Elantxobe is a town and municipality located in the province of Biscay, in the autonomous community of Basque Country, northern Spain. ELANTXOBE in the Bernardo Estornés Lasa - Auñamendi Encyclopedia
Ferdinand II of Aragon
Ferdinand II, called the Catholic, was King of Aragon from 1479 until his death. His marriage in 1469 to Isabella, the future queen of Castile, was the marital and political "cornerstone in the foundation of the Spanish monarchy." As a consequence of his marriage to Isabella I, he was de jure uxoris King of Castile as Ferdinand V from 1474 until her death in 1504. At Isabella's death the crown of Castile passed to their daughter Joanna, by the terms of their prenuptial agreement and her last will and testament. Following the death of Joanna's husband Philip I of Spain, her alleged mental illness, Ferdinand was recognized as regent of Castile from 1508 until his own death. In 1504, after a war with France, he became King of Naples as Ferdinand III, reuniting Naples with Sicily permanently and for the first time since 1458. In 1512, he became King of Navarre by conquest. In 1506 he married Germaine of Foix of France, but Ferdinand's only son and child of that marriage died soon after birth. Ferdinand had a role in inaugurating the first European encounters in the future Americas, since he and Isabella sponsored the first voyage of Christopher Columbus, in 1492.
That year was the final victory in the war with Granada which defeated the last Muslim state in Iberia and all of Western Europe. This brought to a close the centuries-long Christian reconquest of Iberia. For that Christian victory, Pope Alexander VI, born in the Kingdom of Valencia, awarded the royal couple the title of Catholic Monarchs. At Ferdinand's death Joanna's son, Ferdinand's grandson, Charles I, co-ruler in name over all the several Iberian kingdoms except for Portugal, succeeded him, making Charles the first King of Spain. However, during the regency of Ferdinand, many called him the King of Spain as distinct from his daughter Joanna, "queen of Castile". Ferdinand was born in Sada Palace, Sos del Rey Católico, Kingdom of Aragon, as the son of John II of Aragon by his second wife, Juana Enríquez, he married Infanta Isabella, the half-sister and heiress of Henry IV of Castile, on 19 October 1469 in Valladolid, Kingdom of Castile and Leon. Isabella belonged to the royal House of Trastámara, the two were cousins by descent from John I of Castile.
They were married with a clear prenuptial agreement on sharing power, under the joint motto "tanto monta, monta tanto." He became jure uxoris King of Castile when Isabella succeeded her deceased brother in 1474 to be crowned as Queen Isabella I of Castile. The two young monarchs were obliged to fight a civil war against Joan of Castile, the purported daughter of Henry IV, were swiftly successful; when Ferdinand succeeded his father as King of Aragon in 1479, the Crown of Castile and the various territories of the Crown of Aragon were united in a personal union. The various states were not formally administered as a single unit, but as separate political units under the same Crown; the first years of Ferdinand and Isabella's joint rule saw the Spanish conquest of the Nasrid dynasty of the Emirate of Granada, the last Islamic al-Andalus entity on the Iberian peninsula, completed in 1492. The completion of the Reconquista was not the only significant act performed by Ferdinand and Isabella in that year.
In March 1492, the monarchs issued the Edict of Expulsion of the Jews called the Alhambra Decree, a document which ordered all Jews either to be baptised and convert to Christianity or to leave the country. It allowed Mudéjar Moors and converso Marrano Jews to stay, while expelling all unconverted Jews from Castile and Aragon. 1492 was the year in which the monarchs commissioned Christopher Columbus to find a westward maritime route for access to Asia, which resulted in the Spanish arrival in the Americas. In 1494 the Treaty of Tordesillas divided the entire world beyond Europe between Portugal and Castile for conquest and dominion purposes – by a north–south line drawn down the Atlantic Ocean. Ferdinand violated the 1491 Treaty of Granada peace treaty in 1502 by dismissing the guaranteed religious freedom for Mudéjar Muslims. Ferdinand forced all Muslims in Castile and Aragon to convert, converso Moriscos, to Catholicism, or else be expelled; some of the Muslims who remained were mudéjar artisans, who could design and build in the Moorish style.
