Travel information, videos and reviews on the beautiful Canary Islands Highlights of Canary Islands Canary Islands The islands of the eternal spring, the archipelago Canary Islands, located in the Atlantic Ocean, form a part of Spain, although they are more closely situated to Africa. The seven islands: La Palma, Tenerife, Gran Canaria, Fuerteventura, Lanzarote, and the two lesser unspoilt islands of Hierro and Gomera, form a part of a volcanic mountain range which lies beneath the Atlantic Ocean. The all year sub-tropical climate, which is regulated by the Gulf Stream and Trade Winds, attracts thousands of visitors every year to the islands who come to enjoy the sun, sea, nightlife and hospitality of the Canarian people. However, it’s all too easy to arrive on your trip to the Canary Islands, plonk yourself on the beach and stay there without actually exploring all of the marvellous attractions that the islands have to offer. History The Canary Islands birth dates back to 8-12 million years ago, with the development of a volcanic mountain range underwater in the Atlantic, which at different intervals erupted forming the archipelago.

It is understood that the first people were of aboriginal and of northwest African origin, they were named Guanches. They were conquered by the Spanish over 500 years ago, but not without putting up a great fight. During the dark ages the islands were forgotten by Europe, and it wasn’t until the 13th century that they were once again rediscovered. In the 14th century they were conquered on behalf of the Spanish by the Norman captain, Jean de Bethencourt, who conquered Lanzarote. When Christopher Columbus stopped on in the Canary Islands on his way to discover the Americas, it put the islands on the map as a strategic stop-off point for many years to follow. Tenerife The island of Tenerife is the largest of the Canary archipelago and is known as the island of eternal spring because of its all year round excellent climate. The island is full of stark contrasts and has a great variety of scenery which varies through the regions. A mountain chain runs through its centre fro Anaga to Teno and on both of its slopes there are large, exuberantly fertile valleys, among them especially La Orotava and Gumar.

In the heart of the chain there is a gigantic, natural crater, called Las Cañadas del Teide, which is about 29 km across and has officially been declared a National Park. It lies over 2,000 m above sea level. North of the crater stands El Pico del Teide (Mount Teide), a 3,718 m high mountain, which is the highest point in Spain. It is snow covered in the winter and marks the island with its unique silhouette. The capital city is Santa Cruz de Tenerife, and the most popular holiday destinations include Playa de las Americas, Los Cristianos,, Puerto de la Cruz and Adeje. Gran Canaria The island of Gran Canaria is situated in the centre of the Canary Island archipelago and is the third largest island after Tenerife and Fuerteventura. Its diversity of landscapes, magnificent beaches and friendly, laid-back atmosphere make Gran Canaria an ideal family holiday destination, anytime of the year. Las Palmas is the capital of the island and its main destination resorts are Puerto Rico, Maspalomas, with its beautiful sand dune nature reserve, Puerto de Mogan and Playa del Ingles.

Fuerteventura Fuerteventura is the island closest to the coast of North Africa, being just 100 kilometres from Morocco. It’s the second largest island and is renowned for its long, golden sand beaches and sand dunes. The island is a paradise for sun worshippers and water sports enthusiasts. It is also believed to be the oldest of all of the islands in the Archipelago. The capital of Fuerteventura is Puerto del Rosario, and its main destination resorts are Antigua, Caleta de Fuste, Corralejo and El Cotillo and Morro Jable. Lanzarote Lanzarote is situated just 70 miles off the coast of Africa, the most easterly of the Canary Islands and one of the smallest. As with the other Canary Islands, Lanzarote has a volcanic landscape, which gives the impression that you are in a lunar environment; so much so that parts of the movie Planet of the Apes were shot here. The island has a UNESCO Biosphere Reserve protected status. Arrecife is the capital of the island and the main destination resorts are Puerto del Carmen, Arrecife, Puerto Calero, Playa Blanca and Costa Teguise.

La Palma La Palma is recognised as one of the most naturally beautiful and unspoilt of all the seven Canary Islands. The development of tourism here has been strictly controlled and if you are after a typical package holiday scenario, with upbeat bars, McDonalds and English breakfast, then La Palma is not the destination for you. The island is popular for those seeking a rural tourism option, walking holidays, eco tourists, or those who just want to chill out in stunning natural surroundings. Don’t expect 365 days of sunshine here either, as La Palma is much more lush, green and considerably wetter! The island is made up three main touristic zones: Los Cancajos to the east, and Puerto Naos and Tazacorte to the west. El Hierro El Hierro is an eco tourist’s heaven and a paradise location for scuba divers. A biosphere reserve, the island hosts very little tourism, but if you want to escape from the humdrum of every day life and people, then El Hierro offers a wonderful option; a land of volcanoes, lava fields, lush valleys and dramatic cliffs which reach up to 1000m high.

La Gomera Home to the National Park and UNESCO World Heritage Site of La Garanjonay, La Gomera is a natural jewel in the archipelago. Where you find species that are otherwise extinct in most destinations, dense forests, deep ravines and a landscape that has been sculpted over millions of years. Cuisine Much of the cuisine of the Canary Islands combines traditional Spanish fayre, with African and South American gastronomy. The volcanic roots of the island are also reflected in the dishes. Fish obviously plays an important role in the gastronomy of Gran Canaria and especially popular are locally caught Langoustines, Mussels, Octopus, Atlantic Mackerel, and Sardines. Meat dishes are popular, especially steaks and stews, but most meat tends to be imported in, as there is not much livestock on the island. The Canary Islands grape growing culture dates back centuries and the unique flavour that comes from the volcanic terrains is very special. There are many wine routes that can be explored throughout the islands, where you can discover the different vineyards and their denominations. Climate The climate of the Canary Islands is mild, enjoying pleasant temperatures all year round.

