Custom Search

sábado, 30 de octubre de 2010

La Gomera island


La Gomera (pronounced [la ɣoˈmeɾa]) is one of Spain's Canary Islands, located in the Atlantic Ocean off the coast of Africa. In area, it is the second-smallest of the seven main islands of this group. It is located at 28°06′N 17°08′W / 28.1°N 17.133°W / 28.1; -17.133.

Ecology

The island is of volcanic origin and roughly circular; it is about 22 km (15 miles) in diameter and rises to 1487 m (nearly 5000 feet) at the island's highest peak, Garajonay. Its shape is rather like an orange that has been cut in half and then split into segments, which has left deep ravines or barrancos between them. These barrancos, in turn, are covered by the laurisilva - or laurel rain forest.
The upper reaches of this densely wooded region are almost permanently shrouded in clouds and mist, and as a result are covered in lush and diverse vegetation: they form the protected environment of Spain's Garajonay National Park, which was declared a UNESCO World Heritage Site in 1986. The slopes are criss-crossed by paths that present varying levels of difficulty to visitors, and stunning views to seasoned hikers.
The central mountains catch the moisture from the trade wind clouds and yield a dense jungle climate in the cooler air, which contrasts with the warmer, sun-baked cliffs near sea level.
Between these extremes one finds a fascinating gamut of microclimates; for centuries, the inhabitants of La Gomera have farmed the lower levels by channelling runoff water to irrigate their vineyards, orchards and banana groves.

Culture
In 2003, some 19,580 people lived on La Gomera.
The local wine is distinctive, and is often accompanied with a tapa (snack) of local cheese, roasted pork or goat meat. Other culinary specialities include almogrote, a cheese spread, and miel de palma, a syrup extracted from palm trees.
The inhabitants of La Gomera have a unique way of communicating across deep ravines by means of an amazing whistled speech called Silbo Gomero. This whistled language is indigenous to the island, and its existence has been documented since Roman times. Invented by the original inhabitants of the island, the Guanches, Silbo Gomero was adopted by the Spanish settlers in the 16th century and survived after the Guanches died out. When this unique means of communication was threatened with extinction at the dawn of the 21st century, the local government required all children to learn it in school.
In the mountains of La Gomera, its original inhabitants worshipped their god, whom they called Orahan; the summit and centre of the island served as their grand sanctuary. Indeed, many of the natives took refuge in this sacred territory in 1489, as they faced imminent defeat at the hands of the Spaniards, and it was here that the conquest of La Gomera was drawn to a close. Modern-day archaeologists have found several ceremonial stone constructions here, which appear to represent sacrificial altar stones, slate hollows or cavities. It was here that the Guanches built pyres upon which to make offerings of goats and sheep to their god. This same god, Orahan, was known on La Palma as Abora and on Tenerife and Gran Canaria as Arocan. The Guanches also interred their dead in caves, which still dot the landscape.
Christopher Columbus made La Gomera his last port of call before crossing the Atlantic in 1492. He stopped here to replenish his crew's wine and water, intending to stay only four days. However, he became romantically involved with Beatriz de Bobadilla y Ossorio, the governor of La Gomera, and he ended up staying one month. When he finally sailed she gave him cuttings of sugarcane, which became the first to reach the New World. The house in San Sebastián in which he is reputed to have stayed is now a tourist attraction.


