ROUTE AROUND the ISLAND of LANZAROTE Lanzarote – One Week Route Around the Island
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Redalyc.Urbanismo Y Crecimiento Turístico En Lanzarote Durante La
Papeles de Geografía ISSN: 0213-1781 [email protected] Universidad de Murcia España González Morales, Alejandro Urbanismo y crecimiento turístico en lanzarote durante la segunda mitad del siglo XX Papeles de Geografía, núm. 44, julio-diciembre, 2006, pp. 39-57 Universidad de Murcia Murcia, España Disponible en: http://www.redalyc.org/articulo.oa?id=40704403 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Papeles de Geografía ISSN: 0213-1781 2006, 44; pp. 39-57 URBANISMO Y CRECIMIENTO TURÍSTICO EN LANZAROTE DURANTE LA SEGUNDA MITAD DEL SIGLO XX Alejandro González Morales* Universidad de Las Palmas de Gran Canaria RESUMEN En este trabajo analizamos las diferentes etapas por las que ha pasado el desarrollo turís- tico de la isla de Lanzarote. Se distinguen tres periodos de características diferenciadas. El primero, antes de los años setenta, supone el desarrollo de una incipiente industria turística, donde predominan el capital belga y francés; el segundo es un periodo que abarca desde 1973 hasta 1983, en estos 10 años la isla experimenta un cambio sustancial, el capital alemán se vuelve hegemónico y se desarrolla con fuerza el denominado turismo de masas, sobre todo en el municipio de Tías (Puerto del Carmen); por último a partir de principios de los ochenta nos encontramos con una etapa de similares características que la anterior hasta 1995, con un gran desarrollo de Yaiza y Teguise, a partir de esta fecha y hasta la actualidad se introducen los valores de sostenibilidad, aunque sin demasiado éxito, pues se sigue construyendo mucho y no de precisamente alta calidad. -
Assessing Qualitative Long-Term Volcanic Hazards at Lanzarote Island
1 Assessing qualitative long-term volcanic hazards at Lanzarote 2 Island (Canary Islands) 3 4 Laura Becerril1, Joan Martí1, a, Stefania Bartolini1, Adelina Geyer1 5 1. Institute of Earth Sciences Jaume Almera, ICTJA-CSIC, Lluís Solé i Sabarís s/n, 08028 Barcelona, 6 Spain 7 a. Now at the Institut des Sciences de la Terre d’Orleans (ISTO, CNRS), Université d’Orleans, Campus 8 Géosciences, 1A rue de la Férolerie, F45071, Orleans Cedex 2. 9 10 11 Correspondence to: Laura Becerril ([email protected]) 12 13 Abstract. Conducting long-term hazard assessment in active volcanic areas is of primordial importance 14 for land-use planning and to define emergency plans able to be applied in case of a crisis. Definition of 15 scenario hazard maps helps to mitigate the consequences of future eruptions by anticipating to the events 16 that may occur. Lanzarote is an active volcanic island that has hosted the largest (>1.5 km3 DRE) and 17 longest (6 years) eruption, the Timanfaya eruption (1730-36), on the Canary Islands in historical times 18 (last 600 years). This eruption brought severe economic losses and forced local people to migrate. In spite 19 of all these facts, no comprehensive hazard assessment neither hazard maps have been developed for the 20 island. In this work, we present an integrated long-term volcanic hazard evaluation using a systematic 21 methodology that includes spatial analysis and simulations of the most probable expected eruptive scenar- 22 ios. 23 24 1 Introduction 25 26 Active volcanic areas require conducting long-term hazard assessment in order to ensure a rational land 27 planning and to elaborate precise emergency plans that can be applied in case of a crisis. -
– Canary Islands Cruise Program from Tenerife –
– Canary Islands Cruise Program from Tenerife – DAY PLACE PROGRAM Embarkation between 14:30 and 16:00 from Los Christianos Port, bustling with life due to its 1 Tenerife - wide range of bars, restaurants and resorts. After you board, you will enjoy a Welcome Cristianos Port Cocktail followed by an evening dinner. Late embarkation is possible until 23:00. Overnight in port. Early morning arrival in Santa Cruz de la Palma. Optional full day excursion visiting the historic old town of Santa Cruz de La Palma and to Taburiente National Park. Then travel 2 La Palma - towards the crater itself, weather permitting. A visit to El Paso, a nice traditional Canary Santa Cruz de village will take place just in