Across the Pyrenees
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Libro De RUTA 2017
Libro de RUTA 2017 Gran Trail Aneto-Posets.105 km / 6 760 m+ 40.7 km of the course at an altitude above 2000 m / 10.1 km of paved roads 20.8 km of tracks / 57.9 km of footpaths / 16.2 km off-trail The Gran Trail Aneto-Posets covers all manner of terrain, from tracks and footpaths to snowfields and blockfields that surround the highest peaks in the Pyrenees: Aneto (3404 m) and Posets (3375 m). It is a spectacular race which takes place under conditions of semi self-sufficiency, joining these two mountainous massifs together to comprise a boundless route. The Gran Trail starts off from the village of Benasque with a lap around Aneto heading towards La Renclusa refuge to then head off up the Barrancs valley, climb to the Salenques mountain pass (2797 m) and from there towards the Vallibierna valley. After passing through Benasque once again, the climb up to Cerler begins, from where the route drops down to the picturesque village of Anciles and on to Eriste before starting the lap around the Posets massif. This section includes the highest point of the race, Forqueta mountain pass at 2900 m. From this point, the course takes runners down to the Biadós refuge following the GR11 leading to the Estós refuge before returning to Benasque to end the race. Vuelta al Aneto. 55 km / 3 630 m+ 27.5 km of the course at an altitude above 2000 m / 6.1 km of paved roads 8.8 km of tracks / 24.2 km of footpaths / 15.9 km off-trail The Vuelta al Aneto takes place over all manner of terrain, from tracks and footpaths to snowfields and blockfields surrounding the Maladeta massif, crowning off at the peak of Aneto (3404 m). -
High Route of Maladetas (Pyrenees)
CICMA: 2608 +34 629 379 894 [email protected] SKI TOURING HIGH ROUTE OF MALADETAS (PYRENEES) CICMA: 2608 +34 629 379 894 [email protected] CICMA: 2608 +34 629 379 894 [email protected] The Massif of Maladetas with the Aneto Peak (3.404 m) The opening of the mountain hut Cap de Llauset, in a strategic is an exceptional terrain for ski touring. In addition, its place of these mountains, gives us a multitude of options to make a circular tour around the Maladetas and to visit other mountains height and orientation allows to extend the season until with many options for skiing. May and even June, having to postpone summer plans for later. During three days and two nights at the Cap de Llauset mountain hut we will make a high route around the Maladetas and also ascend to summits such as the Vallibierna Peak (3.058 m). CICMA: 2608 +34 629 379 894 [email protected] CICMA: 2608 +34 629 379 894 [email protected] THE DESTINATION The Posets-Maladeta Natural Park is located to the north of the region of Ribagorza in the province of Lérida and northeast of Sobrarbe in the province of Huesca It includes two of the highest massifs of the Pyrenees: the Aneto (3,404 m) with other summits such as Pico Maladeta (3,308 m), and the Massif del Posets (3,375 m) with other mythical peaks such as Perdiguero (3,221 m). In the Posets-Maladeta Natural Park we can enjoy the privilege of observing some of the glaciers that still remain in the Pyrenees, such as the legendary Aneto glacier in the Maladeta massif or the Llardana glacier in the Posets massif. -
Forest Fire Prevention Plans in National Parks: Ordesa Nacional Park and Monte Perdido1
Proceedings of the Second International Symposium on Fire Economics, Planning, and Policy: A Global View Forest Fire Prevention Plans in National Parks: Ordesa Nacional Park and Monte Perdido1 Basilio Rada,2 Luis Marquina3 Summary Protected natural spaces contribute to the well being of society in various ways such as maintaining biological diversity and quality of the landscape, regulation of water sources and nutrient cycles, production of soil, protection against natural catastrophes and the provision of recreation areas, education, science and culture, aspects which attain maximum relevance in the lands under the protection of the National Park. The singular nature and the high degree of protection to a large extent limit management, since the principles of conservation and natural processes prevail in these areas. Nevertheless the inevitable responsibility to ensure now and in future, the ecological economic and social functions of these spaces goes on to assume a management model on the lines of compliance with the Pan European Criteria for Sustainable Forest Management. In 2000 management of the Ordesa and Monte Perdido Park , in the Spanish Pyrenees which was declared a natural park in 1918, took the initiative to devise a Plan for the Prevention of Forest Fires in the park and its surroundings which may be a reference for the other parks comprising the network of Spanish National Parks. The Plan analyses the effectiveness of current protection resources, supported by cartography which aids decision making, fuel maps, fire risk, visibility, territorial isochrones and areas which at the same time plan the necessary measures to guarantee the protection of this space, which in many areas is inaccessible due to the steep landscape. -
