rue Rene Panhard, 75013, Paris, France e College of Geographical Science, Nanjing Normal University, Nanjing, 210023, China article info abstract Article history: In this work, three important Pleistocene sites of the Madrid basin located close to the junction of the Received 26 April 2017 Manzanares (PRERESA site) and the Jarama (Valdocarros site and Maresa quarry) rivers have been Received in revised form studied in order to improve the existing chronological framework of the basin and to clarify the 21 August 2017 geological evolution of these fluvial systems and their relationship with human occupations. To do so, Accepted 8 September 2017 Electron Spin Resonance (ESR) dating was applied to four fossil teeth and nine optically bleached quartz Available online 22 September 2017 grain samples. Most of the obtained dates are consistent with the existing preliminary age estimates by biostratigraphy, luminescence (OSL and TL) or Amino Acid Racemization (AAR) dating. -
The (Re)Positioning of the Spanish Metropolitan System Within the European Urban System (1986-2006) Malcolm C. Burns
The (re)positioning of the Spanish metropolitan system within the European urban system (1986-2006) Malcolm C. Burns Tesi Doctoral dirigit per: Dr. Josep Roca Cladera Universitat Politècnica de Catalunya Programa de Doctorat d’Arquitectura en Gestió i Valoració Urbana Barcelona, juny de 2008 APPENDICES 411 The (re)positioning of the Spanish metropolitan system within the European urban system (1986-2006) 412 Appendix 1: Extract from the 1800 Account of Population of Great Britain 413 The (re)positioning of the Spanish metropolitan system within the European urban system (1986-2006) 414 Appendix 2: Extract from the 1910 Census of Population of the United States 421 The (re)positioning of the Spanish metropolitan system within the European urban system (1986-2006) 422 Appendix 3: Administrative composition of the Spanish Metropolitan Urban System (2001) 427 The (re)positioning of the Spanish metropolitan system within the European urban system (1986-2006) 428 1. Metropolitan area of Madrid (2001) Code INE Name of municipality Population LTL (2001) POR (2001) (2001) 5002 Adrada (La) 1960 550 702 5013 Arenal (El) 1059 200 303 5041 Burgohondo 1214 239 350 5054 Casavieja 1548 326 465 5055 Casillas 818 84 228 5057 Cebreros 3156 730 1084 5066 Cuevas del Valle 620 87 187 5075 Fresnedilla 101 38 33 5082 Gavilanes 706 141 215 5089 Guisando 635 70 171 5095 Higuera de las Dueña 326 44 89 5100 Hornillo (El) 391 41 94 5102 Hoyo de Pinares (El) 2345 333 791 5110 Lanzahíta 895 210 257 5115 Maello 636 149 206 5127 Mijares 916 144 262 5132 Mombeltrán 1123 -
Landscape-Based Fire Scenarios and Fire Types in the Ayllón Massif (Central Mountain Range, Spain), 19Th and 20Th Centuries1
Cuadernos de Investigación Geográfica 2020 Nº 46 (1) pp. 103-126 eISSN 1697-9540 Geographical Research Letters DOI: http://doi.org/10.18172/cig.3796 © Universidad de La Rioja LANDSCAPE-BASED FIRE SCENARIOS AND FIRE TYPES IN THE AYLLÓN MASSIF (CENTRAL MOUNTAIN RANGE, SPAIN), 19TH AND 20TH CENTURIES1 C.R. SEQUEIRA1*, C. MONTIEL-MOLINA1, F.C. REGO2 1Department of Geography, Faculty of Geography and History, Complutense University of Madrid, Spain. 