Average temperatures during the summer months average 26-28C; during the winter months the temperature rarely drops below 22 degrees, making it a perfect all year round destination. See all articles Los Gigantes - Tenerife´s Charming Seaside Town of Giants Los Gigantes is a small, charming seaside town on the west coast of Tenerife. Discover what this must-see destination has to offer you! The Papagayo Beach Collection, Lanzarote Sheltered in the Los Ajaches Natural Park lies the best collection of beaches in Lanzarote - Playas de Papagayo. Welcome to paradise! Top 5 places to go on Fuerteventura The 5 best things to do and places to go on the island of Fuerteventura. Your trip wouldn´t be complete without seeing these places! Ethical whale and dolphin watching in Tenerife Fancy an extra special travel experience? Read our guide to ethical whale and watching trips in Tenerife.

Canary Islands guide | El Hierro, Fuerteventura, Gomera, Gran Canaria, Lanzarote, La Palma, Tenerife | Spanish-Living.com Home › Explore › Regions of Spain › Guide to the Canary Islands The Romans dubbed the Canary Islands the Fortunate Islands when they stumbled upon these hidden treasures off the West coast of Africa more than 2000 years ago. And the Canary Islands are fortunate indeed – blessed with a near perfect climate and magnificent landscapes which make them a magnet for millions of 21st century foreign 'invaders' each year. Despite their proximity to Africa, the islands together form one of the 17 autonomous communities of Spain. But unlike the Costas of mainland Spain, the Canaries enjoy pleasantly warm temperatures throughout the year making them a favourite holiday destination for winter and summer sun seekers alike. The sub-tropical climate of the Canary Islands (which are more or less on the same latitude as Orlando in Florida) is tempered by the cooling Trade Winds and the warm waters of the Gulf Stream.

The result is a 'land of eternal spring' where average temperatures range between 18C and 24C and the sea is a joy to swim in at any time of the year. Together with their glorious weather, these islands offer a huge range of natural and man-made attractions which entice around 14 million visitors a year to their shores. There are vast volcanic craters, spectacular black beaches, ancient forests and crystal clear waters inhabited by whales and dolphins. The quieter islands are a paradise for nature lovers whilst the most popular islands provide action-packed resort areas with every conceivable form of facility and entertainment for foreign visitors. The archipelago consists of five main holiday islands – Tenerife , Lanzarote , Gran Canaria , Fuerteventura and La Palma – along with the two small islands of Gomera and Hierro and several tiny uninhabited islands. Tenerife is the biggest and busiest of all the islands and it’s the one with the broadest appeal. The island offers everything from bustling beachfront resorts and family fun centres to ancient pyramids and Spain’s highest mountain.

Gran Canaria , to the South East of Tenerife , is at the heart of the archipelago and is another island which appeals both to party people and those who prefer to enjoy Canarian culture and quiet country villages. The island boasts one of the most riotous resorts in the Canaries – Playa del Ingles which is a mecca for gays, travellers and round-the-clock revellers. The capital, Las Palmas, has a different feel altogether with its distinctly Canarian character, historic buildings and museums. Elsewhere on the island you’ll find snow capped mountains, traditional villages virtually untouched by tourism, a desert landscape and tropical fruit plantations. Fuerteventura and Lanzarote lie at the eastern edge of the island group, closest to Africa. Fuerteventura has some of the longest and best beaches in the Canaries and attracts watersports enthusiasts and those wanting a relaxing 'sun and sea' holiday rather than foam party aficionados. Lanzarote is home to some of the most mind-blowing landscapes in the world with its weird petrified lava formations, volcanic craters and underground cave systems.

The most westerly islands - La Palma , La Gomera and El Hierro – are more lush, green and unspoilt than the 'big four' holiday islands. They’re the haunts of artists, walkers and nature lovers who prefer to steer clear of resorts geared to the package holiday market. It’s a common misconception that the Canaries are named after the songbirds which inhabit the islands. In fact the reverse is true and the birds take their name from the islands which were home to packs of wild dogs in ancient times. The Spanish word Canarias comes from the Latin word meaning 'of the dogs'.

General Info for the Canary Islands The following numbers should only be called if there is an emergency: 091 - Policia Nacional Canary Islands - Boat Trip Boat Trip Boat trip finder in Spain Language: Home » Canary Islands Canary Islands Canary Islands are an archipelago in the Atlantic Ocean which forms one of the seventeen autonomous communities of Spain , recognized as a nationality , and one of the outermost regions of the Union Europea.5 It consists of seven main islands : El Hierro , La Gomera , La Palma and Tenerife , which are the province of Santa Cruz de Tenerife , and Fuerteventura, Gran Canaria and Lanzarote , which make up the province of Las Palmas.6 also part of the island territories Canary Archipelago Chinijo (La Graciosa, Alegranza , Montaña Clara , Roque Roque East and West ) and Isla de Lobos, all belonging to the province of Las Palmas. La Graciosa is the only of these islands are inhabited . The Canary Islands are one of the places with the best climate in the world to enjoy an exceptional holiday in any season .

Seven different and unique islands , ideal to unwind from the routine, recharge your batteries and return home with renewed body and mind . Its beaches , its volcanic nature , lively and hospitable lifestyle and the ability to choose from all kinds of outdoor activities , and a worthy pointing and quality leisure offer, make the most repeat visitors over once . Canary Islands – Travel guide at Wikivoyage Regions[ edit ] The following islands make up the Canary chain: Gran Canaria — The largest island by population, its capital city (Las Palmas de Gran Canaria) has the shared title of capital of the Canaries. Green and steep in the north, dry and flat in the south. Fuerteventura — good for windsurfing Lanzarote — Low lying and arid, with a spectacular volcanic landscape in the west of the island (National Park of Timanfaya). The capital is Arrecife and has its own airport (ACE code). Lanzarote is also of volcanic origin. The island, along with others, emerged after the breakup of the African and the American continental plates. The greatest recorded eruptions occurred between 1730 and 1736. This area is preserved as the Timanfaya National Park.