La Palma island


La Palma (Spanish pronunciation: [la ˈpalma]) is located at 28°40′N 17°52′W / 28.667°N 17.867°W / 28.667; -17.867, making it the most north-westerly of the Canary Islands. La Palma has an area of 706 km2 making it the fifth largest of the seven main Canary Islands. The total population is about 86,000, of which 18,000 (2003 data) live in the capital, Santa Cruz de la Palma and about 20,000 (2004 data) in Los Llanos de Aridane.
La Palma, like the other islands of the Canary Island archipelago, is a volcanic ocean island. The volcano rises almost 7 km (4 mi) above the floor of the Atlantic Ocean. There is road access from sea level to the summit at 2,423 m (7,949 ft), which is marked by an outcrop of rocks called Los Muchachos ("The Lads"). This is the site of the Roque de los Muchachos Observatory, one of the world's premier astronomical observatories.
La Palma's geography is a result of the volcanic formation of the island. The highest peaks reach over 2,400 m (7,874 ft) above sea level, and the base of the island is located almost 4,000 m (13,123 ft) below sea level. The northern part of La Palma is dominated by the Caldera de Taburiente, with a width of 9 km (6 mi) and a depth of 1,500 m (4,921 ft). It is surrounded by a ring of mountains ranging from 1,600 m (5,249 ft) to 2,400 m (7,874 ft) in height. Only the deep Barranco de las Angustias ("Valley of Fear") canyon leads into the inner area of the caldera which is a national park. It can be reached only by hiking. The outer slopes are cut by numerous gorges which run from 2,000 m (6,562 ft) down to the sea. Today, only few of these carry water due to the many water tunnels that have been cut into the islands structure.
In 1815, the great German geologist Leopold von Buch visited the Canary Islands. It was as a result of his visit to La Palma and Tenerife where he visited the Las Cañadas and Taburiente calderas, that the Spanish word for cauldron - "Caldera" - was introduced into the geological vocabulary.
From the Caldera de Taburiente  to the south runs the ridge Cumbre Nueva. The southern part of La Palma is dominated by the Cumbre Vieja, a volcanic ridge formed by numerous volcanic cones built of lava and scoria. The Cumbre Vieja is active - but dormant, with the last eruption occurring in 1971 at the Teneguia vent which is located at the southern end of the Cumbre Vieja - Punta de Fuencaliente, (The Point of the Hot Fountain).
La Palma is dominated by the colours blue, green and black. Blue represent the surrounding ocean, Green represents the abundant plant life (which is the most diverse in the Canary Islands) and Black comes from the volcanic rocks that forms the landscape and the numerous playas (beaches) of black sand.
La Palma is nicknamed "Isla Bonita"  ("beautiful island") and the "island of San Pedro" (after its patron Saint: Peter). San Pedro is also a music venue on the island where international bands play, something which may be referred to in La Isla Bonita.
Santa Cruz de La Palma (the island's main port) retains many elegant 17th and 18th century houses, and produces high quality hand made cigars made from locally grown tobacco.
Economy
The local economy is based on a variety of things including: tourism and agriculture. Platanos (or Bananas) are grown throughout the island with many banana farms found on the western side of the island in the valley of Los Llanos de Aridane. Other plants include: Strelitzia (or 'Bird of Paradise') flowers, avocados, and grapes (which are grown well in the volcanic soil). The wine from the grapes is prized. Local ranchers have other herds such as cows and goats (from which they make goat cheese).
Fisherman in 'Puerto Naos' will catch fish to sell at the market.
Flora and fauna




As with all the Canary Islands, La Palma has several endemic species.Although large areas have been deforested, the upland areas of La Palma retain some of the temperate cloud forest, or laurisilva (laurel forest), dominated by Laurus, but including Juniperus cedrus (Canary Islands Juniper) and other trees. This is a relic of the Pliocene subtropical forests which used to cover all the Canary Islands.
The Canary Island Pine (Pinus canariensis) is endemic to all the Western Canary Islands, whilst Genista stenopetala, or sweet broom and Spartocytisus supranubius, a white broom known locally as Retama del Teide, are native to La Palma and Tenerife. Echium webbii, a variety of Echium virescens (Tower of jewels) is endemic to La Palma, as are Ceropegia fusca and Ceropegia dichotoma; varieties of Cardoncillo.

Fuerteventura island


Fuerteventura (pronounced [fweɾteβenˈtuɾa]), a Spanish island, is one of the Canary Islands, in the Atlantic Ocean off the coast of Africa. It is situated at 28°20' north, 14°00' west. At 1,660 km² it is also the second largest of the islands.
Geography
Located just 100 kilometres off the coast of North Africa, it is the second biggest of the islands, after Tenerife, and has the longest beaches in the archipelago. The island is a destination for sun, beach and watersports enthusiasts. It lies on the same latitude as Florida and Mexico and temperatures here rarely fall below 18 °C (64 °F) or rise above 24 °C (75 °F). There are no fewer than 152 beaches along its coastline - 50 kilometres of fine, white sand and 25 kilometres of black volcanic shingle.
Climate



