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Planos De Información: V. Oferta De Transporte
Santa Cruz Tegueste de Tenerife Tacoronte La Laguna El Sauzal La Matanza de Acentejo El Rosario La Victoria Santa Puerto de de Acentejo Ursula la Cruz San Juan de la Rambla Candelaria Los Los Realejos Arafo Silos Buenavista del Norte Icod de El Tanque los Vinos Garachico La Guancha Santiago del Teide Guimar La Orotava Fasnia Guia de Isora Arico Vilaflor Adeje Granadilla de Abona San Miguel Arona Líneas de Tranvía Paradas de Guaguas y Tranvía Paradas de Guaguas y Tranvía Líneas de Transporte Público Líneas de Guagua TÍTULO: APÉNDICE: Escalas: Plano: Fecha: Nº Plano: MAYO 2012 1 PLAN TERRITORIAL ESPECIAL DE ORDENACIÓN PLANOS DE INFORMACIÓN: 1:260,000 LÍNEAS Y PARADAS DE Revisión: Hoja: DEL TRANSPORTE DE TENERIFE 0 2,500 5,000 TRANSPORTE PÚBLICO V. OFERTA DE TRANSPORTE PÚBLICO Metros 01 Santa Cruz Tegueste de Tenerife La Laguna Tacoronte El Sauzal La Matanza de Acentejo El Rosario La Victoria Santa Puerto de de Acentejo Ursula la Cruz San Juan de la Rambla Candelaria Los Los Realejos Arafo Silos Buenavista del Norte Icod de El Tanque los Vinos Garachico La Guancha Santiago Guimar del Teide La Orotava Fasnia Guia de Isora Arico Vilaflor Adeje Granadilla de Abona San Miguel [Expediciones/día] Arona 0 - 100 101 - 250 251 - 500 501 - 1000 1001 - 1500 TÍTULO: APÉNDICE: Escalas: Plano: Fecha: Nº Plano: PLAN TERRITORIAL ESPECIAL DE ORDENACIÓN MAYO 4 PLANOS DE INFORMACIÓN: 1:250,000 2012 DEL TRANSPORTE DE TENERIFE Revisión: Hoja: 0 2,500 5,000 EXPEDICIONES POR TRAMO DOCUMENTO DE APROBACIÓN INICIAL V. OFERTA DE TRANSPORTE PÚBLICO Metros 01 Santa -
Documento Informativo
CA LI ÚB Plan Rector de Uso y Gestión P Plan Especial Prot. Paisajística N IÓ Normas de Conservación AC Plan Especial de Protección Paisajística M R Plan Director FO IN Color para parques naturales [ PANTONE 116 CV ] Color gris de fondo [Modelo RGB: R - 229,G - 229, B - 229] GOBIERNO DE CANARIAS SS OO ÓN CONSEJERÍA DE MEDIO AMBIENTE Y ICC CI ORDENACIÓN TERRITORIAL TTI A VICECONSEJERÍA DE ÁÁ M A ORDENACIÓN TERRITORIAL M R IC EEM FO L DIRECCIÓN GENERAL DE ORDENACIÓN TT IN ÚB DEL TERRITORIO P JJOO Plan Director BBAA RRAA NN TT ReservaIIÓÓ Natural Especial CCdel Chinyero AA CCEE BB AANN OO AAVV PPRR AA Parque Rural Parque Natural Reserva Natural Integral Reserva Natural Especial IVAIVA Sendero ITIT Paisaje Protegido FFININ Monumento Natural DEE Sitio de Interés Científico DocDumento Informativo Reserva Natural Especial del Chinyero Plan Director Contenidos Descripción de la Reserva Natural Especial del Chinyero....................... 2 Introducción ...................................................................................................2 Localización ........................................................................................................2 Medio físico.....................................................................................................3 Clima .................................................................................................................3 Geología y Geomorfología....................................................................................8 Morfología ........................................................................................................12 -
Världsarvslistan
http://wimnell.com/omr91b.pdf • Tipasa • Kasbah of Algiers Världsarvslistan Andorra http://whc.unesco.org/en/list/ • Madriu-Perafita-Claror Valley Argentina The World Heritage List includes 936 properties forming part of the • Los Glaciares # cultural and natural heritage which the World Heritage Committee • Jesuit Missions of the Guaranis: San Ignacio Mini, Santa Ana, considers as having outstanding universal value. Nuestra Señora de Loreto and Santa Maria Mayor (Argentina), Ruins of Sao Miguel das Missoes (Brazil) * These include 725 cultural , 183 natural and 28 mixed properties in • Iguazu National Park 153 States Parties. As of November 2011, 188 States Parties have • Cueva de las Manos, Río Pinturas ratified the World Heritage Convention. • Península Valdés • Ischigualasto / Talampaya Natural Parks Afghanistan • Jesuit Block and Estancias of Córdoba • Quebrada de Humahuaca • Minaret and Archaeological Remains of Jam Armenia • Cultural Landscape and Archaeological Remains of the Bamiyan Valley • Monasteries of Haghpat and Sanahin Albania • Cathedral and Churches of Echmiatsin and the Archaeological Site of Zvartnots • Butrint • Monastery of Geghard and the Upper Azat Valley • Historic Centres of Berat and Gjirokastra Australia Algeria • Great Barrier Reef • Al Qal'a of Beni Hammad • Kakadu National Park • Djémila • Willandra Lakes Region • M'Zab Valley • Lord Howe Island Group • Tassili n'Ajjer # • Tasmanian Wilderness • Timgad • Gondwana Rainforests of Australia 1 • Uluru-Kata Tjuta National Park 2 • Qal’at al-Bahrain – Ancient Harbour -