Map of La Rioja Haro Wine Festival
TRAVEL AROUND SPAIN SPAIN Contents Introduction.................................................................6 General information......................................................7 Transports.................................................................10 Accommodation..........................................................13 Food.........................................................................15 Culture......................................................................16 Region by region and places to visit..............................18 Andalusia........................................................19 Aragon............................................................22 Asturias..........................................................25 Balearic Islands...............................................28 Basque Country................................................31 Canary Islands.................................................34 Cantabria........................................................37 Castille-La Mancha...........................................40 Castille and León.............................................43 Catalonia........................................................46 Ceuta.............................................................49 Extremadura....................................................52 Galicia............................................................55 La Rioja..........................................................58 Madrid............................................................61 -
3. Cueva De Chaves .87 3.1
NICCOLÒ MAZZUCCO The Human Occupation of the Southern Central Pyrenees in the Sixth-Third Millennia cal BC: a Traceological Analysis of Flaked Stone Assemblages TESIS DOCTORAL DEPARTAMENT DE PREHISTÒRIA FACULTAT DE LETRES L Director: Dr. Ignacio Clemente-Conte Co-Director: Dr. Juan Francisco Gibaja Bao Tutor: Dra. Maria Saña Seguí Universitat Autònoma de Barcelona 2014 This work has been founded by the JAE-Predoc scholarship program (year 2010-2014) of the Spanish National Research Council (CSIC), realized at the Milà i Fontanals Institution of Barcelona (IMF). This research has been carried out as part of the research group “Archaeology of the Social Dynamics” (Grup d'Arqueologia de les dinàmiques socials) of the Department of Archaeology and Anthropology of the IMF. Moreover, the author is also member of the Consolidated Research Group by the Government of Catalonia “Archaeology of the social resources and territory management” (Arqueologia de la gestió dels recursos socials i territori - AGREST 2014-2016 - UAB-CSIC) and of the research group “High-mountain Archaeology” (Grup d'Arqueologia d'Alta Muntanya - GAAM). 2 Todos los trabajos de arqueología, de una forma u otra, se podrían considerar trabajos de equipo. Esta tesis es el resultado del esfuerzo y de la participación de muchas personas que han ido aconsejándome y ayudándome a lo largo de su desarrollo. Antes de todo, quiero dar las gracias a mis directores, Ignacio Clemente Conte y Juan Francisco Gibaja Bao, por la confianza recibida y, sobre todo, por haberme dado la posibilidad de vivir esta experiencia. Asimismo, quiero extender mis agradecimientos a todos los compañeros del Departamento de Arqueología y Antropología, así como a todo el personal de la Milà i Fontanals. -
Cirques Have Growth Spurts During Deglacial and Interglacial Periods: Evidence from 10Be and 26Al Nuclide Inventories in the Central and Eastern Pyrenees Y
Cirques have growth spurts during deglacial and interglacial periods: Evidence from 10Be and 26Al nuclide inventories in the central and eastern Pyrenees Y. Crest, M Delmas, Regis Braucher, Y. Gunnell, M Calvet, A.S.T.E.R. Team To cite this version: Y. Crest, M Delmas, Regis Braucher, Y. Gunnell, M Calvet, et al.. Cirques have growth spurts during deglacial and interglacial periods: Evidence from 10Be and 26Al nuclide inventories in the central and eastern Pyrenees. Geomorphology, Elsevier, 2017, 278, pp.60 - 77. 10.1016/j.geomorph.2016.10.035. hal-01420871 HAL Id: hal-01420871 https://hal-amu.archives-ouvertes.fr/hal-01420871 Submitted on 21 Dec 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Geomorphology 278 (2017) 60–77 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Cirques have growth spurts during deglacial and interglacial periods: Evidence from 10Be and 26Al nuclide inventories in the central and eastern Pyrenees Y. Crest a,⁎,M.Delmasa,R.Braucherb, Y. Gunnell c,M.Calveta, ASTER Team b,1: a Univ Perpignan Via-Domitia, UMR 7194 CNRS Histoire Naturelle de l'Homme Préhistorique, 66860 Perpignan Cedex, France b Aix-Marseille Université, CNRS–IRD–Collège de France, UMR 34 CEREGE, Technopôle de l'Environnement Arbois–Méditerranée, BP80, 13545 Aix-en-Provence, France c Univ Lyon Lumière, Department of Geography, UMR 5600 CNRS Environnement Ville Société, 5 avenue Pierre Mendès-France, F-69676 Bron, France article info abstract Article history: Cirques are emblematic landforms of alpine landscapes. -
