War of the Spanish Succession
The War of the Spanish Succession was a European conflict of the early 18th century, triggered by the death of the childless Charles II of Spain in November 1700. His closest heirs were members of the Austrian Habsburg and French Bourbon families. Charles left an undivided Monarchy of Spain to Louis XIV's grandson Philip, proclaimed King of Spain on 16 November 1700. Disputes over separation of the Spanish and French crowns and commercial rights led to war in 1701 between the Bourbons of France and Spain and the Grand Alliance, whose candidate was Archduke Charles, younger son of Leopold I, Holy Roman Emperor. By the end of 1706, Allied victories in Italy and the Low Countries forced the French back within their borders but they were unable to make a decisive breakthrough. Control of the sea allowed the Allies to conduct successful offensives in Spain, but lack of popular support for Archduke Charles meant they could not hold territory outside the coastal areas. Conflict extended to European colonies in North America, where it is known as Queen Anne's War, the West Indies as well as minor struggles in Colonial India.
Related conflicts include Rákóczi's War of Independence in Hungary, funded by France and the 1704–1710 Camisard rebellion in South-East France, funded by Britain. When his elder brother Joseph died in 1711, Charles succeeded him as Emperor, undermining the primary driver behind the war, to prevent Spain being united with either France or Austria; the 1710 British election returned a new government committed to ending it and with the Allied war effort now dependent on British financing, this forced the others to make peace. The war ended with the 1713 Treaty of Utrecht, followed in 1714 by the treaties of Rastatt and Baden. In return for confirmation as King of Spain, Philip V renounced his place in the line of succession to the French throne, both for himself and his descendants; the Dutch Republic was granted its Barrier Fortresses, while France acknowledged the Protestant succession in Britain and agreed to end support for the Stuart exiles. In the longer term, the commercial provisions of Utrecht confirmed Britain's status as the leading European maritime and commercial power, while the Dutch lost their position as the pre-eminent economic power in Asia and the war marked their decline as a first-rank power.
Other long-term impacts include the creation of a centralised Spanish state and the acceleration of the break-up of the Holy Roman Empire into larger and more powerful German principalities. In 1665 Charles II became the last male Habsburg King of Spain. In 1670, England agreed to support the rights of Louis XIV to the Spanish throne in the Treaty of Dover, while the terms of the 1688 Grand Alliance committed England and the Dutch Republic to back Leopold. In 1700, the Spanish Empire included possessions in Italy, the Spanish Netherlands, the Philippines and the Americas and though no longer the dominant great power, it remained intact. Since acquisition of the Empire by either the Austrian Habsburgs or French Bourbons would change the balance of power in Europe, its inheritance led to a war that involved most of the European powers; the 1700-1721 Great Northern War is considered a connected conflict, since it impacted the involvement of states such as Sweden, Denmark–Norway and Russia. During the 1688–1697 Nine Years War, armies had increased in size from an average of 25,000 in 1648 to over 100,000 by 1697, a level unsustainable for pre-industrial economies.
The 1690s marked the lowest point of the Little Ice Age, a period of colder and wetter weather that drastically reduced crop yields. The Great Famine of 1695-1697 killed between 15-25% of the population in present-day Scotland, Finland, Latvia and Sweden, with an estimated two million deaths in France and Northern Italy; the 1697 Treaty of Ryswick was therefore the result of mutual exhaustion and Louis XIV's acceptance that France could not achieve its objectives without allies. Leopold refused to sign and did so with extreme reluctance in October 1697. Unlike France or Austria, the Crown of Spain could be inherited through the female line; this allowed Charles' sisters Maria Theresa and Margaret Theresa to pass their rights as rulers onto the children of their respective marriages with Louis XIV and Emperor Leopold. Despite being opponents in the recent Nine Years War, Louis XIV and William III of England now attempted to resolve the Succession by diplomacy. In 1685, Maria Antonia, daughter of Leopold and Margaret, married Maximillian Emanuel of Bavaria and they had a son, Joseph Ferdinand.
The 1698 Treaty of the Hague or First Partition Treaty between France and the Dutch Republic made the six year old heir to the bulk of the Spanish Monarchy and divided its European territories between France and Austria. The Spanish refused to accept the division of their Empire and on 14 November 1698, Charles published his Will, making Joseph Ferdinand heir to an independent and undivided Spanish monarchy; when he died of smallpox in February 1699, a new solution was required. This was of doubtful legality but France and the Nethe
Cartagena is a Spanish city and a major naval station located in the Region of Murcia, by the Mediterranean coast, south-eastern Spain. As of January 2018, it has a population of 213,943 inhabitants, being the Region’s second largest municipality and the country’s sixth largest non-Province-capital city; the metropolitan area of Cartagena, known as Campo de Cartagena, has a population of 409,586 inhabitants. Cartagena has been inhabited for over two millennia, being founded around 227 BC by the Carthaginian Hasdrubal the Fair as Qart Hadasht the same name as the original city of Carthage; the city had its heyday during the Roman Empire, when it was known as Carthago Nova and Carthago Spartaria, capital of the province of Carthaginensis. It was one of the important cities during the Umayyad invasion of Hispania, under its Arabic name of Qartayannat al-Halfa. Much of the historical weight of Cartagena in the past goes to its coveted defensive port, one of the most important in the western Mediterranean.