The climate on Fuerteventura is pleasant throughout the year. The island is also often referred to as the island of eternal spring. The sea adjusts the temperature making the hot Sahara winds blow away from the island. The island's name in English translates as 'strong fortune' or 'strong wind', the Spanish word for wind being 'viento'. During the winter months, temperatures average a high of 22 °C (72 °F) and a low of around 15 °C (59 °F) whereas during the summer a mean high of 35 °C (95 °F) and a low of 20 °C (68 °F) can be expected. Precipitation is about 147 mm per year, most of which falls in the winter.
A sandstorm known as the Calima - (similar to the Scirocco wind that blows North from the Sahara into Europe) - blows to the southwest from the Sahara desert and can cause high temperatures, low visibility and drying air. Temperatures during this phenomenon rise temporarily by approximately 10 degrees Celsius. The wind brings in fine white sand, visibility can drop to between 100 to 200 m (328.08 to 656.17 ft) or even lower and can even bring the African locusts to the island.
Economy



The economy of Fuerteventura is mainly based on tourism. Primary tourist areas are located around the existing towns of Corralejo in the north and Morro Jable in Jandia, plus the purely tourist development of Caleta de Fuste, south of Puerto del Rosario. Other main industries are fishing and agriculture (cereals and vegetables). The famous Majorero cheese is locally made from the milk of the indigenous majorera goat.

Tenerife island


Tenerife (Spanish pronunciation: [teneˈɾife]) (Webster's pronunciation: \ˌte-nə-ˈrē-(ˌ)fā, -ˈrēf, -ˈrif\ ... 4 syllables, not 2) is the largest of the seven Canary Islands, Spain, in the Atlantic Ocean off the coast of Africa. Tenerife has an area of 2034.38 square kilometers, and 899,833 inhabitants. It is the most populated island of the Canary Islands and Spain. About 43% of the population of the Canary Islands is on this island. About five million tourists visit Tenerife each year, which is also one of the busiest Spanish resorts and the first of Canary Islands.Tenerife also has one of the world's largest carnivals, and the Carnival of Santa Cruz de Tenerife now aspires to become a World Heritage Site.Tenerife is the only Spanish island that has two airports. Tenerife is the largest number of tourists it receives, it is also headquarters of the main financial institution of the archipelago, Tenerife so is the economic capital of the Canary Islands.


Santa Cruz de Tenerife is the capital of the island and the seat of the island council (cabildo insular). The city is capital of the autonomous community of Canary Islands (shared with Las Palmas), sharing governmental institutions such as Presidency and ministries. Between the 1833 territorial division of Spain and 1927 Santa Cruz de Tenerife was the sole capital of the Canary Islands, until in 1927 a decree ordered that the capital of the Canary Islands be shared, as it remains as at present.
The island is home to the University of La Laguna, which was founded in 1792 and is the oldest university in the Canaries. San Cristóbal de La Laguna (World Heritage Site) is the second city of the island and the third one of the archipelago. The city of La Laguna was also capital of the Canary Islands until Santa Cruz replaced it in 1833.


Tenerife also has the highest elevation of Spain, a World Heritage Site that is the third largest volcano in the world from its base, El Teide. The island's capital contains the architectural symbol of the Canary Islands, the modern Auditorio de Tenerife.

Geography
The oldest mountain ranges in Tenerife rose from the Atlantic Ocean by volcanic eruption which gave birth to the island around twelve million years ago.The island as it is today was formed three million years ago by the fusion of three different islands made up of the mountain ranges of Anaga, Teno and Valle de San Lorenzo,due to volcanic activity from Teide. The volcano is visible from most parts of the island today, and the crater is 17 km long at some points.
Economy
Tenerife is the economic capital of the Canary Islands.Even though Tenerife's economy is highly specialized in the service sector, which makes 78% of its total production capacity, the importance of the rest of the economic sectors is key to its production development. In this sense, the primary sector, which only represents 1.98% of the total product, groups activities that are important to the sustainable development of the island's economy. The energy sector which contributes 2.85% has a primary role in the development of renewable energy sources. The industrial sector which shares in 5.80% is a growing activity in the island, vis-a-vis the new possibilities created by technological advances. Finally, the construction sector with 11.29% of the total production has a strategic priority, because it is a sector with relative stability which permits multiple possibilities of development and employment opportunities.