This was practised by the Spanish inquisitors on the converso Marrano Jewish population of Spain. The main architect behind the Spanish Inquisition was King Ferdinand II. Ferdinand destroyed over ten thousand Arabic manuscripts in Granada alone; the latter part of Ferdinand's life was taken up with disputes with successive Kings of France over control of Italy, the so-called Italian Wars. In 1494, Charles VIII of France invaded Italy and expelled Alfonso II, Ferdinand's first cousin once removed and stepson of Ferdinand's sister, from the throne of Naples. Ferdinand allied with various Italian princes and with Emperor Maximilian I to expel the French by 1496 and install Alfonso's son, Ferdinand, on the Neapolitan throne. In 1501, following the death of Ferdinand II of Naples and accession of his uncle Frederick, Ferdinand signed an agreement with Charles VIII's successor, Louis XII, who had just asserted his claims to the Duchy of Milan, to partition Naples between them, w
An oceanic climate known as a marine climate or maritime climate, is the Köppen classification of climate typical of west coasts in higher middle latitudes of continents, features mild summers and mild winters, with a narrow annual temperature range and few extremes of temperature, with the exception for transitional areas to continental and highland climates. Oceanic climates are defined as having a monthly mean temperature below 22 °C in the warmest month, above 0 °C in the coldest month, it lacks a dry season, as precipitation is more evenly dispersed throughout the year. It is the predominant climate type across much of Western Europe including the United Kingdom, the Pacific Northwest region of the United States and Canada, portions of central Mexico, southwestern South America, southeastern Australia including Tasmania, New Zealand, as well as isolated locations elsewhere. Oceanic climates are characterised by a narrower annual range of temperatures than in other places at a comparable latitude, do not have the dry summers of Mediterranean climates or the hot summers of humid subtropical.
Oceanic climates are most dominant in Europe, where they spread much farther inland than in other continents. Oceanic climates can have considerable storm activity as they are located in the belt of the stormy westerlies. Many oceanic climates have frequent cloudy or overcast conditions due to the near constant storms and lows tracking over or near them; the annual range of temperatures is smaller than typical climates at these latitudes due to the constant stable marine air masses that pass through oceanic climates, which lack both warm and cool fronts. Locations with oceanic climates tend to feature cloudy conditions with precipitation, though it can experience clear, sunny days. London is an example of an oceanic climate, it experiences constant precipitation throughout the entire year. Despite this, thunderstorms are quite rare since hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year.
However, some areas with this climate see some snowfall annually during winter. Most oceanic climate zones, or at least a part of them, experience at least one snowfall per year. In the poleward locations of the oceanic climate zone, snowfall is more commonplace. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature. In the Köppen climate classification, Oceanic climates have a mean temperature of 0 °C or higher in the coldest month, compared to continental climates where the coldest month has a mean temperature of below 0 °C. Summers are cool, with the warmest month having a mean temperature below 22 °C. Poleward of the latter is a zone of the aforementioned subpolar oceanic climate, with long but mild winters and cool and short summers. Examples of this climate include parts of coastal Iceland, Norway, the Scottish Highlands, the mountains of Vancouver Island, Haida Gwaii in Canada, in the Northern Hemisphere and extreme southern Chile and Argentina in the Southern Hemisphere, the Tasmanian Central Highlands, parts of New Zealand.
Oceanic climates are not always found in coastal locations on the aforementioned parallels. The polar jet stream, which moves in a west to east direction across the middle latitudes, advances low pressure systems and fronts. In coastal areas of the higher middle latitudes, the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are a reflection of the ocean adjacent to them. In the fall and early spring, when the polar jet stream is most active, the frequent passing of marine weather systems creates the frequent fog, cloudy skies, light drizzle associated with oceanic climates. In summer, high pressure pushes the prevailing westerlies north of many oceanic climates creating a drier summer climate; the North Atlantic Gulf Stream, a tropical oceanic current that passes north of the Caribbean and up the East Coast of the United States to North Carolina heads east-northeast to the Azores, is thought to modify the climate of Northwest Europe. As a result of the Gulf Stream, west-coast areas located in high latitudes like Ireland, the UK, Norway have much milder winters than would otherwise be the case.