Tenerife — The island of Tenerife has many museums and monuments that serve as portrayals of its rich history. As the largest island of the seven, its oldest mountain ranges are young compared to its neighboring islands. Volcanic activity did not begin to occur here until eight to twelve million years ago, while other islands had it well over 20 million years ago. The highest mountain of Spain, El Teide. 3rd largest volcano in the world in extension (Volcano 3718 meters high). The Capital city is Santa Cruz de Tenerife , home to the Canary Island Parliament. The title of capital city is shared with San Cristóbal de La Laguna. With a population of 899,833 people, it is the most populated island. Another popular city on the island is San Cristobal de La Laguna. Here you can find the oldest university in the Canary Islands. La Gomera — The Magic Isle - walker's paradise. It is shaped like an orange that has been cut in half and split into segments. The terrain is rough, which has left deep ravines or barrancos between them.

These barrancos, in turn, are covered by the laurisilva ((laurel rain forest)). It is home to the only remaining Laurisilva rain forest in northern Africa. The local wine has a distinct taste, and is often accompanied with a tapa (snack) of local cheese, roasted pork or goat meat. Other cultural dishes include almogrote, a cheese spread, and a syrup extracted from palm trees called miel de palma. The local people have a unique way of communicating across deep ravines by using a whistled speech called Silbo Gomero. This whistled language is indigenous to the island, and its existence has been documented since Roman times. La Palma — 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's geographic layout is a result of the volcanic formation of the island.

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, located at the southern end of the Cumbre Vieja. El Hierro — 'The edge of the world'. It is also known as the Meridian Island. Cities[ edit ] Las Palmas — the largest city, situated on Gran Canaria and one of the capitals of the Canary Islands Santa Cruz de Tenerife — another capital of the Canary Islands, situated on Tenerife Demographics[ edit ] The islands have a population of 2 million. Since the Canary Islands are a major European tourist destination, all the major islands have well-developed communication systems, airports, and ports. Ethnically the population is mostly a mix of Spanish, European (German and British), South American, and especially Cuban and Venezuelan as well as Northern and Sub-Sahara African. There are also historical minorities such as Indians, Koreans and lately Russians.

Pico del Teide (on Tenerife) at 3718 metres above sea level is the highest point in both the Canary Islands and Spanish territory. Each island speaks with a slightly different accent and there is a strong rivalry between the main islands of Tenerife and Gran Canaria. Most of the accents in the Canary Islands are closer to Latin American Spanish than to Castililan Spanish spoken in continental Spain. The Canary Islands are very modern, very European, and extremely liberal. History[ edit ] Ancient legend claims the Canary Islands are the ‘lost islands’ of Atlantis. They have also been referred to as the lands without sorrow, holding on to the edge of the world. The first settlers were from North Africa. Known as Phoenicians, they arrived in the 10th century B.C. The main economic system was built around agriculture and animal farming. During the 14th century, the Islands were continuously invaded by different European countries. By plane[ edit ] The Canaries is a popular destination with Europeans, and swarms of charter and discount flights descend on the island year round.

The two airports (North/TFN & South/TFS) on Tenerife and the Gran Canaria Airport (LPA) are the busiest, but it's also possible to fly to many of the other islands, albeit it's often more expensive. By train[ edit ] A tram linking Santa Cruz bus station and La Laguna opened in 2007 costing €2.35 return in about 40 minutes. There are also tentative plans for a train linking Santa Cruz and Los Cristianos. By bus[ edit ] Buses are the most common method of public transportation around the islands. Mile per mile they are expensive while compared to mainland Spain but you are not going to travel really far away. We are, after all, islands. Most buses in touristic routes are adequate. Do not expect the drivers to know more than a couple of sentences in English or German, though they would try to be helpful. By taxi[ edit ] Taxis can be expensive, and inside a city they are not worth the money unless you are in a real hurry or cannot balance yourself after a shopping day.

By ship[ edit ] If you want to travel between the islands a good option might be to take a ship if you are in any particular hurry, specially between close by islands. Most ferries are now quite modern and cheap. The most important companies are Fred Olsen , Transmediterránea and Armas . By plane[ edit ] If you are afraid of the sea, or get sick just by staring at a ship, then a plane is what you need, and that usually means a turboprop ATR-72 or ATR-42 by one of the airlines like Binter or Canaryfly. They are perfectly safe and adequately fast as you are likely to spend more time at the airport than in the plane itself. Do[ edit ] Lanzarote: There is a bustling nightlife in four main resorts... Arrecife, Costa Teguise, Puerto del Carmen and Playa Blanca. Gran Canaria: The main resorts on the Island are Las Palmas, Maspalomas,Puerto Rico and Playa del Ingles. Tenerife: The main resorts are Santa Cruz, Puerto de la Cruz, and Playa de las Americas.

Fuerteventura: The main resorts of Fuerteventura are Corralejo, Caleta de Fuste and Morro Jable. Tenerife Auditorium: The Tenerife Auditorium is an incredible building designed by the famous Spanish architect Santiago Calatrava. It is highly recommended to tourists to visit this incredible structure and even to enjoy any of the concerts and events held in it. Loro Parque: The amazing Loro Parque (Parrot Pak) will surely fascinate you no matter your age. A visit to the park can take you nearly a whole day, so reserve some time for it. The park which was originally devoted to parrots shows has now grown into Tenerife's second biggest attraction after mount Teide.

The Loro parque is home to the world’s most important Parrot collection with over 300 species, an amazing seal show, Dolphin Show, Parrot Show, Aquarium with Shark tunnel, Gorillas, Chimpanzees, Tigers, Jaguars, Flamingos, Alligators, Tortoises, Orchid House, Gambian Market, a 'NaturaVision' Cinema and the worlds largest Penguinarium with a reproduction Antarctic climate within which 12 tons of snow falls a day. Puerto de la Cruz Puerto de la Cruz is one of the top resorts in the Canary Islands. It is also the longest established most complete of all resorts on Tenerife. The old part of the town keeps beautiful spots, one of the few places where the locals still work, eat and drink. Much of the area around the old fishing port is full of narrow cobbled streets packed with colonial architecture. British tourism arrived here over a century ago and today 'el Puerto' has a wide span of magnificent hotels to suit all tastes and budgets. In addition to its old world charms it offers some of the best visitor attractions in the islands.