Flora and fauna
The island of Tenerife has a remarkable ecological diversity in spite of its small surface area, which is a consequence of the special environmental conditions on the island, where its distinct orography modifies the general climatic conditions at a local level, producing a significant variety of microclimates. This vast existence of natural microclimates and, therefore, habitats, means that a rich and diverse flora (1400 species of plants) exists on the island, with well over a hundred entirely endemic to Tenerife. Endemic species include Vipers bugloss, Teide white broom, Teide violet etc. The fauna of the island has many endemic invertebrates and unique reptile, bird and mammal species. The fauna of Tenerife includes some 400 species of fish, 56 birds, 5 reptiles, 2 amphibians, 13 land mammals and several thousand invertebrates, along with several species of marine turtles, whales and dolphins. Before the arrival of the aborigines, Tenerife and the Canaries were inhabited by now-extinct endemic animals, e.g. giant lizards (Gallotia goliath), or the giant rat (Canariomys bravoi).

The vegetation of Tenerife can be divided into 6 major zones that are directly related to altitude and the direction in which they face.
Lower Xerophylic Zone: 0 - 700m. Xerophylic shrubs that are well adapted to long dry spells, intense sun-shine and strong winds. Many endemic species. Spurges, cactus spurge, wax plants, etc.
Thermophile forest: 200 – 600 m. Transition zone. Moderate temperatures and rainfall. Area deteriorated by human activity. Many endemic species: Juniper, dragon trees, palm trees, etc.
Laurel Forest: 500 – 1000 m. Dense forest of large trees, descendants of the Tertiary Age flora, situated in a zone of frequent rainfall and mists. A wide variety of species with abundant undergrowth of bushes herbaceous plants and ferns. Laurels, holly, ebony, mahogany, etc.
Wax Myrtle: 1000–1500 m. A dryer vegetation, poorer in species. It replaces the degraded laurel forest. Of great forestry importance. Wax myrtles, tree heath, holly, etc.
Pine Forest: 800 – 2000 m. Open pine forest, with thin and unvaried undergrowth. Canary Island pine (Pinus canariensis), broom, rock rose, etc.
High mountain: over 2000 m. Dry climate, intense solar radiation and extreme temperatures. Flora well adapted to the conditions.

Lanzarote island


Lanzarote (pronounced [lanθaˈɾote] or [lansaˈɾote]) – a Spanish island in the Atlantic Ocean – is the easternmost of the autonomous Canary Islands approximately 125 km off the coast of Africa and 1,000 km from the Iberian Peninsula. Covering 845.9 km2, it stands as the fourth largest of the islands. The first recorded name for the island, given by Angelino Dulcert, was Insula de Lanzarotus Marocelus, after the Genoese navigator Lancelotto Malocello, from which the modern name is derived. The island's name in the native language was Titerro(y)gatra, which may mean "the red mountains".

Geography
Lanzarote – situated at 29°00' north, 13°40' west – is located 11 km north-east of Fuerteventura and just over 1 km from La Graciosa. The dimensions of the island are 60 km from north to south and 25 km from west to east. Lanzarote has 213 km of coastline, of which 10 km are sand, 16.5 km are beach, and the remainder is rocky. Its dramatic landscape includes the mountain ranges of Famara (671m) in the north and Ajaches (608m) to the south. South of the Famara massif is the El Jable desert which separates Famara and Montañas del Fuego.
The highest peak is Peñas del Chache elevating 670m above sea level. The "Tunnel of Atlantis" is the largest submerged volcanic tunnel in the world. The island has a UNESCO Biosphere Reserve protected site status. But this status was endangered by a local corruption scandal. Since May 2009 police have arrested the former president of Lanzarote, the former mayor of Arrecife and more than 20 politicians and businessmen in connection with illegal building permits along the Lanzarote's coastline. UNESCO has threatened to revoke Lanzarote's Biosphere Reserve status "If the developments are not respecting local needs and are impacting on the environment".
Lanzarote is the easternmost island of the Canary Islands and has volcanic origin. It was born through fiery eruptions and has solidified lava streams as well as extravagant rock formations.

Demographics
As of 2008, a total of 139,506 people lived on Lanzarote  which is an increase of 9.4% from 2006 (127,457). The seat of the island government (Cabildo Insular) is in the capital, Arrecife, which has a population of 59,040. The majority of the inhabitants (73.9%) are Spanish, with a sizeable number of residents from other European nations, mainly British (4.0%), Germans (2.6%) and Irish (2.5%). Other populous groups include immigrants from Colombia, Morocco, Ecuador, Western Africa, China and India, who constitute a large proportion of the remaining 15.6% of the population.