The lowland attributes of western Europe help drive marine air masses into continental areas, enabling cities such as Dresden and Vienna to have maritime climates in spite of being located well inland from the ocean. Oceanic climates in Europe occur in Northwest Europe, from Ireland and Great Britain eastward to central Europe. Most of France, the Netherlands, Germany, the north coast of Spain, the western Azores off the coast of Portugal, the south of Kosovo and southern portions of Sweden have oceanic climates. Examples of oceanic climates are found in Glasgow, Bergen, Dublin, Bilbao, Donostia-San Sebastian, Bayonne, Züri
Amorebieta-Etxano known as Zornotza, is a town and municipality located in Biscay in the Basque Country, an Autonomous Community in northern Spain. At the time of the 2014 census, the population of the municipality was 18,579, with 16,907 inhabitants living in Amorebieta; the mayor is Andoni Agirrebeitia. Amorebieta-Etxano is an inland town in the comarca of Duranguesado in the province of Biscay in northern Spain, it is about 25 km east of Bilbao and close to the European route E70 which runs along the north coast of Spain. It is located in the valley of the River Ibaizabal. Amorebieta-Etxano has a rich historical heritage; the municipality of Amorebieta-Etxano came into being on 26 January 1951 as the result of a merger between Amorebieta and Etxano, two communities in the historic administrative district of Merindad de Zornotza. The other parts of the district were merged into the neighbouring municipality of Muxika; the new coat of arms shows the union between Etxano. In the 2014 census, Amorebieta had a population of 16,907 while that of Etxano was 221.
The town is divided into several districts. The church of Santa María de la Asunción is in the centre of Amorebieta on the banks of the Ibaizaba, it is a large Renaissance building started in 1555 and opened for worship in 1608 and is noted for its altarpiece. Another Renaissance church is the Parroquia de San Juan Bautista de Larrea; this dates back to 1647, in 1704 it was given to the Carmelite Order to found a convent. In San Antonio is the hermitage of San Miguel de Dudea, nearby is the Neoclassical López Palace. A branch of the international company Tecnalia Research & Innovation is located here in the Parque Empresarial Boroa where the firm employs 1500 people. Xabier Etxeita Jon Aurtenetxe Beñat Intxausti, a professional cyclist. Amorebieta Etxano, Official web page Amorebieta-Etxano in the Bernardo Estornés Lasa – Auñamendi Encyclopedia
Autonomous communities of Spain
In Spain, an autonomous community is a first-level political and administrative division, created in accordance with the Spanish constitution of 1978, with the aim of guaranteeing limited autonomy of the nationalities and regions that make up Spain. Spain is not a federation, but a decentralized unitary state. While sovereignty is vested in the nation as a whole, represented in the central institutions of government, the nation has, in variable degrees, devolved power to the communities, which, in turn, exercise their right to self-government within the limits set forth in the constitution and their autonomous statutes; each community has its own set of devolved powers. Some scholars have referred to the resulting system as a federal system in all but name, or a "federation without federalism". There are 17 autonomous communities and two autonomous cities that are collectively known as "autonomies"; the two autonomous cities have the right to become autonomous communities, but neither has yet exercised it.
This unique framework of territorial administration is known as the "State of Autonomies". The autonomous communities are governed according to the constitution and their own organic laws known as Statutes of Autonomy, which contain all the competences that they assume. Since devolution was intended to be asymmetrical in nature, the scope of competences vary for each community, but all have the same parliamentary structure. Spain is a diverse country made up of several different regions with varying economic and social structures, as well as different languages and historical and cultural traditions. While the entire Spanish territory was united under one crown in 1479 this was not a process of national homogenization or amalgamation; the constituent territories—be it crowns, principalities or dominions—retained much of their former institutional existence, including limited legislative, judicial or fiscal autonomy. These territories exhibited a variety of local customs, laws and currencies until the mid nineteenth century.