2Centro de Ecologia Aplicada Prof. Baeta Neves, School of Agriculture, University of Lisbon, Portugal. ABSTRACT. Wildfires have been a major landscape disturbance factor throughout history in inland mountain areas of Spain. This paper aims to understand the interaction of fire regimes and landscape dynamics during the last two centuries within a socio-spatial context. The study area selected for this historical and spatial analysis is the Ayllón massif, in the Central Mountain Range. The theoretical background used to identify the driving forces of fire regime changes over the 19th and 20th centuries in this mountain area includes landscape-based fire scenarios and fire-type concepts. Both concepts have been addressed in recent studies from a spatial planning and fire management approach in an attempt to understand current fire landscapes and wildfire risk. However, this is the first time that these concepts have been applied to show that both spatial and temporal scales are crucial for an understanding of the current wildfire panorama, and that fire history related to landscape dynamics is fundamental in socio-spatial differences in fire regimes. Four variables (fire history, land use, population and settlement system, and forest management) were assessed to define historical landscape-based fire scenarios, and three fire feature variables (fire extent, fire cause, and spatial distribution pattern) were considered to define historical fire-types. -
Large Flake Acheulean in the Middle of Tagus Basin (Spain)
Quaternary International 411 (2016) 349e366 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Large flake Acheulean in the middle of Tagus basin (Spain): Middle stretch of the river Tagus valley and lower stretches of the rivers Jarama and Manzanares valleys * Susana Rubio-Jara a, Joaquín Panera b, , Juan Rodríguez-de-Tembleque c, Manuel Santonja b, Alfredo Perez-Gonz alez b a Instituto de Evolucion en Africa (I.D.E.A.), Museo de San Isidro, Plaza de San Andres 2, 28005 Madrid, Spain b Centro Nacional de Investigacion sobre la Evolucion Humana (C.E.N.I.E.H.), Paseo Sierra de Atapuerca, s/n, 09002 Burgos, Spain c Asociacion Nacional el Hombre y el Medio, Madrid, Spain article info abstract Article history: The highest concentration of Palaeolithic sites known in the Iberian Peninsula is located in the lower Available online 5 January 2016 stretches of the Manzanares and Jarama rivers. This area, together with a number of zones in the Tagus valley, constitutes one of the most important archives for the knowledge of the European Pleistocene. Keywords: The purpose of this paper is to establish the chronological frame and the technological strategies Pleistocene implemented in manufacturing lithic tools during the Acheulean techno-complex in the middle stretch Acheulean of the Tagus basin. Use of large flakes for making bifaces is common in the Acheulean assemblages from Palaeolithic this area, as well as in the rest of the Iberian Peninsula and the south of France. Tagus, Jarama and Manzanares rivers Iberian Peninsula The earliest Acheulean evidence has been dated to between MIS 15 and MIS 13. -
Nuestro Accionariado Informe De Incidencia
Nuestro accionariado Informe de incidencia Incidencia Reparto Reparto Accionista Accionista Emplazamiento accionarial accionarial DependenciaEnte Público técnica Canal de Isabel II 82,3996 % Fuenlabrada 0,6079 % FechaMadrid / / Responsable10,0000 del informe % Fuente El Saz de Jarama 0,0193 % Acebeda, La 0,0002 % Fuentidueña de Tajo 0,0064 % DescripciónAjalvir de la incidencia 0,0119 % Garganta de los Montes 0,0012 % Álamo, El 0,0247 % Gargantilla del Lozoya y Pinilla 0,0012 % Alcobendas 0,3363 % de Buitrago Getafe 0,5167 % Alcorcón 0,5142 % Griñón 0,0292 % Algete 0,0626 % Guadalix de la Sierra 0,0180 % Alpedrete 0,0402 % Humanes de Madrid 0,0567 % Ambite 0,0017 % Loeches 0,0222 % Anchuelo 0,0033 % Majadahonda 0,2122 % Aranjuez 0,1682 % Meco 0,0384 % IncidenciaArganda del no�ficada Rey 0,1623 % Mejorada del Campo 0,0697 % Arroyomolinos 0,0495 % Sí Molar, El 0,0234 % Belmonte de Tajo 0,0046 % Moraleja de Enmedio 0,0148 % BoadillaNo del Monte 0,1366 % Morata de Tajuña 0,0226 % Brea de Tajo 0,0017 % Móstoles 0,6294 % ActuaciónCadalso de llevada los Vidrios a cabo 0,0090 % Navalcarnero 0,0706 % Campo Real 0,0161 % Navas del Rey 0,0080 % Carabaña 0,0061 % Nuevo Baztán 0,0192 % Casarrubuelos 0,0096 % Paracuellos de Jarama 0,0496 % Cenicientos 0,0064 % Parla 0,3672 % ión en inscripción 34, NIF A86488087, Domicilio Social: C/ Santa Engracia, 125, 28003 Madrid. 