time before we stop in a restaurant for an inclusive lunch. The la Palma tour continues with the visit La Glorieta near Las Manchas and arrival at the Volcano San Antonio for an optional walk to the volcano rim. Overnight in Port. Early morning sailing and arrival in Valle Gran Rey, La Gomera Island. Upon morning arrival in Valle Gran Rey de La Gomera. There you can participate in the optional half day 3 La Gomera - excursion passing through the villages of Arure and Valle Hermoso to reach the small village Valle Gran Rey of Rosas, where you can enjoy a demonstration of the famous Gomera whistling language. Continue to the Garajonay National Park, a paradise of laurel, nature reserve, declared as Universal Patrimony by the UNESCO. Evening sailing to Tenerife. We arrive in Santa Cruz de Tenerife in the morning. -
Seabirds in the Northern Islets of Lanzarote, Canary Islands
2003 Breeding seabirds in Lanzarote 41 Status and distribution of breeding seabirds in the northern islets of Lanzarote, Canary Islands Beneharo Rodríguez Leandro de León Aurelio Martín Jesús Alonso & ManuelNogales Rodriguez B., de León L., Martin A., Alonso J. & Nogales M. 2003. Status and distribution of breeding seabirds in the northern islets of Lanzarote, Canary Islands. Atlantic We describe the results Seabirds 5(2): 41-56. ofa survey ofbreeding seabirds carried out between 2000 and 2002 in the northern islets of Lanzarote, Canary Islands, with particular emphasis on their status and distribution. For White-faced Storm- petrel Pelagodroma marina, Madeiran Storm-petrel Oceanodroma Castro, Lesser Black- backed Gull Larus [fuscus] graellsii and Yellow-leggedGull Larus cachinnans atlantis, some new colonies were discovered on different islets. All species have maintained their numbers the last 15 with the the which over years, exception of Yellow-leggedGull, has undergonea in well-documented increase; 1987, about 400 breedingpairs were estimated but during the present study, almost 1000 pairs were counted. In addition, some comments on threats to these seabird populations are presented. On La Graciosa, feral cats are a majorpredator of the European Storm-petrelpopulation, killing more than 50 birds duringthis study alone. Departamento de Biologia Animal (Zoologia), Universidad de La Laguna, 38206 Tenerife, Canary Islands, Spain. E-mail: [email protected] INTRODUCTION The most important sites for seabirds in the Canarian archipelago are small uninhabitedrocks where introduced or islets, generally no predators are present, such as Roques de Salmor (El Hierro), Roques de Anaga (Tenerife), Isla de Lobos (Fuerteventura) and especially the northem islets of Lanzarote (known as the Chinijo Archipelago; Martin & Hemandez 1985; Martin & Nogales 1993; Martin & Lorenzo 2001). -
The Volcanic Islands of the Canaries from Lanzarote to Tenerife Tue 03 November 2020 Tue 10 November 2020
The Volcanic Islands of the Canaries From Lanzarote to Tenerife Tue 03 November 2020 Tue 10 November 2020 During our one-week discovery cruise, we will experience the stunningly beautiful landscape of the Canary Islands. From Lanzarote, the 'Island of the Fire Mountains', we set course for Tenerife, the 'Island of Eternal Spring'. Blue-water cruising in one of the most beautiful areas of the Atlantic, the wind in our sails, being accompanied by dolphins, the volcanoes as landmarks: these are all things that make this cruise an experience you will never forget. Come on board and enjoy relaxation under the sails. Enjoy a swim in the ocean and a stroll along a beach of the Canary archipelago. This is where you will go on board: Lanzarote – Volcanic craters in the midst of the trade winds Our crew will welcome you on board in the Marina Puerto Calero, near the port of Arrecife on the Canary island of Lanzarote. Embarkation takes place at 19:00 hours. Afterwards, you will have dinner together in the comfortable lounge, where you will quickly feel at home on the Eye of the Wind's deck and get to know your fellow sailors. The trade winds bring warm air from Africa, creating a pleasant climate. Even in November, average air and water temperatures reach about 20 degrees around the eastern islands of the Canary Islands archipelago. The black, brown and red peaks of the volcanic cones rise more than 600 metres into the air. Parts of the island are covered with a black layer of lava; palm trees and agaves make up most of the flora. -