From the 18th century onwards, the Bourbon kings and the government tried to establish a more centralized regime. Leading figures of the Spanish Enlightenment advocated for the building of a Spanish nation beyond the internal territorial boundaries; this culminated in 1833, when Spain was divided into 49 provinces, which served as transmission belts for policies developed in Madrid. However, unlike in other European countries such as France, where regional languages were spoken in rural areas or less developed regions, two important regional languages of Spain were spoken in some of the most industrialized areas, moreover, enjoyed higher levels of prosperity, in addition to having their own cultures and historical consciousness; these were Catalonia. This gave rise to peripheral nationalisms along with Spanish nationalism; therefore and social changes that had produced a national cultural unification in France had the opposite effect in Spain. As such, Spanish history since the late 19th century has been shaped by a dialectical struggle between Spanish nationalism and peripheral nationalisms in Catalonia and the Basque Country, to a lesser degree in Galicia.
In a response to Catalan demands, limited autonomy was granted to Catalonia in 1914, only to be abolished in 1923. It was granted again in 1932 during the Second Spanish Republic, when the Generalitat, Catalonia's mediaeval institution of government, was restored; the constitution of 1931 envisaged a territorial division for all Spain in "autonomous regions", never attained—only Catalonia, the Basque Country and Galicia had approved "Statutes of Autonomy"—the process being thwarted by the Spanish Civil War that broke out in 1936, the victory of the rebel Nationalist forces under Francisco Franco. During General Franco's dictatorial regime, centralism was most forcefully enforced as a way of preserving the "unity of the Spanish nation". Peripheral nationalism, along with communism and atheism were regarded by his regime as the main threats, his attempts to fight separatism with heavy-handed but sporadic repression, his severe suppression of language and regional identities backfired: the demands for democracy became intertwined with demands for the recognition of a pluralistic vision of the Spanish nationhood.
When Franco died in 1975, Spain entered into a phase of transition towards democracy. The most difficult task of the newly democratically elected Cortes Generales in 1977 acting as a Constituent Assembly was to transition from a unitary centralized state into a decentralized state in a way that would satisfy the demands of the peripheral nationalists; the Prime Minister of Spain, Adolfo Suárez, met with Josep Tarradellas, president of the Generalitat of Catalonia in exile. An agreement was made so that the Generalitat would be restored and limited competencies would be transferred while the constitution was still being written. Shortly after, the government allowed the creation of "assemblies of members of parliament" integrated by deputies and senators of the different territories of Spain, so that they could constitute "pre-autonomic regimes" for their regions as well; the Fathers of the Constitution had to strike a balance between the opposing views of Spain—on the one hand, the centralist view inherited from Franco's regime, on the other hand federalism and a pluralistic view of Spain as a "nation of nations".
Bay of Biscay
The Bay of Biscay is a gulf of the northeast Atlantic Ocean located south of the Celtic Sea. It lies along the western coast of France from Point Penmarc'h to the Spanish border, the northern coast of Spain west to Cape Ortegal; the south area of the Bay of Biscay washes over the northern coast of Spain and is known as the Cantabrian Sea. The average depth is 1,744 metres and the greatest depth is 4,735 metres; the Bay of Biscay is named after Biscay on the northern Spanish coast standing for the western Basque districts. Its name in other languages is: Asturian: golfu de Biscaya Basque: Bizkaiko golkoa Breton: pleg-mor Gwaskogn French: golfe de Gascogne Galician: golfo de Biscaia Gascon and Occitan: golf de Gasconha Latin: Sinus Biscaiensis Spanish: Golfo de Vizcaya Parts of the continental shelf extend far into the bay, resulting in shallow waters in many areas and thus the rough seas for which the region is known. Large storms occur in the bay during the winter months; the Bay of Biscay is home to some of the Atlantic Ocean's fiercest weather.
