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Peñas Del Chache
Peñas del Chache is the highest altitude of the island of Lanzarote, Canary Islands, Spain, with a height of 672 meters above sea level. It is located in the north of the island, in the municipality of Haría (municipality), Haría. Toponymy The term Chache is of probably of Guanche language, Guanche origin. As for its possible meaning, the philologist Maximiano Trapero has proposed its translation as 'the height'. Characteristics Peñas del Chache is a rocky mountain located in the Famara massif. The top is occupied by an installation of the Air Surveillance Squadron. Geology Peñas del Chache is a basaltic intrusive formation dating from the Miocene period, and is part of the Famara volcanic edifice, one of the oldest massifs on the island. Vegetation The surroundings of the Peñas del Chache were characterized by thickets of the Canarian thermophilic forest in the past. However, historical human activity has caused its near disappearance, finding itself dominated by substitu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spanish Air Force
The Spanish Air and Space Force () is the aerial and space warfare branch of the Spanish Armed Forces. History Early stages Hot air balloons have been used with military purposes in Spain as far back as 1896. In 1905, with the help of Alfredo Kindelán, Leonardo Torres Quevedo directed the construction of the first Spanish dirigible in the Army Military Aerostatics Service, created in 1896 and located in Guadalajara. The new airship was completed successfully in 1908 and, named 'Torres Quevedo', made numerous test and exhibition flights.Francisco A. González Redondo''Leonardo Torres Quevedo, 1902–1908. The Foundations for 100 years of Airship designs''In book: Proceedings of the 7th International Airship Convention, pp.1–12, Publisher: German Society for Aeronautics and Astronautics (DGLR), October 2008. The Spanish Army's air arm, however, took off formally in 1909 when Colonel Pedro Vives Vich and Captain Alfredo Kindelán made an official trip to different Euro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haría (municipality)
Haría is a Municipalities of Spain, municipality on the island of Lanzarote in the Canary Islands, the northernmost and easternmost Canarian municipality. Surrounded on three sides by the Atlantic Ocean, the municipality is bordered to the south by the municipality of Teguise, Las Palmas, Teguise. It forms part of Las Palmas Province. The seat of the municipality is the town of Haría (village), Haría. The population of the municipality was 4,872 in 2013.Instituto Canario de Estadística , population The total land area of the municipality is . Geography The west of the municipality is largely mountainous, with much of the western coastline rising steeply a little way inland. Numerous ''miradors'' (viewpoints) on this high ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lanzarote
Lanzarote (, , ) is a Spanish island, the easternmost of the Canary Islands, off the north coast of Africa and from the Iberian Peninsula. Covering , Lanzarote is the fourth-largest of the islands in the archipelago. With 163,230 inhabitants at the beginning of 2024, it is the third most populous Canary Island, after Tenerife and Gran Canaria. Located in the centre-west of the island is Timanfaya National Park, one of its main attractions. The island was declared a biosphere reserve by UNESCO in 1993. The island's capital is Arrecife, which lies on the eastern coastline. It is the smaller main island of the Province of Las Palmas. The first recorded name for the island, given by Italian-Majorcan cartographer Angelino Dulcert, was ''Insula de Lanzarotus Marocelus'', after the Genoa, Genoese navigator Lancelotto Malocello, from which the modern name is derived. The island's name in the native Guanche language was ''Tyterogaka'' or ''Tytheroygaka'', which may mean "one that ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canary Islands
The Canary Islands (; ) or Canaries are an archipelago in the Atlantic Ocean and the southernmost Autonomous communities of Spain, Autonomous Community of Spain. They are located in the northwest of Africa, with the closest point to the continent being 100 kilometres (62 miles) away. The islands have a population of 2.25 million people and are the most populous overseas Special member state territories and the European Union, special territory of the European Union. The seven main islands are from largest to smallest in area, Tenerife, Fuerteventura, Gran Canaria, Lanzarote, La Palma, La Gomera, and El Hierro. The only other populated island is Graciosa, Canary Islands, La Graciosa, which administratively is dependent on Lanzarote. The archipelago includes many smaller islands and islets, including Alegranza, Islote de Lobos, Isla de Lobos, Montaña Clara, Roque del Oeste, and Roque del Este. It includes a number of rocks, including Roque de Garachico, Garachico and Roques de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcano
A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high to intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less viscous mafic magma. Extensive felsic lava flows are uncommon, but can travel as far as 8 km (5 mi). The term ''composite volcano'' is used because strata are usually mixed and uneven instead of neat layers. They are among the most common types of volcanoes; more than 700 stratovolcanoes have erupted lava during the Holocene Epoch (the last 11,700 years), and many ol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guanche Language