Cartagena has been the capital of the Spanish Navy's Maritime Department of the Mediterranean since the arrival of the Spanish Bourbons in the 18th century. As far back as the 16th century it was one of the most important naval ports in Spain, together with Ferrol in the North, it is still an important naval seaport, the main military haven of Spain, is home to a large naval shipyard. The confluence of civilizations as well as its strategic harbour, together with the rise of the local mining industry is manifested by a unique artistic heritage, with a number of landmarks such as the Roman Theatre, the second largest of the Iberian Peninsula after the one in Mérida, an abundance of Phoenician, Roman and Moorish remains, a plethora of Art Nouveau buildings, a result of the bourgeoisie from the early 20th century. Cartagena is now established as a major cruise ship destination in the Mediterranean and an emerging cultural focus, it is the first of a number of cities that have been named Cartagena, most notably Cartagena de Indias in Colombia.
The city of Cartagena is located in the southeastern region of Spain in the Campo de Cartagena. The Cartagena region can be viewed as a great plain inclined in the direction NW-SE, bordered at the north and the northwest by pre-coastal mountain ranges, at the south and southwest by coastal mountain ranges; the dominant geology of the region is sedimentary. The city is located just at the end of the new AP-7 motorway; the following villages are part of Cartagena municipality: La Azohía, Isla Plana, Los Urrutias and Los Nietos. The Old Town is limited by five small hills following the example of Rome. In the past, there was an inner sea between the hills called the Estero that dried up. On this site, the "Ensanche" was built at the beginning of the 20th century; the urban area is delimited or crossed by several watercourses, some of which go deep into the urban network during a large part of their courses. Cartagena has a hot semi-arid climate, its location near the ocean moderates the temperature, annual precipitation does not surpass 300 mm.
The annual average temperature goes up to around 20.4 °C, making it—for the year 2014–the warmest city in Europe. The coldest month is January, with an average temperature of 13.7 °C. In August, the warmest month, the average temperature is 28.7 °C. The wind is an important climatic factor in the region. Despite the intense mining and industrial exploitation that the area has suffered for centuries, the territory around Cartagena city hosts an extraordinary natural wealth and diversity, with a large number of botanical endemic species. Part of its area is subject to different levels of legal protection. Cartagena’s coastal mountains have one of the highest levels of botanical biodiversity on the Iberian Peninsula. A number of surprising Ibero-African species, which are only found in southern Spain and North Africa. Among these, there stands out Tetraclinis articulata or Sandarac native to Morocco, Tunisia and Cartagena, growing at low altitudes in a hot, dry Mediterranean woodland; some species are endangered like the siempreviva de Cartagena, the rabogato del Mar Menor, the zamarrilla de Cartagena, the manzanilla de escombreras, the garbancillo de Tallante and the jara de Cartagena Cistus heterophyllus carthaginensis).
Among the animal species includes some threatened or endangered ones like the peregrine falcon, the Eurasian eagle-owl, the golden eagle and the Bonelli's eagle, the Spur-thighed Tortoise, the Greater Horseshoe Bat and the Spanish toothcarp, an fish endemic to south-eastern Spain. In addition, the presence of the common chameleon has been documented for about 30 years, although it is not clear whether it is native or introduced; some other species of note include the greater flamingo, the red fox, the European rabbit, the European badger, the Beech marten, the common genet, the wildcat and the wild boar. Mar Menor, a salty lagoon separated from the Mediterranean sea by a sand bar 22 kilometres in length and with a variable width
A lagoon is a shallow body of water separated from a larger body of water by barrier islands or reefs. Lagoons are divided into coastal lagoons and atoll lagoons, they have been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as estuaries. Lagoons are common coastal features around many parts of the world. Lagoons are shallow elongated bodies of water separated from a larger body of water by a shallow or exposed shoal, coral reef, or similar feature; some authorities include fresh water bodies in the definition of "lagoon", while others explicitly restrict "lagoon" to bodies of water with some degree of salinity. The distinction between "lagoon" and "estuary" varies between authorities. Richard A. Davis Jr. restricts "lagoon" to bodies of water with little or no fresh water inflow, little or no tidal flow, calls any bay that receives a regular flow of fresh water an "estuary". Davis does state that the terms "lagoon" and "estuary" are "often loosely applied in scientific literature."