Conductive Structures Around Las Cañadas Caldera, Tenerife (Canary Islands, Spain): a Structural Control
Geologica Acta, Vol.8, Nº 1, March 2010, 67-82 DOI: 10.1344/105.000001516 Available online at www.geologica-acta.com Conductive structures around Las Cañadas caldera, Tenerife (Canary Islands, Spain): A structural control * N. COPPO P.A. SCHNEGG P. FALCO and R. COSTA Geomagnetism group, Department of Geology, University of Neuchâtel CP 158, 2009 Neuchâtel, Switzerland *corresponding author E-mail: [email protected] ABSTRACT External eastern areas of the Las Cañadas caldera (LCC) of Tenerife (Canary Islands, Spain) have been investigated using the audiomagnetotelluric (AMT) method with the aim to characterize the physical rock properties at shallow depth and the thickness of a first resistive layer. Using the results of 50 AMT tensors carried out in the period range of 0.001 s to 0.3 s, this study provides six unpublished AMT profiles distributed in the upper Orotava valley and data from the Pedro Gil caldera (Dorsal Ridge). Showing obvious 1-D behaviour, soundings have been processed through 1-D modeling and gathered to form profiles. Underlying a resistive cover (150-2000 Ωm), a conductive layer at shallow depth (18-140 Ωm, 250-1100 m b.g.l.) which is characterized by a “wavy-like” structure, often parallel to the topography, appears in all profiles. This paper points out the ubiquitous existence in Tenerife of such a conductive layer, which is the consequence of two different processes: a) according to geological data, the enhanced conductivity of the flanks is interpreted as a plastic breccia within a clayish matrix generated during huge lateral collapse; and b) along main tectonic structures and inside calderas, this layer is formed by hydrothermal alteration processes. -
Mount Teide in the Work of Olivia Stone: Landscape As a Tourism Resource
Cuadernos de Turismo, nº 39, (2017); pp. 611-614 Universidad de Murcia ISSN: 1139-7861 eISSN: 1989-4635 MOUNT TEIDE IN THE WORK OF OLIVIA STONE: LANDSCAPE AS A TOURISM RESOURCE Esther Beltrán Yanes Universidad de La Laguna (Tenerife) [email protected] 1. INTRODUCTION The landscape and nature of the Canary Islands stand out on the world map for their diversity and originality. This fragmented insular space combines a variety of geographical factors, namely volcanism and its subtropical location, resulting in many diverse landscapes all within a small area (7,493 km2). Romanticism, a cultural movement that inspired the beginning of leisure travel to the Canary Islands, took traveling beyond the strictly European borders and brought it to more exotic and distant destinations, which, in the late nineteenth century, began to place this archipelago northwest of the African continent in the limelight. The objective of the paper presented is twofold. On the one hand, our objective is to explore the tourist interest in the landscape of the Canary Islands, and especially by the predominantly natural physiognomy, among Europeans, particularly among the British in the late nineteenth century. And secondly, once this first objective has been fulfilled, we will demonstrate that one of the main centres of attraction in this sense was the exceptional scenery associated with the stunning Teide stratovolcano. To accomplish this dual objective, it was first essential to make a brief analysis of the European culture of British high society that inspired leisure travel and spending free time in nature and the countryside during that era, and then analyse the stories of travellers who were drawn to visit the islands due to the landscape and who played an important role in the tourism industry taking off during those years. -