Tenerife Beaches The volcanic nature of the island of Tenerife meant that the land has few natural beaches. Those that exist are characterised by black sand created from the island's volcanic rocks. The demand for tourist sun-bathing space, however, has led to the creation of resorts and man-made beaches, with golden sand having been imported in some cases. Some of the best beaches of Tenerife are Los Gigantes and San Juan in the west and Fañabe, in the South with its golden sand, showers and excellent facilities. Also popular are Torviscas with its marina, Playa las Americas for its grey sandy stretches and los Cristianos' beach. Candelaria in the east has a small black shingle beach. Up north Puerto de la Cruz has a beach with fine black sand, and at Santa Cruz golden sand has been imported for its Terasitas beach. Boat Trips from Tenerife A large number of companies offer boat trips for tourists, varying from a 'booze cruise' on a cruiser offering lunch, drinks and watersports to a trip around the island on a sailing boat or catamaran. One of the main attractions is the chance to see whales and dolphins in the wild.

Visitors on most trips spot whales; dolphins are not so much of a certainty but can be seen generally - often very close to the boat. Trips go from either Puerto Colon in Playa de las Americas, or from the port at Los Cristianos and most operators offer a free bus service from the larger hotels in the main resorts. Big Game Fishing around Tenerife The Canary Islands are one of the best spots in the world for big game fishing and a number of companies offer fishing trips in Tenerife. While blue marlin are the most highly prized trophy fish there are plenty of other species including white marlin, wahoo, dorado, yellowfin tuna, and mako and hammerhead sharks. Regular catches of blue marlin range from 331 to 496 pounds (150 to 225kg) with last year's record standing at 794 pounds (360kg). Trips cost around €45 including all equipment, but excluding lunch. Exchange rates fluctuate. Current rates for these and other currencies are available from XE.com The euro (€)" is the currency of the Canaries.

Eat[ edit ] Papas Arrugadas with mojo verde Canarian cuisine is a mix between Spanish, Latin and African cultures. Most of Canarian cuisine is a variety of fresh vegetables, fruit and fish, generally light meals, more easy to digest in a warm climate. Meat is usually consumed as a part of stews or as steaks. The local fish is quite good. You will find a wide variety of international recipes of fish and seafood, too. Two popular fish dishes from Tenerife are Caldereta, a meal with tomatoes, goat meat and potatoes and the Sancocho Canario, a salted fish, usually white, in a “mojo” sauce. The Tapas concept is one of the most delicious Spanish contributions to international gastronomy. A Tapa is a light and small piece of food that Spaniards have either before lunch or dinner, usually with a glass of wine or beer. The Tapa can be presented in several ways. It can be made as a pincho (with a stick), as a mini-dish of a traditional recipe, as a canapé, etc... The Canary Islands are Europe's only exporter of plantain bananas. They are famously delicious here.

These bananas are usually fried and are also commonly found in the West Indies. Papas Arrugadas or papa sancochada - Potatoes boiled in very salty water until they are "wrinkly" -- hence the name -- and served with mojo picón, a spicy cold red sauce made with chili and garlic. These are often served as a tapa. Gofio - Grain flour used especially at breakfast or to accompany potaje, a local stew. Conejo en salmorejo Gran Canaria of the Canary Islands | Globerovers Magazine Home » Featured Articles » Gran Canaria of the Canary Islands Gran Canaria of the Canary Islands Sun, Sea, Beaches, Sand Dunes, and Spanish Culture Posted on January 3, 2016 Located on an archipelago of the North Atlantic Ocean just 110 km off the west coast of Morocco, the Canary Islands (Islas Canarias)are geographically part of Africa, politically part of Spain, but notably more Spanish than African. Alas, during the high season of the European holidays, these islands are more European than Spanish. Most of the islands are quite rugged as they are of volcanic origin and mostly originate from fissure vents.

Geologists reckon that much of the islands were formed during the Miocene period between 14 and 9 million years ago. This period was followed by one of erosion, which lasted some 4 million years. Playa del Ingles, Gran Canaria Island From the oldest to the youngest, the islands are Lanzarote, Fuerteventura, Gran Canaria, Tenerife, La Gomera, La Palma and El Hierro. In fact, La Palma and El Hierro, the youngest of the island chain, are still above the oceanic hot spot of slow-moving, thick oceanic plates and thus still in their shield building phase. Many more recent volcanic activities have reshaped, expanded and destroyed the islands. For example, at El Hierro island intense earthquake activity since July 2011 resulted in a new submarine eruption which started on October 2011 at a vent just off the southern tip of the island. Playa del Ingles, Gran Canaria Island The larger and more popular islands such as Tenerife, Gran Canaria, Fuerteventura, and Lanzarote are best avoided during the peak holidays such as August, December, and January when the European vacationers invade them.

The islands of Tenerife and Gran Canaria are the liveliest tourist resort areas while the remaining islands are markedly quiet. With a sub-tropical climate regulated by the Gulf Stream and the Trade Winds, the weather is all-year good and it is no wonder that the Canaries are referred to as “The Land of Eternal Spring”. Temperatures are very moderate and rarely fall below 18°C in the winter or rise above 25°C in summer. The islands are all very unique in their own way and may have different appeals to different people. The most visible landmark on the island of Tenerife is Mount Teide (3,718 m) which is the third highest volcano in the world (after Mauna Loa and Mauna Kea in Hawaii). Lanzarote Island offers some of the most extraordinary volcanic landscapes on the planet with fields of petrified lava and beaches of black volcanic sand. Fuerteventura Island has the longest beaches in the archipelago and is a great place to explore the rugged nature.

La Playa de Mogan, Gran Canaria Island La Palma Island (San Miguel de La Palma) is the most volcanically active of the Canary Islands and offers the impressive Taburiente crater and fewer tourists. Gran Canaria Island is fairly large (1,560 km2) and is the second most populous of the Canary Islands. While it can get quite crowded with tourists during the high and peak seasons, the island is big and there are many places to avoid the tourists, who tend to mainly congregate around the beach areas of the “tourist towns”. Founded in 1478, the main city on Gran Canaria is Palmas de Gran Canaria (or just Las Palmas) and is located in the northeast of the island. Many tourists don’t care to visit the city as they head straight from the airport to the southern beaches. However, the city is certainly worth a few days if you are interested in the local culture and history rather than just the sun, sea, and tourist activities in the south. Las Palmas has a very local flavour and if you speak Spanish, you will easily make friends with the locals as you sit on the boardwalk watching the sunset over the Atlantic.