Timothy M. Kusky characterizes lagoons as being elongated parallel to the coast, while estuaries are drowned river valleys, elongated perpendicular to the coast; when used within the context of a distinctive portion of coral reef ecosystems, the term "lagoon" is synonymous with the term "back reef" or "backreef", more used by coral reef scientists to refer to the same area. Coastal lagoons are classified as inland bodies of water. Many lagoons do not include "lagoon" in their common names. Albemarle and Pamlico sounds in North Carolina, Great South Bay between Long Island and the barrier beaches of Fire Island in New York, Isle of Wight Bay, which separates Ocean City, Maryland from the rest of Worcester County, Banana River in Florida, Lake Illawarra in New South Wales, Montrose Basin in Scotland, Broad Water in Wales have all been classified as lagoons, despite their names. In England, The Fleet at Chesil Beach has been described as a lagoon. In Latin America, the term laguna in Spanish, which lagoon translates to, may be used for a small fresh water lake in a similar way a creek is considered a small river.
However, sometimes it is popularly used to describe a full-sized lake, such as Laguna Catemaco in Mexico, the third largest lake by area in the country. The brackish water lagoon may be thus explicitly identified as a "coastal lagoon". In Portuguese the same usage is found: lagoa may be a body of shallow sea water, or a small freshwater lake not linked to the sea. Lagoon is derived from the Italian laguna, which refers to the waters around Venice, the Lagoon of Venice. Laguna is attested in English by at least 1612, had been Anglicized to "lagune" by 1673. In 1697 William Dampier referred to a "Lake of Salt water" on the coast of Mexico. Captain James Cook described an island "of Oval form with a Lagoon in the middle" in 1769. Atoll lagoons form as coral reefs grow upwards while the islands that the reefs surround subside, until only the reefs remain above sea level. Unlike the lagoons that form shoreward of fringing reefs, atoll lagoons contain some deep portions. Coastal lagoons form along sloping coasts where barrier islands or reefs can develop off-shore, the sea-level is rising relative to the land along the shore.
Coastal lagoons do not form along steep or rocky coasts, or if the range of tides is more than 4 metres. Due to the gentle slope of the coast, coastal lagoons are shallow, they are sensitive to changes in sea level due to global warming. A relative drop in sea level may leave a lagoon dry, while a rise in sea level may let the sea breach or destroy barrier islands, leave reefs too deep under water to protect the lagoon. Coastal lagoons are young and dynamic, may be short-lived in geological terms. Coastal lagoons are common. In the United States, lagoons are found along more than 75 percent of the Gulf coasts. Coastal lagoons are connected to the open ocean by inlets between barrier islands; the number and size of the inlets, precipitation and inflow of fresh water all affect the nature of the lagoon. Lagoons with little or no interchange with the open ocean, little or no inflow of fresh water, high evaporation rates, such as Lake St. Lucia, in South Africa, may become saline. Lagoons with no connection to the open ocean and significant inflow of fresh water, such as the Lake Worth Lagoon in Florida in the middle of the 19th century, may be fresh.
On the other hand, lagoons with many wide inlets, such as the Wadden Sea, have strong tidal currents and mixing. Coastal lagoons tend to accumulate sediments from inflowing rivers, from runoff from the shores of the lagoon, from sediment carried into the lagoon through inlets by the tide. Large quantities of sediment may be be deposited in a lagoon when storm waves overwash barrier islands. Mangroves and marsh plants can facilitate the accumulation of sediment in a lagoon. Benthic organisms may destabilize sediments. River-mouth lagoons on mixed sand and gravel beaches form at the river-coast interface where a braided, although sometimes meandering, river interacts with a coastal environment, affected by longshore drift; the lagoons which form on the MSG coastlines are common on the east coast of the South Island of New Zealand and have long been referred to as hapua by the Māori. This classification differentiates hapua from similar lagoons located on the N
The Costa Cálida is the 250 km stretch of Mediterranean coastline of the Spanish province of Murcia. This region has a micro-climate which features comparatively hot mean annual temperatures and a relative degree of aridity; the Costa Cálida extends from El Mojón in the north near the province of Alicante, to near the municipality of Águilas in the south bordering on the region of Almería province. The northern end of this coastline includes the Mar Menor, a coastal saltwater lagoon which at around 170 km2 is Europe's largest; the Mar Menor is separated from the Mediterranean by a 22 km-long spit of land called La Manga, on which most of the tourism development for the region has been constructed. Cartagena and Mazarrón are two other important coastal towns in the region. Golf is a popular pastime for residents. There are many PGA championship courses such as El Valle which hosted the PGA European Seniors Tour in June 2011, Hacienda del Alamo, the longest golf course in Spain and the famous La Manga Club.