Canary Islands)
|00000325|| J. Geophys. 46, 319-334, 1979 Journal of Geophysics Palaeomagnetism and the Early Magmatic History of Fuerteventura (Canary Islands) K. M. Storetvedt, H. Mongstad Vage, S. Aase, and R. L0vlie Department of Geophysics, University of Bergen, Allegt. 70, N-5014 Bergen-Universitetet, Norway Abstract. Thermal and alternating field demagnetization combined with studies of the convergence points of remagnetization circles have been carried out on a variety of '"ocks from Fuerteventura. The older (post-Albian) rocks, including the basement plutonics, the sheeted dike complex and the earliest subaerial lava sequence (lava Series I), have a multicomponent remanence while the younger lava Series II of Miocene/Pliocene age has dominantly a one-component magnetization. Comparison of the results with recent pa laeomagnetic data from Gran Canaria/Tenerife and with results from conti nental Africa and Europe suggest a late Cretaceous origin of the basal intrusive rocks while the subaerial volcanism (lava Series I) most likely initiated at around the Cretaceous/Tertiary boundary. This implies that there is a nearly 50-m.y.-long period of volcanic quiescence and erosion between lava Series I and lava Series II. The apparent contradiction between these conclusions and the few K/Ar dates available is discussed. Key words: Palaeomagnetism - Age of early Fuerteventura magmatism. 1. Introduction The oldest exposed rocks in Fuerteventura are found in the western part of the island, the so-called Betancuria massif (Fuster et al., 1968; Rothe, 1968) (Fig. 1). This basement complex, which Gastesi (1973) believes to be a piece of uplifted oceanic crust, has a core of layered basic and ultra-basic plutonics which in part occurs in faulted contact with Lower-Middle Cretaceous terrige nous and calcareous elastic, deep-water sediments of basically turbiditic origin (Robertson and Stillman, 1979). -
Boletín 156/2019
X legislatura Número 156 Año 2019 25 de noviembre El texto del Boletín Oficial del Parlamento de Canarias puede ser consultado gratuitamente a través de Internet en la siguiente dirección: http://www.parcan.es PROPOSICIONES NO DE LEY EN PLENO En trámite 10L/PNLP-0063 Del GP Socialista Canario, sobre la contratación de un servicio de transporte sanitario aéreo mediante helicóptero de soporte vital avanzado, con base en Fuerteventura. Página 1 10L/PNLP-0065 Del GP Nueva Canarias (NC), sobre regulación efectiva del juego y las apuestas en Canarias contra las adicciones. Página 5 PROPOSICIONES NO DE LEY EN PLENO En trámite 10L/PNLP-0063 Del GP Socialista Canario, sobre la contratación de un servicio de transporte sanitario aéreo mediante helicóptero de soporte vital avanzado, con base en Fuerteventura. (Registro de entrada núm. 5407, de 15/11/2019). Presidencia La Mesa del Parlamento, en reunión celebrada el día 20 de noviembre de 2019, adoptó el acuerdo que se indica respecto del asunto de referencia: 2.- Proposiciones no de ley en pleno 2.1.- Del GP Socialista Canario, sobre la contratación de un servicio de transporte sanitario aéreo mediante helicóptero de soporte vital avanzado, con base en Fuerteventura. De conformidad con lo establecido en el artículo 185 del Reglamento de la Cámara, la Mesa acuerda: Primero.- Admitir a trámite la proposición no de ley de referencia y disponer su tramitación ante el Pleno. Segundo.- Ordenar su publicación en el Boletín Oficial del Parlamento. Tercero.- Trasladar este acuerdo al Gobierno y al autor de la iniciativa. En ejecución de dicho acuerdo y de conformidad con lo previsto en el artículo 111 del Reglamento del Parlamento de Canarias, dispongo su publicación en el Boletín Oficial del Parlamento. -
Canary Islands