RUTA GUIADA Aneto Y Posets: Gigantes Del Pirineo (4 Días)
1 RUTA GUIADA Aneto y Posets: gigantes del Pirineo (4 días) Alcanzamos las dos cimas más elevadas de los Pirineos en el Parque Natural Posets-Maladeta. ¡Alta montaña en estado puro! Benasque, La Ribagorza, Huesca RUTES PIRINEUS TURISME ACTIU DE MUNTANYA SL www.rutespirineus.cat | www.rutaspirineos.org | www.pyreneestrails.com RUTA GUIADA Aneto y Posets: gigantes del Pirineo (4 días) ¿POR QUÉ HACER ESTA RUTA? Este programa de 4 días nos permitirá ascender las dos montañas más altas de los Pirineos: el pico Aneto (3.404m) y el pico Posets (3.375m), ambas situadas en la cabecera del valle de Benasque, donde se concentra el mayor número de tresmiles de la cordillera. Durante la ruta tendremos la oportunidad de adentrarnos en el Parque Natural Posets-Maladeta, un precioso espacio protegido que destaca por su gran riqueza natural y por una geología excepcional. Los dos primeros días de ruta los dedicaremos a la ascensión al pico Posets, la segunda cima más alta del Pirineo. La ascensión a esta gran montaña nos permitirá descubrir el valle de Eriste, el valle de Llardaneta, la Canal Fonda, el espectacular Diente de Llardana y, como colofón final, la espectacular arista que nos llevará hasta la cima. Desde la cumbre del Posets podremos gozar de unas grandes panorámicas de todo el Pirineo al ser una de las montañas más aislada de entre las grandes cumbres pirenaicas. Después de pasar una segunda noche en un cálido hostal en Benasque, el tercer día subiremos hasta el refugio de la Renclusa, que está situado en un paraje excepcional justo a los pies de la Maladeta. -
Flora Y Vegetación Del Parque Nacional De Ordesa Y Monte Perdido (Sobrarbe, Pirineo Central Aragonés)
Universidad de Barcelona Facultad de Biología Departamento de Biología Vegetal Flora y vegetación del Parque Nacional de Ordesa y Monte Perdido (Sobrarbe, Pirineo central aragonés) Bases científicas para su gestión sostenible Memoria presentada por José Luis Benito Alonso, licenciado en Biología, para optar al grado de Doctor en Biología Programa de doctorado “Vegetales y fitocenosis”, curso 1994/96 Abril de 2005 Flora y vegetación del Parque Nacional de Ordesa y Monte Perdido 3. Vegetación CAPÍTULO 3. VEGETACIÓN ......................................................................................... 313 1. Introducción................................................................................................................................... 313 2. Catálogo de comunidades vegetales .......................................................................................... 314 2.1. Vegetación de turberas y pastos higroturbosos........................................................................ 314 CL. SCHEUCHZERIO PALUSTRIS-CARICETEA NIGRAE Tüxen 1937 .................................... 314 Or. Caricetalia davallianae Br.-Bl. 1949................................................................................. 314 Al. Caricion davallianae Klika 1934.................................................................................... 314 Al. Caricion maritimae Br.-Bl. in Volk 1940 nom . mut . prop ............................................... 315 2.2. Juncales, herbazales húmedos y prados de siega .................................................................. -
Geological Sciences Alumni Newsletter November 2016 1
GEOLOGICAL SCIENCES ALUMNI NEWSLETTER NOVEMBER 2016 1 ALUMNI NEWSLETTER 2016 Roster From Our Department Chair 2 Assistant Professors Noel Bartlow (Stanford University 2013) Faculty Geophysics and tectonics News 4 John W. Huntley (Virginia Tech, 2007) Research Grants 5 Paleontology and Paleoecology James D. Schiffbauer (Virginia Tech, 2009) Visiting scientists/staff recognition 13 Paleontology and geochemistry Visiting Speakers 14 Associate Professors Martin S. Appold (Johns Hopkins University, 1998) Conference 15 Hydrogeology Francisco G. Gomez (Cornell University, 1999) Field Camp 16 Paleoseismology and neotectonics Research Professors Selly 18 Cheryl A. Kelley (University of North Carolina, 1993) Undergraduate Program 