Guanche is an extinct language or dialect continuum that was spoken by the Guanches of the Canary Islands until the 16th or 17th century. It died out after the conquest of the Canary Islands as the Guanche ethnic group was assimilated into the dominant Spanish culture. The Guanche language is known today through sentences and individual words that were recorded by early geographers, as well as through several place-names and some Guanche words that were retained in the Canary Islanders' Spanish. Classification Guanche has not been classified with any certainty. Many linguists propose that Guanche was likely a Berber language, or at least genealogically related to the Berber languages to some extent as an Afroasiatic language. However, recognizable Berber words are primarily agricultural or livestock vocabulary, whereas no Berber grammatical inflections have been identified, and there is a large stock of vocabulary that does not bear any resemblance to Berber whatsoever. It ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Famara
Famara is the main mountainous massif in the north of the island of Lanzarote in the Canary Islands. It is the eastern slope of a volcano erupting in the Miocene. The cliffs of Famara (''Risco de Famara'') are the remains of a caldera of about ten kilometres in diameter centred on the south of Graciosa, Canary Islands, La Graciosa. The cliffs of Famara peak at an altitude of 671 m at the Peñas del Chache. A village at the range's seaside is Caleta de Famara, part of Teguise (municipality), Teguise. Playa de Famara The beach south of the cliffs of Famara, the Playa de Famara, is one of sand and volcanic pebbles. It is two kilometres long. Its orientation towards the Atlantic Ocean makes it suitable for the practice of surfing. (fr) A popular seaside resort, Caleta de Famara, has been built here. It is part ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first epoch (geology), geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene followed the Oligocene and preceded the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by distinct global events but by regionally defined transitions from the warmer Oligocene to the cooler Pliocene Epoch. During the Early Miocene, Afro-Arabia collided with Eurasia, severing the connection between the Mediterranean and Indian Oceans, and allowing the interchange of fauna between Eurasia and Africa, including the dispersal of proboscideans and Ape, hominoids into Eurasia. During the late Miocene, the conn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Euphorbia Regis-jubae
''Euphorbia regis-jubae'' is a species of flowering plant in the family Euphorbiaceae, native to the eastern Canary Islands, western Morocco, north-western Western Sahara. The specific epithet honours the contributions of King Juba II to natural history and his role in bringing the genus to notice. In Spanish, it is known as . It has often been confused with '' Euphorbia lamarckii''. Description ''Euphorbia regis-jubae'' is a shrub, up to tall. It has light brown stems and terminal rosettes of leaves that are narrow and oblong, with a pointed or somewhat blunt apex. The inflorescences are pedunculate, umbel-like, usually simple with five to eight rays, more rarely compound. The greenish-yellow floral bracts are large, not joined at the base, and persist when the fruit has formed. The fruit capsules are light brown or red. The seeds have a stalked elaiosome (caruncle). File:Teguise - Camino de Teguise al las Nieves - Euphorbia regis-jubae 04 ies.jpg, Inflorescence File:Euphorb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Asteriscus Intermedius , a structure in the inner ear
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''Asteriscus'' may refer to: * ''Asteriscus'' (plant), a genus of flowering plants * Asteriscus, a component of the otolith An otolith (, ' ear + , ', a stone), also called otoconium, statolith, or statoconium, is a calcium carbonate structure in the saccule or utricle (ear), utricle of the inner ear, specifically in the vestibular system of vertebrates. The saccule ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lavandula Dentata
''Lavandula dentata'', the fringed lavender or French lavender, is a species of flowering plant in the family Lamiaceae, native to the Mediterranean basin, Eritrea, Ethiopia, Yemen, and the Arabian Peninsula. Growing to tall, it has gray-green, linear or lance-shaped leaves with toothed edges and a lightly woolly texture. The long-lasting, narrow spikes of purple flowers, topped with pale violet bracts, first appear in late spring. The whole plant is strongly aromatic with the typical lavender fragrance. Its native habitat includes low hills with limestone substrates amidst other shrubs. It is present on Madeira and the Canary Islands. One of several species known by the English common name French lavender (see also '' Lavandula stoechas''), it is commonly grown as an ornamental plant and its essential oil is used in perfumes. Like other lavenders, it is particularly associated with dry, sunny, well-drained conditions in alkaline soil. But it will tolerate a range of condition ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Canary Islands
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