The city is blessed with many colonial buildings and colourful neighbourhoods abound. Many restaurants serve up Spanish and other dishes. Indulge in the tapas such as Salpicon de mariscos, Carne con papas, and Ropa Vieja while sipping on some of the popular Spanish beers such as Dorado, Tropical and San Miguel. The islands’ centuries-old wine industry has enjoyed unprecedented attention in the past few years. At a latitude of roughly 28°N the Canary Islands is the most tropical of Europe’s wine regions. La Playa de Mogan, Gran Canaria Island The Canary Islands have been known for the famed sweet Malmsey wine, made from the Malvasia grape which is also grown in California’s Central Coast, the Balkans, Croatia, Slovenia, Portugal, Italy and Spain. Malmsey wine is very popular with the English, Dutch and Germans, but today a wide range of indigenous grapes is grown. International varieties such as Malmsey are largely absent, yet not extinct. While the local wines are good, the most popular drink in Gran Canaria is the rum from the town of Arucas.

Arucas is a district to the east of Las Palmas and offers important agricultural, architectural and urban assets to the Canaries. In addition, the Arehucas Rum Distillery was established here in 1884 by Alfonso Gourié as the “Sugar Factory San Pedro” and has since then made the most popular rum in this part of the world. Reputedly being the oldest rum factory and cellar in Europe, it distributes about 80% of its annual production of 4 million litres across the Canary Islands. La Playa de Mogan, Gran Canaria Island In addition to its popular drink, Arehucas Rum, the Arehucas Rum Distillery also makes a wide range of spirits including rum honey and banana cream liqueurs such as Crème de Banana and Côctel de Plátano Banadrink. Las Palmas town, Gran Canaria Island Among the best rums are Carta Oro, Carta Blanca, the 7-year old oak barrel matured Arehucas, 12-year old Reserva Espcial, Ron Carmelo and the Ron Miel Guanche honey rum.

At the top is the 30 year old oak matured Captain Kidd Rum which sells at over US$200 per bottle. After a few days of soaking up the culture in Las Palmas, take a bus to Maspalomas in the far south of the island. There are many tourist hotels and home stays in the town known for its vibrant night life, long stretches of beach, and the massive sand dunes known as Maspalomas Dunes. For all-inclusive package tours, the accommodation stretches up along the south western part of the island towards the little town of Playa de Mogán. Even if you don’t stay along this stretch of tourist havens, take a day trip by local bus from Maspalomas and hop off at whichever location attracts your fancy. Playa de Mogán, at the furthest end of this coastal road, is a pretty little village which has some local culture to be savoured. Many restaurants are located along the beach. From here you can also travel by local ferry along the coast to other towns towards Maspalomas. Another site which will require private transportation such as a 4-wheel vehicle, is Bandama Caldera near the town of Tafira.

At a height of 570 m above sea level the caldera is for the more adventurous and if fit enough you can descend on foot. The steep walk to the bottom of the caldera takes about half an hour. Volcanic ash of different hues is in great abundance around the caldera. En route to the caldera stop at the small town of Teror which is right at the centre of the island and is reached via a steep winding road. The town is characterised by typical buildings, balconies and rural island life. Enjoy the sunny Canaries! Canary Islands Figure 5: Genetic evolution of the Canary Islands from Miocene to present (Carracedo, 1999). Figure 6: Formation stages of volcanic islands associated with “hot spots” (modified from Walker, 1990). Figure 7: Basaltic pillow lavas of the submarine stage from La Palma island (Barranco Las Angustias). Figure 8: Basaltic lava flows of the shield-building stage from Gran Canaria (the cliffs of Güigüi).

Figure 9: Unconformity between a trachy-phonolitic cone sheet of the declining stage and horizontal volcanic rocks of the rejuvenation stage from Gran Canaria (Barranco de Tejeda). Figure 10: Line of strombolian cones in Timanfaya National Park associated with the rejuvenation stage of Lanzarote. The successive stages are commonly separated from each other by time gaps several million years long and there are sometimes time gaps withing a single stage. In addition, the landscape of the Canaries is characterized by collapse structures – vertical collapse calderas (such as the Caldera de Tejeda in Gran Canaria), gravitational collapse scarps and embayments (Figure 11) such as El Golfo, Julán y Las Playas and El Hierro (Figure 12) and rift zones (Figure 13), locally known as “dorsales” (such as the Cumbre Vieja volcano in La Palma). Figure 11: Debris avalanches, debris flows and slumps in the Canaries zone (M. Canals, 2003). Click on image for enlargement.

Figure 12: Giant landslides of El Hierro (M. Canals, 2003). Figure 13: Aerial view of the southern part of La Palma and Cumbre Nueva rift (Photo: S. Socorro).

The Canaries also show some interesting differences with the Hawaii Islands, however: the geochemical evolution of their magmas (alkaline suite), the formation of central stratovolcanoes (Roque Nublo in Gran Canaria and Teide in Tenerife (Figure 14), the island tectonics, e.g., ductile shears associated with transtensive systems (Fernandez et al., 1997; Figure 15), compressional structures such as recumbent folds (Robertson & Stillman, 1979), blocks differentially uplifted from the sea floor – 2 km for La Palma and 2 – 4 km for Fuerteventura, and tectonic lineaments with different azimuths in each island, and the small or zero subsidence – in several islands there are marine structures and deposits of different ages up to several million years old that appear to have remained close to present-day sea level. Figure 14: Northwest littoral area of Tenerife and view of the Teide stratovolcano. Figure 15: Shear zone associated with the submarine stage of Fuerteventura (Caleta de la Cruz, west coast).