Geotechnical Analysis of Large Volcanic Landslides: the La Orotava Events on Tenerife, Canary Islands
Geotechnical analysis of large volcanic landslides: The La Orotava events on Tenerife, Canary Islands. A dissertation submitted to the TECHNICAL UNIVERSITY OF CATALONIA for the degree of Doctor of Sciences (Geologic) presented by Marcel Hürlimann Supervisors: Dr. A. Ledesma Dep. of Geotechnical Engineering and Geosciences, Technical University of Catalonia Dr. J. Martí Institute of Earth Sciences 'Jaume Almera', Spanish Research Council Barcelona October, 1999 Geotechnical analysis of large volcanic landslides: The La Orotava events on Tenerife, Canary Islands. Marcel Hürlimann "Getöse, Krachen und Geprassel erfüllt wie tief brüllender Donner die Luft – erschüttert jedes lebende Ohr und Herz, und tönt im Wiederhall von tausend Bergesklüften noch grässlicher." Schuttbuch des Goldauer Bergsturzes (Dr. Karl Zay, 1807) ACKNOWLEDGEMENTS This study was supervised by Alberto Ledesma from the Department of Geotechnical Engineering and Geosciences, School of Civil Engineering, 'Universitat Politècnica de Catalunya' (UPC) and Joan Martí from the Institute of Earth Sciences 'Jaume Almera', Spanish Research Council (CSIC). I owe many thanks to them and my Ph.D. would not have been the same without their continuous support and encouragement. To combine the ideas of an engineer and a volcanologist was not always easy, but the inter-disciplinary structure certainly improved the results of this work. I am very grateful to many people at the Department of Geotechnical Engineering and Geosciences (UPC) and the Institute of Earth Sciences 'Jaume Almera' (CSIC) who helped me in various ways. Special thanks to Antonio Lloret, Tomás Pérez and José Álvarez who introduced me into the design and handling of the apparatuses of the geotechnical laboratory and to Ignasi Queralt who carried out the X-ray analyses. -
Quarterly Magazine for Airlines, Airports, Tour-Operators and Tourism Authorities Issue 18
AenaNews Quarterly magazine for airlines, airports, tour-operators and tourism authorities Issue 18 Index Canary Islands Airports Latest News on Spanish Airports Page Q1 2018 Aena’s financial and traffic Trolley Fast Lane available at Palma Aena will attend the 142 IATA Slot results de Mallorca Airport Conference in Vancouver from 19-21 Total consolidated revenue increased to 841.8 Palma de Mallorca Airport has created two June and World Routes in Guangzhou million euros (+6.0% compared to Q1 2017), “Trolley Fast Lanes” in modules A and D that from 15-18 September of which commercial revenue1 accounted are intended to optimice the luggage transfer Our Airline Customer Relations and Airport for 26.4% (26.0% in Q1 2017). Commercial time between the aircraft and the baggage Marketing Team hope to see you in Vancouver revenue grew +7.5% to 221.9 million euros. claim area, especially during the peak season, and in our stand number HNS407 in when around 70,000 luggages are handled EBITDA for the period stood at 364.2 million Guangzhou. per day, and thus improve the passenger euros, which represents a growth of +13.8% experience at the airport with a fast delivery compared to Q1 2017. of their luggage and reduce delivery times for Consolidated attributable net profit came to airlines and handling agents. 111.1 million euros (+37.4% compared to Q1 2017) reflecting the positive evolution of the business. Regarding traffic results Aena’s airports (YTD April 2018) reached 71.5 million passengers (+7.6% increase over YTD April 2017). A.S. -
3. Canary Islands and the Laurel Forest 13
The Laurel Forest An Example for Biodiversity Hotspots threatened by Human Impact and Global Change Dissertation 2014 Dissertation submitted to the Combined Faculties for the Natural Sciences and for Mathematics of the Ruperto–Carola–University of Heidelberg, Germany for the degree of Doctor of Natural Sciences presented by Dipl. biol. Anja Betzin born in Kassel, Hessen, Germany Oral examination date: 2 The Laurel Forest An Example for Biodiversity Hotspots threatened by Human Impact and Global Change Referees: Prof. Dr. Marcus A. Koch Prof. Dr. Claudia Erbar 3 Eidesstattliche Erklärung Hiermit erkläre ich, dass ich die vorgelegte Dissertation selbst verfasst und mich dabei keiner anderen