125, 28003 Domicilio Engracia, 34, NIF A86488087, Social: C/ Santa ión en inscripción Ciempozuelos 0,0692 % Pelayos de la Presa 0,0078 % Cobeña 0,0188 % Perales de Tajuña 0,0088 % Colmenar del Arroyo 0,0044 % pción 1ª. Denominac Pinto 0,1360 % Colmenar de Oreja 0,0257 % Pozuelo de Alarcón 0,2530 % ReportajeColmenar fotográfico Viejo 0,1358 % Quijorna 0,0087 % ColladoSí Mediano 0,0199 % Rascafría 0,0061 % Collado Villalba 0,1830 % No Ribatejada 0,0020 % Corpa 0,0018 % Rivas-Vaciamadrid 0,2164 % Cubas de la Sagra 0,0145 % Robledo de Chavela 0,0118 % Chapinería 0,0065 % Rozas de Madrid, Las 0,2691 % drid al Tomo 29.733, Folio 86, Sección 8, Hoja M-534929. -
Madrid-Mondejar-Driebes Linea 322
Arganda del Rey (Hospital) Ambite - 322 - Ambite 322 Arganda del Rey (Hospital) ARGANDA DEL REY Ctra. Loeches ARGANDA DEL REY (Hospital delAv. sureste) del EjércitoZoco Plaza AyuntamientoMayor Baja Ctra. M-204 Ctra. M-204 Ctra. M-204 AMBITE (Hospital del Sureste) Ctra. Loeches Zoco Real Plaza AyuntamientoMayor Baja Ctra. M-204 Ctra. M-204 Ctra. M-204 AMBITE ARGANDA DEL REY ARGANDA DEL REY PERALES PERALES ARGANDA DEL REY DE TAJUÑA TIELMES CARABAÑA ORUSCO AMBITE ARGANDA DEL REY DE TAJUÑA TIELMES CARABAÑA ORUSCO AMBITE B3 C1 C2 B3 C1 C2 Tiempo estimado de recorrido 10 17 30 40 50 min 50 min 40 23 20 Tiempo estimado de recorrido HORARIOS DE PASO APROXIMADO (Vigente todo el año) HORARIOS DE PASO APROXIMADO 291014 291014 (Vigente todo el año) Arganda Perales de Tielmes Carabaña Orusco Ambite Arganda del Rey Perales de Tielmes Carabaña Orusco Ambite Tajuña del Rey Tajuña Lunes a viernes laborables Lunes a viernes laborables 6:00 6:15 6:20 6:25 6:30 6:35 14:40 14:30p 14:25 14:15 14:08 14:00 p 14:30n 14:45 14:50 14:55 15:00 15:05 22:10 22:00 21:55 21:45 21:38 21:30n 15:20 15:35 15:40 15:45 15:50 15:55 23:10 23:00 22:55 22:45 22:38 22:30 19:35 20:00 20:05 20:10 20:15 20:20 Sábados laborables Sábados laborables 10:40 10:30 10:25 10:15 10:08 10:00 11:15 11:30 11:35 11:40 11:45 11:50 13:10 13:00 12:55 12:45 12:38 12:30 15:30 15:45 15:50 15:55 16:00 16:05 23:25 23:15 23:10 23:00 22:53 22:45 Domingos y festivos sin servicio. -
Large Flake Acheulean in the Middle of Tagus Basin (Spain)
Quaternary International xxx (2015) 1e18 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Large flake Acheulean in the middle of Tagus basin (Spain): Middle stretch of the river Tagus valley and lower stretches of the rivers Jarama and Manzanares valleys * Susana Rubio-Jara a, Joaquín Panera b, , Juan Rodríguez-de-Tembleque c, Manuel Santonja b, Alfredo Perez-Gonz alez b a Instituto de Evolucion en Africa (I.D.E.A.), Museo de San Isidro, Plaza de San Andres 2, 28005 Madrid, Spain b Centro Nacional de Investigacion sobre la Evolucion Humana (C.E.N.I.E.H.), Paseo Sierra de Atapuerca, s/n, 09002 Burgos, Spain c Asociacion Nacional el Hombre y el Medio, Madrid, Spain article info abstract Article history: The highest concentration of Palaeolithic sites known in the Iberian Peninsula is located in the lower Available online xxx stretches of the Manzanares and Jarama rivers. This area, together with a number of zones in the Tagus valley, constitutes one of the most important archives for the knowledge of the European