Up until recent years it was a regular occurrence for merchant vessels to founder in Biscay storms. The International Hydrographic Organization defines the limits of the Bay of Biscay as "a line joining Cap Ortegal to Penmarch Point"; the southernmost portion is the Cantabrian Sea. The main rivers that empty into the Bay of Biscay are Loire, Garonne, Adour, Bidasoa, Urumea, Urola, Artibai, Oka, Nervión, Agüera, Asón, Pas, Nansa, Sella, Nalón, Esva, Eo, Landro and Sor. In late spring and early summer a large fog triangle fills the southwestern half of the bay, covering just a few kilometers inland; as winter begins, weather becomes severe. Depressions enter from the west frequently and they either bounce north to the British Isles or they enter the Ebro Valley, dry out, are reborn in the form of powerful thunderstorms as they reach the Mediterranean Sea; these depressions cause severe weather at sea and bring light though constant rain to its shores. Sometimes powerful windstorms form if the pressure falls traveling along the Gulf Stream at great speed, resembling a hurricane, crashing in this bay with their maximum power, such as the Klaus storm.
The Gulf Stream enters the bay following the continental shelf's border anti-clockwise, keeping temperatures moderate all year long. The main cities on the shores of the Bay of Biscay are Bordeaux, Biarritz, Nantes, La Rochelle, Donostia-San Sebastián, Santander, Gijón and Avilés; the southern end of the gulf is called in Spanish "Mar Cantábrico", from the Estaca de Bares, as far as the mouth of Adour river, but this name is not used in English. It was named by Romans in the 1st century BC as Sinus Cantabrorum and Mare Gallaecum. On some medieval maps, the Bay of Biscay is marked as El Mar del los Vascos; the Bay of Biscay has been the site of many famous naval engagements over the centuries. In 1592 the Spanish defeated an English fleet during the eponymous Battle of the Bay of Biscay; the Biscay campaign of June 1795 consisted of a series of manoeuvres and two battles fought between the British Channel Fleet and the French Atlantic Fleet off the southern coast of Brittany during the second year of the French Revolutionary Wars.
USS Californian sank here after striking a naval mine on 22 June 1918. In 1920 SS Afrique sank after losing power and drifting into a reef in a storm with the loss of 575 lives. On 28 December 1943, the Battle of the Bay of Biscay was fought between HMS Glasgow and HMS Enterprise and a group of German destroyers as part of Operation Stonewall during World War II. U-667 sank on 25 August 1944 in position 46 ° 00 ′ N 01 ° 30 ′ W. All hands were lost. On 12 April 1970, Soviet submarine K-8 sank in the Bay of Biscay due to a fire that crippled the submarine's nuclear reactors. An attempt to save the sub failed, resulting in the death of forty sailors and the loss of four nuclear torpedoes. Due to the great depth, no salvage operation was attempted; the car ferries from Gijón to Nantes/Saint-Nazaire, Portsmouth to Bilbao and from Plymouth and Poole to Santander provide one of the most convenient ways to see cetaceans in European waters. Specialist groups take the ferries to hear more information. Volunteers and employees of ORCA observe and monitor cetacean activity from the bridge of the ships on Brittany Ferries' Portsmouth to Santander route.
Many species of whales and dolphins can be seen in this area. Most it is one of the few places in the world where the beaked whales, such as the Cuvier's beaked whale, have been observed frequently. Biscay Dolphin Research monitored cetacean activity from the P&O Ferries cruiseferry Pride of Bilbao, on voyages from Portsmouth to Bilbao. North Atlantic Right Whales, one of the most endangered whales, once came to the bay for feeding and for calving as well, but whaling activities by Basque people wiped them out sometime prior to 1850s; the eastern population of this species are considered to be extinct, a