19 Aquatic geochemistry Mian Liu (University of Arizona, 1989) Study Abroad Program 20 Geophysics Kenneth G. MacLeod (University of Washington, 1992) Photo Gallery Paleontology and biogeochemistry Field Trips 23 Field Camp 24 Peter I. Nabelek (SUNY, Stony Brook, 1983) Outreach 25 Trace-element geochemistry Alumni Reunion 26 Eric A. Sandvol (New Mexico State University, 1995) Undergraduate Presentations 27 Seismotectonics Kevin L. Shelton (Yale University, 1982) Students Economic geology La Reunion 28 Alan G. Whittington (Open University, 1997) Soldati Award 29 Crustal petrology and volcanology Geology Club 30 Student Chapter of AEG-AAPG 31 Director of Field Studies MU Geology Graduate Society 32 Miriam Barquero-Molina (University of Texas, 2009) Undergraduate 33 Awards 34 Field methods Graduate 35 Publications 37 Professors Emeriti Presentation 38 Robert L. Bauer (University of Minnesota, 1982) Precambrian geology Development Activities Raymond L. Ethington (University of Iowa, 1958) Activities 40 Conodont biostratigraphy Contributions 41 Thomas J. Freeman (University of Texas, 1962) Endowmenta 43 Carbonate petrology Faculty Awards 45 Glen R. Himmelberg (University of Minnesota, 1965) Board Members 46 From Our Board Chair 47 Chemical petrology Michael B. -
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Difficult Hiking Route Aneto Peak
Difficult Hiking route Aneto Peak Aneto, the highest peak in the Pyrenees at 3.404 meters, is situated in the Natural Park of Posets-Maladeta. It is the source of many legends and a great challenge to climbers and trekkers. A worthy challenge but also dangerous. Although it isn’t an excessively difficult climb, it is a “three thousander” and there is a glacier to cross and other minor difficulties which people tend to forget and in fact many climb the mountain who are not really well prepared to do so. ROUTE The ideal starting point for the ascent of Aneto is the refuge of the Renclusa. From here there is a path going SE. It’s difficult to lose your way due to the piles of marker stones and the amount of climbers on the path. The zig zagging path rises fairly gently through increasingly sparse vegetation. In 1 hour and 40 minutes the Aneto glacier can be seen from the Lower Portillon at 2.818 meters. From here you go down to the glacier via a well worn path. After about three and a half hours the path reaches the Coronas Pass and only the final stretch of glacier, with its enormous cracks, remains. Here you will find the dangerous Mahoma’s Crossing where you will have to climb using the previously installed hooks you will find there. From here you have only to continue along the sharp ridge to reach the highest point in the Pyrenees. DETAILS • Location: Posets - Maladeta Natural Park • Ascent time: 6 hours • Descent time: 5 hours • Recommended dates: summer • Difficulty: The scree slopes are dangerous as is the stretch over the glacier, on the windy, narrow paths of the crest and a piolet, rope and crampons should be used • Level: for experienced and well equipped mountaineers. -
The Little Ice Age in Iberian Mountains T ⁎ M
Earth-Science Reviews 177 (2018) 175–208 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev The Little Ice Age in Iberian mountains T ⁎ M. Olivaa, , J. Ruiz-Fernándezb, M. Barriendosc, G. Benitod, J.M. Cuadrate, F. Domínguez-Castrof, J.M. García-Ruizf, S. Giraltg, A. Gómez-Ortiza, A. Hernándezh, O. López-Costasi,j, J.I. López-Morenof, J.A. López-Sáezk, A. Martínez-Cortizasi, A. Morenof, M. Prohoml, M.A. Saze, E. Serranom, E. Tejedore, R. Trigoh, B. Valero-Garcésf, S.M. Vicente-Serranof a Department of Geography, University of Barcelona, Spain b Department of Geography, University of Oviedo, Spain c Department of Modern History, University of Barcelona, Spain d Museo Nacional de Ciencias Naturales (MNCN-CSIC), Madrid, Spain e Department of Geography and Spatial Planning, University of Zaragoza, Spain f Instituto Pirenaico de Ecología (IPE-CSIC), Campus de Aula Dei, Zaragoza, Spain g Institute of Earth Sciences, Jaume Almera (ICTJA-CSIC), Barcelona, Spain h Instituto Dom Luiz (IDL), Faculdade de Ciências, Universidade de Lisboa, Lisbon, Portugal i Group Earth System Science, Universidade de Santiago de Compostela, Spain j Laboratory of Physical & Forensic Anthropology, Universidad de Granada, Spain k Institute of History – CSIC, Spain l Meteorological Service of Catalonia, Spain m Department of Geography, University of Valladolid, Spain ARTICLE INFO ABSTRACT Keywords: The Little Ice Age (LIA) is known as one of the coldest stages of the Holocene. Most records from the Northern Little Ice Age Hemisphere show evidence of significantly colder conditions during the LIA, which in some cases had substantial Iberian Peninsula socio-economic consequences.