CANARY ISLANDS EXP CAT PORT CODE TOUR DESCRIPTIVE Duration Discover Agadir from the Kasbah, an ancient fortress that defended this fantastic city, devastated on two occasions by two earthquakes Today, modern architecture dominates this port city. The vibrant centre is filled with Learn Culture AGADIR AGADIR01 FASCINATING AGADIR restaurants, shops and cafes that will entice you to spend a beautiful day in 4h this eclectic city. Check out sights including the central post office, the new council and the court of justice. During the tour make sure to check out the 'Fantasy' show, a highlight of the Berber lifestyle. This tour takes us to the city of Taroudant, a town noted for the pink-red hue of its earthen walls and embankments. We'll head over by coach from Agadir, seeing the lush citrus groves Sous Valley and discovering the different souks Discover Culture AGADIR AGADIR02 SENSATIONS OF TAROUDANT scattered about the city. Once you have reached the centre of Taroudant, do 5h not miss the Place Alaouine ex Assarag, a perfect place to learn more about the culture of the city and enjoy a splendid afternoon picking up lifelong mementos in their stores. Discover the city of Marrakech through its most emblematic corners, such as the Mosque of Kutubia, where we will make a short stop for photos. Our next stop is the Bahia Palace, in the Andalusian style, which was the residence of the chief vizier of the sultan Moulay El Hassan Ba Ahmed. There we will observe some of his masterpieces representing the Moroccan art. With our Feel Culture AGADIR AGADIR03 WONDERS OF MARRAKECH guides we will have an occasion to know the argan oil - an internationally 11h known and indigenous product of Morocco. -
Lanzarote and Chinijo Islands: an Anchialine UNESCO Global Geopark
Lanzarote and Chinijo Islands: An Anchialine UNESCO Global Geopark Alejandro Martínez, Guillermo García-Gómez, Álvaro García-Herrero, Andrea Di Cesare, Gianluca Corno, Rogelio Herrera, Leopoldo Moro, Ester Eckert, and Diego Fontaneto Abstract throughout the 20th century, who have regarded the island The Lanzarote and Chinijo Islands UNESCO Global as a model to understand the origin and evolution of similar Geopark hosts one of the most extensive and diverse groups in other areas of the world. The anchialine habitats volcanic anchialine ecosystems in the world, consisting of in Lanzarote are subject to intense recreational use and the water bodies with marine origin that penetrated inland island itself is a major touristic destination. However, through coastal crevicular systems. Marine infiltration is geologist and biologist working in the local government facilitated by the low rainfall and the permeability of the offices, as well as in UNESCO Global Geopark and coastal terrains. Best known for Túnel de la Atlántida, Biosphere Reserve Institutions have started close collab- Lanzarote has other types of anchialine habitats, such as orations with the touristic centers and independent scientist pools, lakes, and even hand-made wells, all of them from several universities and research centers around the interconnected with the crevicular system. So far, 39 world with the goal of implementing novel conservation endemic stygobitic species of crustacean, annelids, and policies based on the results of state-of-art research. This platyhelminthes have been described in the island. Some of strategy will ensure not only a better understanding of the them belong to lineages previously interpreted as Tethyan anchialine ecosystems in the island in the near future, but vicariant relicts because they belong in ancient groups also its long-term preservation. -
Spatial Patterns and Response to Wave Exposure of Shallow Water Algal Assemblages Across the Canarian Archipelago: a Multi-Scaled Approach
MARINE ECOLOGY PROGRESS SERIES Vol. 311: 15–28, 2006 Published April 13 Mar Ecol Prog Ser Spatial patterns and response to wave exposure of shallow water algal assemblages across the Canarian Archipelago: a multi-scaled approach Fernando Tuya1, 2,*, Ricardo J. Haroun1 1BIOGES, Department of Biology, Campus Tafira, University of Las Palmas de Gran Canaria, 35017 Las Palmas, Canary Islands, Spain 2Present address: Center for Ecosystem Management, Edith Cowan University, 100 Joondalup Drive, Joondalup, Western Australia 6027, Australia ABSTRACT: We conducted a mensurative survey to investigate spatial variability and the effect of wave exposure at a range of spatial scales including islands (100s of km apart), locations within islands (10s of km apart), and sites within locations (100s of m apart), on the composition, abundance and distribution of shallow water algal assemblages across subtidal hard bottoms of the Canarian Archipelago (eastern Atlantic). A multi-scaled hierarchical sampling design provided the framework for