Carbonatites, syenites and gabbros are deformed and intruded by later basaltic dykes. The volume and distribution of the volcanoes provides interesting information about the evolution of the archipelago. The islands rest on an oceanic floor that deepens progressively westward, reaching a depth of 4,000 m in the area of La Palma and El Hierro (Figure 16A). Shaded relief images (Figure 16B), which give an empty ocean view of the Canarian chain, clearly show that the elevation and emerged volume of the islands increase as their age decreases, with a generally westward trend. The islands of Fuerteventura and Lanzarote, and the chain of seamounts off Cape Juby, are parallel to the continental margin, whereas most of the remaining islands of the archipelago follow a general east-west trend. Figure 16: Shaded relief view of the Canary Islands from the east (A) and east-west cross-section (B) (from Carracedo et al., 2002). The dual line of La Palma and El Hierro forms a north-south trend and are thought to be associated with changes in plate motion.

In addition, Rihm et al. (1998) demonstrate the presence of a group of apparently young seamounts (the Las Hijas seamounts) located 70 km SE of El Hierro, perhaps destined to become the next Canarian islands. The rock types in the Canary Islands are diverse and include melilitites, nephelinites, basanites, tholeiitic and alkali basalts, tephrites, rhyiodacites, rhyolites, pantellerites, comendites, trachytes, phonolites and carbonatites. In other words, they comprise a typical oceanic alkaline suite with saturated and undersaturated end members. Most basalts are alkaline in the shield-building stages, trachytes and phonolites are very common in the declining stages, while the rejuvenation stages produced essentially basanites and nephelinites. Total alkali vs. silica (TAS) diagrams of volcanic rocks from the Canary Islands (Figure 17) show that they fall in the alkaline, silica-undersaturated field. There is a generally bimodal grouping into basalt-basanite and trachyte-phonolite compositions.

Figure 17 also shows that most samples correspond to moderately alkaline (alkali basalt-trachyte) or highly alkaline (basanite-phonolite) rocks. Figure 17: Total alkali versus silica diagrams (TAS) with analyses of Canaries volcanic rocks (Carracedo et al., 2002). Rocks of tholeiitic affinity have been recognized only in the oldest units of Gran Canaria and in the most recent lavas of Lanzarote. Ultra-alkaline rocks appear mainly in Gran Canaria (ol-melilitites and nephelinites) and Fuerteventura (ol-nephelinites), corresponding to the rejuvenation stage. There are notable differences in the alkalinity and abundance of rock types between the islands. Gran Canaria has rocks embracing all compositions from the most to the least alkaline, whereas in the other islands the alkalinity of lava flows is mostly homogeneous. The most alkaline is La Palma, whereas Tenerife is less so, being on the boundary between highly and moderately alkaline.

El Hierro, La Gomera, Fuerteventura and Lanzarote show the least overall alkalinity – all are moderately alkaline. The islands with the least abundance of felsic rocks (< 1%) are Lanzarote and El Hierro, with ~ 3% on La Palma, La Gomera and Fuerteventura, and the central islands (Gran Canaria and Tenerife) having the largest abundance (>10%). Mg variation diagrams of Canarian rocks show similar trends in all the islands (Figure 18), with decreasing MgO in basic rocks (basalts, basanites; < 6%) and the trachytic-phonolitic rocks (MgO < 1%). Both CaO and FeO decrease slightly, while Al2O3 rises considerably and TiO2 has a tendency to increase slightly. Trace-element data show the most incompatible elements increasing from the basalts to the trachybasalts and basaltic trachyandesites, with a reduction in Ti and P, possibly due to Fe-Ti oxides and apatite crystallization (Figure 19).

The trace- and radiogenic-isotope contents are characteristic of HIMU OIBs, although with some variations depending on the age of the various units (Weaver, 1991; Hoernle et al., 1991; Thirwall et al., 1997). Figure 18: Plots of MgO vs. major oxides from Canary Islands volcanic rocks (Carracedo et al., 2002). Figure 19: Plots of incompatible trace elements normalized to primitive mantle (Carracedo et al., 2002). Sr-Nd-Pb isotopic analyses have been interpreted as indicating that the magmas of the Canary Islands represent a multicomponent mixture of different reservoirs – a HIMU component and a second end-member with lithospheric (EM), asthenospheric (DM) and additional HIMU components (Cousens et al., 1990; Hoernle & Tilton, 1991; Hoernle et al., 1991; Hoernle & Schmincke, 1993; Neuman et al., 1995).

Summary The Canary archipelago developed at a passive continental margin, on Jurassic oceanic lithosphere and a slow-moving tectonic plate. There are several genetic hypotheses for the Canary Islands, including a propagating fracture, a local extensional ridge, uplifted tectonic blocks and an unifying model but it is generally assumed that the archipelago originated from residual old plume material in the upper mantle. The first alkaline magmatic manifestations of this hot spot occurred at Fuerteventura during the Upper Cretaceous (~ 70 Ma), submarine volcanism started in the Eocene-Oligocene (~ 39 Ma) and subaerial volcanism in the Miocene (~ 20.6 Ma). There is a general progression of the oldest volcanism, thought to be induced by westward motion of the African plate and thus El Hierro island has the oldest dated subaerial Quaternary (~ 1.1 Ma) volcanism. The chain has been active along its entire length during the last million years, however. Canary Island volcanism involves submarine stages, followed by shield-building, declining, erosive and rejuvenation stages.

Three groups of islands are currently in the rejuvenation stage – Fuerteventura, Lanzarote, Gran Canaria and Tenerife. La Gomera is in the erosional stage, and La Palma and El Hierro are in the declining stage. The Canary Islands show some interesting differences with other oceanic islands such as the formation of central stratovolcanoes, island tectonics that include ductile shears and compressional structures, and small or zero subsidence. For more information about the geology of the Canary Islands, see: Carracedo, J.C., Pérez, F.J., Ancochea, E., Meco J., Hernán, F., Cubas C.R., Casillas, R., Rodriguez, E. and Ahijado, A., 2002. Cenozoic volcanism II: The Canary Islands. In: The Geology of Spain. Ed. Gibbons, W. and Moreno, T., Geological Society of London, 439-472. References Anguita, F. and Hernán, F., 1975. A propagating fracture model versus a hot spot origin for the Canary Islands. Earth Planet.