Pleistocene. Keywords: The purpose of this paper is to establish the chronological frame and the technological strategies Pleistocene implemented in manufacturing lithic tools during the Acheulean techno-complex in the middle stretch Acheulean of the Tagus basin. Use of large flakes for making bifaces is common in the Acheulean assemblages from Palaeolithic this area, as well as in the rest of the Iberian Peninsula and the south of France. Tagus, Jarama and Manzanares rivers Iberian Peninsula The earliest Acheulean evidence has been dated to between MIS 15 and MIS 13. -
Plano De Los Transportes De Alcalá De Henares
Calle Jorge Edw A vda. Víctimas del C . J Marséuan ards C T . Sergio error Pitol Plano de los transportes de Alcaláismo de Henares Calle Antonio Gamoneda Glorieta Calle Gonzalo Rojas Enrique II Calle 9 POLÍGONO CAMPORROSO VALDEAVERO 251 Calle F Juan Gelman I 17 Calle Raf M B C E F G C J K L N A 252 DAGANZO CAMARMA DE ESTERUELAS 255 H ar Mutis Calle Alf alle 250 MECO D rancisco Umbr A lfo 254 FUENTE EL SAZ nso 232 CENTRO PENITENCIARIO ALCALÁ- MECO X Calle Álv ael I A venida Calle A onso Centro Salud ve n Sanc Calle José Jiménez Lozano i ho d “Miguel de al a VII II or” y Sánchez F Cervantes” Gusta 10 e-Inclan 1 del Valll v Miguel Angel Blanco “El Ma o V 9 í C EL DESCUBRIMIENTO a c VI a Calle í vda. t 1 r A im lle o a t M er a n s Biblioteca n Pza. Conde losio á e m i V as Calle F e de Barcelona Nacional 3 m enezuela P onso A i nando III C r Adolf a l sé f Calle de Hondur Jo Calle l o b Calle er l as María e n u nando I s n c 9 o Becquer er o s ó e Glorieta m X D Calle de Hondur Calle Rosalía de Castro Juan II C a r S . ancisco Umbr Calle F a I R Calle Sancho Garcés ll a C. a e n R venida Punto Com e Carretera de Meco A d Leopoldo Alas Clarín C edro I c in v h a a A d l Calle Sancho García o 0 l a Calle José Pla y e e U Calle F 0 . -
Precipitations and Floods in the Jarama- Tajo Basin (Central Spain) in the Late 16Th Century
Boletín de la AsociaciónPrecipitations de Geógrafos and floods Españoles in the Jarama-Tajo N.º 60 - 2012, basin págs. (central 441-443 Spain) in the late 16th century I.S.S.N.: 0212-9426 PRECIPITATIONS AND FLOODS IN THE JARAMA- TAJO BASIN (CENTRAL SPAIN) IN THE LATE 16TH CENTURY Teresa Bullón Mata Departamento de Geografía. Universidad Autónoma de Madrid [email protected] The study site is located in the centre of the Iberian Peninsula. It forms part of the basin of the river Jarama, a tributary of the river Tagus. This river drains the territory of Madrid and, at the southern border of the area, it joins with the Tagus. Some sections of the rivers studied possess a snow regime, as their heads are situated in mountain areas, and other sections present torrential drainage, with a high erosive capacity, as they start on flatlands and moors lying upon unconsolidated sediments, situated to the south of the mountains of the Central System. The current regulation system, with numerous reservoirs upriver, has modified the natural circulation of the waters. The numerous interventions and extractions of sand and gravel in the channels and on the riverbanks have eliminated many of the sediment records that had accumulated on the floodplain. The rivers present great mobility within the floodplains they have shaped. The land uses and other human actions developed in these riparian zones since at least medieval times have been adapted to the changing fluvial dynamics, and many of the events related thereto are reflected in written and graphic documents: «And the above mentioned Jarama river is therefore variable and tends to move away from its mother and flow elsewhere» (16th August, 1579.