als der von mir ausdrücklich bezeichneten Quellen und Hilfen bedient habe. Außerdem erkläre ich hiermit, dass ich an keiner anderen Stelle ein Prüfungsverfahren beantragt bzw. die Dissertation in dieser oder anderer Form bereits anderweitig als Prü- fungsarbeit verwendet oder einer anderen Fakultät als Dissertation vorgelegt habe. Heidelberg, den 23.01.2014 .............................................. Anja Betzin 4 Contents I. Summary 9 1. Abstract 10 2. Zusammenfassung 11 II. Introduction 12 3. Canary Islands and the Laurel Forest 13 4. Aims of this Study 20 5. Model Species: Laurus novocanariensis and Ixanthus viscosus 21 5.1. Laurus ...................................... 21 5.2. Ixanthus ..................................... 23 III. Material and Methods 24 6. Sampling 25 7. Laboratory Procedure 27 7.1. DNA Extraction . 27 7.2. AFLP Procedure . 27 7.3. Scoring . 29 7.4. High Resolution Melting . 30 8. Data Analysis 32 8.1. AFLP and HRM Data Analysis . 32 8.2. Hotspots — Diversity in Geographic Space . 34 8.3. Ecology — Ecological and Bioclimatic Analysis . -
Unique Geological Values of Mt. Teide As the Basis of Its Inclusion on The
Seminario_10_2013_d 10/6/13 17:11 Página 36 Unique geological values of Mt. Teide as the basis of its inclusion on the World Heritage List / Juan Carlos Carracedo Universidad de Las Palmas de Gran Canaria Abstract UNESCO created in 1972 the World Heritage List to “preserve the world’s superb natural and sce- nic areas and historic sites for the present and future generations of citizens of the entire world”. Nominated sites must be of ‘outstanding universal value’ and meet stringent selection criteria. Teide National Park (TNP) and the already nominated (1987) Hawaiian Volcanoes National Park (HVNP) correspond to the Ocean Island Basalts (OIB). The main geological elements of TNP inclu- de Las Cañadas Caldera, one of the most spectacular, best exposed and accessible volcanic cal- deras on Earth, two active rifts, and two large felsic stratovolcanoes, Teide and Pico Viejo, rising 3718 m above sea level and around 7500 m above the ocean floor, together forming the third hig- hest volcanic structure in the world after the Mauna Loa and Mauna Kea volcanoes on the island of Hawaii. A different geodynamic setting, causing lower fusion and subsidence rates in Tenerife, lead to longer island life and favoured evolution of magmas and the production of large volumes of differentiated volcanics in Tenerife, scant or absent in Hawaii. This fundamental difference provi- ded a main argument for the inscription of TNP in the World Heritage List because both National Parks complement each other to represent the entire range of products, features and landscapes of oceanic islands. Teide National Park was inscribed in the World Heritage List in 2007 for its natu- ral beauty and its “global importance in providing diverse evidence of the geological processes that underpin the evolution of oceanic islands, these values complementing those of existing volcanic properties on the World Heritage List, such as the Hawaii Volcanoes National Park”. -
Exploration of Lava Tubes in the Teide National Park, a Martian Analog
First International Planetary Cave Research Workshop (2011) 8004.pdf Exploration of lava tubes in the Teide National Park, a martian analog. A. D. Morse 1, A. Lainez 2 and K.T. Howard 3, 1Planetary and Space Sciences Research Institute, The Open University, Walton Hall, Milton Keynes, MK7 6AA UK ([email protected]), 2Department of Mineralogy, The Natural History Museum, Cromwell Road, London, SW7 5BD, UK, 3Cueva del Viento Centro Visitantes, Icod de los Vinos, Tenerife, Spain. Introduction: Lava tubes and volcanic caves are a and the walls were damp. The bottom of the cave was potential habitat for Martian life and a target for astro- filled with boulders blocking any further progress, al- biological studies[1]. Evidence for the existence of though the cold damp draught indicated that the cave Martian caves such as long lava channels and lines of was probably a lot deeper. pits have been identified from orbiting space craft [2] and epithermal neutron maps indicate the presence of water a few metres below the surface [3] which would be accessible to cave life. Inside the caves, any life will have access to water and would be sheltered from the harsh surface conditions of UV radiation and low humidity as well as from the prevailing weather condi- tions. The caves in the Teide national park of Tenerife are an ideal terrestrial analogue of Martian caves. They are situated at an altitude of 2500 m in an area of low humidity. Additionally, contamination is reduced as access to the area is limited for conservation reasons. -