Gran canaria island


Gran Canaria (Spanish pronunciation[ɡɾaŋ kaˈna.ɾja]; originally meaning 'Great [Island] of Dogs') is an island of the Canary Islands. Located in the Atlantic Ocean about 150 kilometers (~93 miles) off the northwestern coast of Africa and about 1350 km (~838 miles) from Europe. Gran Canaria is the second most populous island of the Canary Islands after Tenerife, and the third largest in area after Tenerife and Fuerteventura.

Geography
Gran Canaria is located southeast of Tenerife and west of Fuerteventura. The island is of volcanic origin, mostly made of fissure vents. Gran Canaria is the second most populous island of the Canary Islands after Tenerife. Gran Canaria's surface area is 1,560 km² and its maximum altitude is 1,949 meters (Pico de Las Nieves). It has a round shape, with a diameter of approximately 50 km.] Geology
About 80% of the volume of the island was formed during the Miocene period, between 14 and 9 million years ago. This is called the "Old Cycle" and is estimated to have lasted some 200,000 years and have emitted about 1000 km3, mostly of fissural alkali basalt. This cycle continued with the emission of trachytes, phonolites and peralkaline rocks. This period was followed by one of erosion, which lasted some 4 million years.
A second cycle of volcanic eruptions, known as the "Roque Nublo cycle", took place between 4.5 and 3.4 million years ago. This shorter cycle emitted about 100 km3. Most of the inland peaks were formed by erosion from these materials. This period also started with fissural basalts, but ended with violent eruptions of pyroclastic flows. Some phonolitic features, like the Risco Blanco, were also formed in its last stages.
The third or recent cycle is held to have started some 2.8 million years ago and is considered to be still active. The last eruptions are held to have occurred some 3500 years ago.
The changes in volume, and therefore, weight, of the island have also caused the island to rise above the previous sea level during erosive periods and to sink during eruptive periods. Some of these "fossil beaches" can be seen in the cliff faces of the more eroded northern coast.
Climate
Gran Canaria is noted for its rich variety of micro climates. Generally speaking though, the average daytime high ranges from 20°C in winter, to 26°C in summer. Some cool nights occur in winter, but lows below 10°C are unknown near the coast. Inland the climate is still mild but mountainous areas see the occasional frost or snow. Annual rainfall averages 228 mm, most of this falling in the cooler months, with July, August and September normally rainless. Rainfall is unevenly distributed through the island with some areas being much drier than others. Cloud cover and sunshine is often quite variable during the cooler months, and there can be several rather cloudy days at times in winter. Summers are generally quite sunny however, with the south of the island being most favoured.

CANARY ISLANDS


The Canary Islands (pronounced /kəˈnɛəriː ˈaɪləndz/, also known as the Canaries; Spanish: Islas Canarias, pronounced ) are a Spanish archipelago located just off the northwest coast of mainland Africa, 100 km west of the border between Morocco and the Western Sahara. The Canaries are a Spanish Autonomous Community and an Outermost Region of the European Union. The islands include (from largest to smallest): Tenerife, Fuerteventura, Gran Canaria, Lanzarote, La Palma, La Gomera, El Hierro, La Graciosa, Alegranza and Montaña Clara.
The archipelago's beaches, climate and important natural attractions, especially Teide National Park and Mount Teide (the third largest volcano in the world), make it a major tourist destination, with over 12 million visitors per year, especially Tenerife, Gran Canaria and Lanzarote. The islands have a sub-tropical climate, with long hot days in summer and cooler days in winter.
The capital for the Autonomous Community is shared by the cities of Santa Cruz de Tenerife and Las Palmas de Gran Canaria,which in turn are the capitals of the provinces of Santa Cruz de Tenerife and Las Palmas. Until 1927 Santa Cruz de Tenerife was the only capital. The third largest city of the Canary Islands is San Cristóbal de La Laguna (City World Heritage Site) on the island of Tenerife.
During the times of the Spanish Empire the Canaries were the main stopover for Spanish galleons on their way to America because of the favorable easterly winds.
Custom Search