Sc. Lett., 27, 11-19. Anguita F. and Hernán, F., 2000. The Canary Islands origin: a unifying model. J. Volcanol. Geotherm. Res., 103, 1-26. Araña V. and Ortiz, R., 1986. Marco geodinámico del volcanismo canario. An. Física, 82, 202-231. Balogh, K., Ahijado, A., Casillas, R. and Fernández, C., 1999. Contribution to the chronology of the Basal Complex of Fuerteventura, Canary Islands. J. Volcanol. Geotherm. Res., 90, 81-101 Canas, J.A., Ugalde, A., Pujades, L.G., Carracedo, J.C., Soler, V. and Blanco, M.J., 1998. Intrinsic and scattering seismic wave attenuation in the Canary Islands. J. Geophys.

Res., 103, 15,037-15,050. Canales, J.P. and Dañobeitia, J., 1998. The Canary Islands swell: a coherence analysis of bathymetry and gravity. Geophys. J. Int., 132, 479-488. Cantagrel, J.M., Fuster, J.M., Pin, C., Renaud U., and Ibarrola, E., 1993. Age Miocene inferieur des carbonatites de Fuerteventure (23 Ma:U-Pb zircon) et le magmatisme précoce d´une ile océanique (Iles Canaries). C.R. Acad. Sci. Paris, 316, 1147-1153. Carracedo, J.C., Day, S., Guillou, H., Rodríguez Badiola, E., Canas J.A., and Pérez Torrado, F.J., 1998. Hotspot volcanism close to a passive continental margin: the Canary Islands. Geol.

Mag., 135, 591-604. Carracedo, J.C., Pérez, F.J.; Ancochea, E.; Meco J.; Hernán, F.; Cubas C.R.; Casillas, R.; Rodriguez, E; Ahijado, A. 2002. Cenozoic volcanism II: The Canary Islands. In: The Geology of Spain. Ed. By Gibbons, W. and Moreno, T., The Geological Society of London, 439-472. Cousens, B.L., Sphera, F.J. and Tilton, G.R., 1990. Isotopic patterns in silicic ignimbrites and lava flows of the Mogan and lower Fataga Formations, Gran Canaria, Canary Islands: Temporal changes in mantle source composition. Earth Planet. Sci. Lett., 96, 319-335. Fernández, C., Casillas, R., Ahijado, A., Perelló, V., and Hernández Pacheco, A., 1997.

Shear zones as a result of intraplate tectonics in oceanic crust: the example of the Basal Complex of Fuerteventura (Canary Islands). J. Struct. Geol., 19, 41-57. Fuster, J.M., 1975. Las Islas Canarias: un ejemplo de evolución temporal y espacial del vulcanismo oceánico. Est. Geol., 31, 439-463. Hoernle K., and Tilton G., 1991. Sr-Nd-Pb isotope data for Fuerteventura (Canary Islands) basal complex and subaerial volcanics: application to magma genesis and evolution. Schweiz. Mineral. Petrogra. Mitt., 71, 3-18. Hoernle, K. and Schmincke, H.U., 1993. The role of partial melting in the 15-Ma geochemical evolution of Gran Canaria: A blob model for the Canarian hotspot. J. Pet., 34, 599-626.

Hoernle K., Tilton G., and Schmincke H. U. 1991. Sr-Nd-Pb isotopic evolution of Gran Canaria: Evidence for shallow enriched mantle beneath the Canary Islands. Earth Planet. Sci. Lett., 106, 44-63. Hoernle, K., Zhang, Y.S., and Schmincke, H.U., 1995. Seismic and geochemical evidence for large-scale mantle upwelling beneath the eastern Atlantic and western and central Europe. Nature, 374, 34-39. Hollik, J.S., Rabinowitz, P.D., and Austin, J.A. 1991. Effects of Canary hot spot volcanism on structure of oceanic crust off Morocco. J. Geophys. Res., 96, 12,039-12,067. Le Bas, M.J., Rex D.C, and Stillman, C.J., 1986. The Early magmatic chronology of Fuerteventura, Canary Islands. Geol. Mag., 123, 287-298.

Neumann, E.-R., Wulff-Pedersen, E., Johnesen, K., Andersen, T., Drogh, E. 1995. Petrogenesis of spinel harzburgite and dunite suite xenoliths from Lanzarote, eastern Canary Islands: Implications for the upper mantle. Lithos, 35, 83-107. Oyarzun, R., Doblas, M., López-Ruiz, J., and Cebriá, J.M., 1997. Opening of the central Atlantic and asymmetric mantle upwelling phenomena: Implications for long-lived magmatism in western North-Africa and Europe. Geology, 25, 727-730. Rihm, R., Jacobs, L., Krastel, S., Schmincke, H.U. and Alibés, B., 1998. Las Hijas Seamounts. The next Canary Islands? Terra Nova, 10, 121-125. Robertson, A.H.F. and Stillman, C.J., 1979.

Submarine volcanic and associated sedimentary rocks of the Fuerteventura Basal Complex, Canary Islands. Geol. Mag., 116, 203-214. Roest, W.R., Dañobeitia, J.J., Verhoef, J., and Collette, B.J., 1992. Magnetic anomalies in the Canary Basin and the Mesozoic evolution of the Central North Atlantic. Mar. Geophys. Res., 14, 1-24. Schmincke H. U., 1973. Magmatic evolution and tectonic regime in the Canary, Madeira and Azores Island groups. Geol. Soc. Am. Bull., 84, 633-648. Staudigel H., Feraud G., and Giannerini G., 1986. The history of intrusive activity of the island of La Palma (Canary Islands). J. Volcanol. Geotherm. Res., 27, 299-322. Steiner, C., Hobson, A., Favre, P.

and Stampli, G.M., 1998. Early Jurassic sea-floor spreading in the central Atlantic – The Jurassic sequence of Fuerteventura (Canary Islands). Geol. Soc. Am. Bull., 110, 1304-1317. Thirwall, M.F., Jenkins, C., Vroon, P.C. and Mattey. D.P., 1997. Crustal interaction during construction of oceanic islands: Pb-Sr-Nd-O isotope geochemistry of the shield basalts of Gran Canaria, Canary Islands. Chem. Geol., 135, 233-262. Urgeles, R. (2000): Esllavissaments gegants a les illes Canàries, les Illes d'El Hierro i La Palma . Ed. Universidad de Barcelona. Servicio de Información y Publicaciones. Col.Tesis doctorals microfitxades, 3707. ISBN: 84-475-2353-5. Walker, G.P.L., 1990.