quantifying the variation among samples due to spatial scale and level of wave exposure. Ran- domly placed 50 × 50 cm squares were deployed in shallow rocky-reefs to assess community struc- ture and dominance. Non-parametric multivariate techniques, as well as univariate tests, provided evidence to collectively suggest that shallow water algal assemblages differed between protected (leeward) and exposed (windward) shores, with a consistency of effects across islands, while differ- ent spatial scales were also involved in the variability and patchiness of these assemblages. In this sense, differences were clearly taxon and/or group-specific. In general, the presence and abundance of frondose fucoid species was greater on exposed shores than on protected shores, whereas turf- algae dominated along the protected shores of each island. -
Current Status and Distribution of Birds of Prey in the Canary Islands
Bird Conservation International (2004) 14:203–213. BirdLife International 2004 DOI: 10.1017/S0959270904000255 Printed in the United Kingdom Current status and distribution of birds of prey in the Canary Islands CÉSAR-JAVIER PALACIOS Summary I analyse recent trends in the status and distribution of breeding birds of prey in the Canary Islands (Spain). Populations of Barbary Falcon Falco peregrinus pelegrinoides, Eleonora’s Falcon Falco eleonorae, Sparrowhawk Accipiter nisus granti, Buzzard Buteo buteo insularum and Osprey Pandion haliaetus recovered throughout the 1990s. Egyptian Vulture Neophron percnopterus majorensis continues to be seriously threatened, with a total popula- tion of only around 130 birds. There is a lack of information on status of nocturnal birds of prey, especially of the Canary subspecies of Barn Owl Tyto alba gracilirostris, whose numbers seem to have decreased. Genetic studies should be carried out to clarify the taxonomic status of the birds of prey of the Canary Islands. Introduction The Atlantic archipelago of the Canary Islands is situated 100 km from the coast of Africa, forming part of the Macaronesian region. It comprises seven islands and a series of islets totalling 7,447 km2 (Fernández-Palacios and Días 2001). Seven species of diurnal birds of prey and two nocturnal species breed on the islands, with a total of 11 subspecies with high conservation interest, five of which are endemic to the Canary Islands and two to the Macaronesian region. The first detailed study on the status and distribution of birds of prey of the Canaries was made in 1987/8 by the Tenerife Museum of Natural Sciences (Delgado et al. -
Deep Volcanic Morphology Below Lanzarote, Canaries
1 (Submitted to Journal of Volcanology and Geothermal Research, second revised manuscript, November 2018) 2 Deep volcanic morphology below Lanzarote, Canaries, 3 from gravity inversion: 4 New results for Timanfaya and implications. 5 6 Antonio G. Camacho1, Juan F. Prieto2, Eumenio Ancochea3, and José Fernández1,* 7 1 Instituto de Geociencias (CSIC, UCM). Calle del Doctor Severo Ochoa, nº 7. Facultad de 8 Medicina (Edificio Entrepabellones 7 y 8, 4ª planta). Ciudad Universitaria. 28040-Madrid, 9 Spain. 10 2 ETS de Ingenieros en Topografía, Geodesia y Cartografía, Universidad Politécnica de Madrid, 11 28031-Madrid, Spain. 12 3 Departamento de Petrología y Geoquímica, Fac. CC. Geológicas, Universidad Complutense de 13 Madrid, 28040-Madrid, Spain. 14 *Corresponding author: José Fernández ([email protected]) 15 16 Highlights: 17 - We use published and new gravity data with an improved inversion methodology 18 - 3D density structure is determined solving the inverse gravity problem 19 - Three high-density sources are described as resulting of main volcanic complexes 20 - Timanfaya’s plumbing system is inferred as branches of magma from SW intrusive body 21 - Comparison of gravity results and geology gives different cases of correlation 1 22 Abstract. 23 The deep roots of oceanic island volcanoes are poorly known and geophysical models can help 24 to constrain processes such as magma storage and transport before and during eruptions. 25 Lanzarote, Canary Islands, is a volcanic island in post-erosional phase where, in the 18th 26 century, one of the most important historical eruptions, considering duration and volume, of the 27 Canary Islands took place in the Timanfaya area.