Tenerife by Car the Best Routes
www.webtenerife.com Tenerife by car The best routes Index TENERIFE BY CAR day 3 TOUR 4. The magic of the Isla Baja 25 The whales 11 Map of the island 04 TOUR 5. On the way to heaven 27 Los Gigantes cliffs 11 Now that you’ve arrived! 05 Masca 11 TOUR 6. The Wine Route 29 A DAY IN TENERIFE TOUR 1. A trip through the Tertiary TOUR 7. Fusión of the sea Mount Teide National Park 06 and a World Heritage Site 12 and the mountains in the south of the Island 31 San Cristóbal de La Laguna 06 Ecological treasure 14 Lunar landscape 31 Candelaria 07 TOUR 2. Tradition and the The Mecca for wind sports 32 avant-garde on the coast 16 THREE DAYS IN TENERIFE A centre of tourism 33 day 1 The capital 17 Las Teresitas 18 El Teide and La Orotava TOUR 8. Whale sanctuary 35 Isla Baja 08 TOUR 3. A valley of charm 20 day 2 Puerto de la Cruz 21 USEFUL INFORMATION Santa Cruz and La Laguna Rambla de Castro 22 Tourist Information offices 36 Las Teresitas 09 The Thousand-Year-Old Laurel forest 10 Dragon Tree 23 The Rock of Garachico 24 Tenerife by car TOURIST ATTRACTIONS 1 Auditorio Cruz del 2 Museo de la Naturaleza y el Hombre 12 TEGUESTE Carmen 1 3 TEA Tenerife Espacio de las Artes 5 4 Museo de la Ciencia y el Cosmos LA LAGUNA 5 Museo de Historia TACORONTE 6 Centro Alfarero Casa Miquelas EL SAUZAL 4 3 Casa del Vino 7 SANTA CRUZ DE TENERIFE 7 2 Loro Parque TF-2 8 LA MATANZA 21 1 Cueva del Viento LA VICTORIA 9 PUERTO DE 10 Rambla de Castro LA CRUZ SANTA ÚRSULA 3 11 Museo de Historia: Casa de Carta 8 15 18 11 EL ROSARIO 2 12 Paisaje Lunar 10 BUENAVISTA SAN JUAN DE 13 Siam Park 4 LA OROTAVA DEL NORTE LA RAMBLA 14 Jungle Park LOS SILOS GARACHICO 16 22 15 Casa de la Aduana (Artenerife) ICOD DE LOS REALEJOS CANDELARIA EL TANQUE LOS VINOS 16 Casa Torrehermosa (Artenerife) LA GUANCHA 6 17 Playa de las Américas (Artenerife) ARAFO Masca 9 18 Puerto de La Cruz (Artenerife) 19 Playa de Las Vistas (Artenerife) GÜÍMAR 20 Puerto Colón (Artenerife) 21 Santa Cruz. -
Morphological and Structural Analysis in the Anaga Offshore Massif, Canary Islands: Fractures and Debris Avalanches Relationships
Marine Geophysical Researches (2003) 24: 91–112 © Springer 2005 DOI 10.1007/s11001-004-1335-3 Morphological and structural analysis in the Anaga offshore massif, Canary Islands: fractures and debris avalanches relationships P. Llanes1,∗, A. Muñoz2, A. Muñoz-Mart´ın1,J.Acosta2, P. Herranz2,A.Carbo´1,C.Palomo2 & ZEE Working Group∗∗ 1Universidad Complutense de Madrid. Facultad C.C. Geologicas.´ Departamento de Geodinamica.´ 28040 Madrid, Spain 2Instituto Español de Oceanograf´ıa. Grupo de Cartograf´ıa Multihaz. C. de Mar´ıa n◦ 8. 28002 Madrid, Spain ∗Corresponding Author (Phone: +34-913944834; Fax: +34-913944631; E-mail: [email protected]) Key words: Anaga massif, bathymetry, debris avalanche, fractures, Tenerife island Abstract As part of the ‘National Hydrographic and Oceanographic Research Plan for the Spanish Exclusive Economic Zone’, multibeam bathymetry and seismic reflection profiles were obtained in the Canary Islands aboard the R/V Hespérides. The submarine flanks of the Anaga offshore extension of Tenerife Island are here studied to analyze its geomorphology. In the north sector of the Anaga submarine massif, the extension of the Anaga Debris Avalanche has been mapped for the first time, and a volume of 36 km3 was calculated. The relationship between the Anaga and Orotava Debris Avalanches is also described. Faulting has been recognized as a key process for the occurrence of debris avalanches and the growth of volcanic lineaments. Moreover, faulting affects previous structures and the channelling of debris flows. Structural analysis shows the typical radial pattern of an oceanic island. In addition, a NE-SW dominant direction of faulting was obtained, consistent with the Tenerife Island structural trend seen in the Anaga Massif and Cordillera Dorsal.