Geology and volcanology of the Hawaiian Islands. Pacific Sc., 44, 315-347. Weaver, P.P.E., 1991. The origin of ocean island basalt end-member composition: Trace-element and isotopic constraints. Earth Planet. Sci. Lett., 104, 381-397. last updated December 21st, 2007 Fuerteventura - Boat Trip Boat Trip Boat trip finder in Spain Language: Home » Canary Islands » Fuerteventura Fuerteventura Fuerteventura can be loosely translated as ‘Strong Winds’ or a corruption of French Forte Aventure (‘Great Adventure’) is one of theCanary Islands, in the Atlantic Ocean off the coast of Africa, politically part of Spain. At 1,660 square kilometres (641 sq mi) it is the second largest of the Canary Islands, after Tenerife. It was declared a biosphere reserve by UNESCO on 26 May 2009. Fuerteventura is the oldest island in the Canary Islands dating back 20 million years to a volcanic eruption from the Canary hotspot.

The majority of the island was created about 5 million years ago and since then has been eroded by wind and weather. On the seabed off the west coast of the island rests a block of rock 22 km (14 mi) long and 11 km (7 mi) wide, which appears to have slid off the island largely intact at some point in prehistory, similar to the predicted future collapse of Cumbre Vieja, a geological fault on the neighboring island, La Palma. The last volcanic activity in Fuerteventura was between 4,000 and 5,000 years ago. The highest point in Fuerteventura is Mount Jandía (807 m) in the southwestern part of the island. Geographical features include Istmo de la Pared which is 5 km (3 mi) wide and is the narrowest part of Fuerteventura. The island is divided into two parts, the northern portion which is Maxorata and the southwestern part called the Jandía peninsula. 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 28 °C (82 °F) and a low of 20 °C (68 °F) can be expected. Precipitation is about 147 mm (6 in) per year, most of which falls in autumn and winter. October is the month with highest rainfall. A sandstorm known as the Calima (similar to the Scirocco wind that blows North from the Sahara into Europe) blows southwestward 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 African locusts to the island. Canary Islands mappa Map – Gran Canaria, Lanzarote, Fuerteventura, Tenerife, La Gomera, La Palma, El Hierro – Mappa Canary Islands mappa Map – Gran Canaria, Lanzarote, Fuerteventura, Tenerife, La Gomera, La Palma, El Hierro Posted on by admin The Canary Islands (Spanish: Islas Canarias) are an Atlantic territory of Spain on the west coast of Africa, near Morocco, Cape Verde and the archipelagos of the Azores Islands and Madeira Islands, both Portuguese territories. The following islands make up the Canary chain and are covered in the mappa map: Gran Canaria — The largest island by population, capital city Las Palmas de Gran Canaria. Green and steep in the north, dry and flat in the south. Fuerteventura — windsurfer’s mecca.

Lanzarote — Low lying and arid, with a spectacular volcanic landscape in the west of the island (National Park of Timanfaya). The capital is Arrecife and has its own airport (ACE). Lanzarote is also of volcanic origin. Tenerife — The island of Tenerife has many museums and monuments that serve as portrayals of its rich history. The highest mountain of Spain, El Teide and 3rd largest volcano in the world. The capital is Santa Cruz de Tenerife. The title of capital city is shared with San Cristóbal de La Laguna. La Gomera — The Magic Isle – walker’s paradise. It is shaped like an orange that has been cut in half and split into segments. The local people have a unique way of communicating across deep ravines by using a whistled speech called Silbo Gomero. This whistled language is indigenous to the island, and its existence has been documented since Roman times. La Palma — The capital is Santa Cruz de la Palma. The southern part of La Palma is dominated by the Cumbre Vieja, a volcanic ridge. El Hierro — ‘The edge of the world’.

It is also known as the Meridian Island. The two airports (North/TFN & South/TFS) on Tenerife and the Gran Canaria Airport (LPA) are the busiest, but it’s also possible to fly to many of the other islands – all are covered on the mappa map. Screenshots Holiday rentals - Canary islands, Tenerife, Gran Canaria, Fuerteventura, La Palma, Lanzarote All Canary Islands rentals Happily Lost in the Canary Islands Search for holiday rentals in The Canary Islands consists of 9 islands and a handful of islets. There are 7 major islands: El Hierro, Fuerteventura, Gran Canaria, La Gomera, La Palma, Lanzarote and Tenerife. The 2 minor islands are La Graciosa and Lobos. Geographically, the archipelago is a part of the African continent but the group of islands is under Spanish administration. The Las Palmas de Gran Canaria is the capital of the whole archipelago and is one of Spainâs major cities. Located on the island of Gran Canaria, Las Palmas combines a cosmopolitan and beach lifestyle effortlessly.

The city offers shopping, bars, and a multitude ofrestaurants. The city knows how to celebrate Las Palmas style with spectacular carnivals and the WOMAD music festival. The historic center and a handful of museums make this city a well-balanced playground. Tenerife is the biggest of the major islands and is strangely left out by American tourists when they visit. The islandâs center of attraction is the Pico del Teide and a cable lift is ready to take visitors to the highest point of the archipelago. The word ethereal comes to mind with a close view of the majestic volcano and the rest of the island. Fuerteventura

Question: Tenerife, La Palma, and Fuerteventura are part of what Spanish island chain?
Answer: Canary Islands