Official Tourism Site of Murcia, Spain Guide to Whats Going On in the Costa Calida & Murcia Information for tourists and locals living on the Costa Calida Murcia. Wrong link. Costa Blanca is not Costa Calida
Mudéjar refers to an architecture and decoration style in Christian Iberia, influenced by Moorish taste and workmanship, reaching its greatest expression in medieval Aragon and the city of Toledo. Mudéjar refers to the large group of Muslims in Spain who remained in Christian Iberia despite their territories being reconquered; the distinctive Mudéjar style is still evident in regional architecture, as well as in art, crafts Hispano-Moresque ware, lustreware pottery, exported across Europe. The Mudéjar style was first characterized as a specific aesthetic trend by Spanish art historian Pedro de Madrazo in 1888; this important distinction clarified that the specific qualities were not just signature of specific artisans or craftsmen but it was the collective aesthetic style of Mudéjar Muslims in the Iberian peninsula. Mudéjar was the term used for Moors or Muslims of Al-Andalus who remained in Iberia after the Christian Reconquista but were not forcibly converted to Christianity or forcibly exiled.
The word Mudéjar references cultural borrowings. It was a medieval Spanish borrowing of the Arabic word Mudajjan مدجن, meaning "tamed", referring to Muslims who submitted to the rule of Christian kings; the term originated as a taunt, as the word was applied to domesticated animals such as poultry. The term Mudéjar can be translated from Arabic as "one permitted to remain", which references Christians allowing Muslims to remain in Christian Spain. Another term with the same meaning, ahl al-dajn, was used by Muslim writers, notably al-Wansharisi in his work Kitab al-Mi'yar. Mudéjars in Spain lived under a protected tributary status known as dajn which references ahl al-dajn; this protected status suggested subjugation at the hands of Christian rulers as the word dajn resembled haywanāt dājina which meant "tame animals". Their protected status was enforced by local charters which dictated Christians laws. Muslims of other regions outside of the Iberian Peninsula disapproved of the Mudéjar subjugated status and their willingness to live with non-Muslims.
Mudéjar was used in contrast to both Muslims in Muslim-ruled areas and Moriscos, who were forcibly converted and may or may not have continued to secretly practice Islam. The Treaty of Granada protected religious and cultural freedoms for Muslims in the imminent transition from the Emirate of Granada to a Province of Castile. After the fall of the last Islamic kingdom in the Battle of Granada in January 1492, Mudéjars, unlike the Jews who were expelled that same year, kept a protected religious status, although there were Catholic efforts to convert them. However, over the next several decades this religious freedom deteriorated. Islam was outlawed in Portugal by 1497, the Crown of Castile by 1502, the Crown of Aragon by 1526, forcing the Mudéjars to convert or in some cases leave the country. Following the forced conversion, they faced suspicions that they were not converted but remained crypto-Muslims, were known as Moriscos; the Moriscos, were expelled, in 1609–1614. The Muslim population in Castile immigrated from Toledo and other Andalusi territories.
They were not original to the land in Castile. Muslim immigration into Castile was sponsored settlement by the Kingdom of Castile, it is hypothesized that the slow-growing Christian population demonstrated a need to bring more people into Castile. Primary documents written by the Spanish in Castile in the 13th century indicate that Muslims were able to maintain some agency while in Spain; the Mudéjars were able to maintain their religion, their laws, they had their own judges. The Mudéjars in Castile spoke the Romance dialects as their Christian neighbors. Like the Mudéjars in Castile and Catalan Mudéjars spoke the Romance languages of their Christian counterparts. However, unlike the Mudéjars in Castile, there were Muslim villages in Aragon and, to a lesser extent, in south-western Catalonia which populated the land before Christian conquests, setting up a history of Muslim cultivation and population of the land. Besides the large Muslim populations in Granada and Valencia, the Aragonese Muslim peasants were the most well-established Muslim community in the region, while in Catalonia Muslim authoctonous presence was limited only to the Low Ebro and Low Segre areas.
Aragonese and Catalan Muslims were under the jurisdiction of the Christian Crown and were designated a special status. This status applied to the Mudéjar cultivators, the exarici, this status made them subservient to their Christian superiors because by law, they were required to cultivate the land of royal estates. However, this status was beneficial as the law suggested that this land be passed down through Muslim family members. Despite their expulsion at the end of the Morisco period, the Mudéjars in Aragon left evidence of their style in architecture, while in Catalonia only some reminiscences of this architecture can be appreciated in some Gothic churches and cathedrals in some shires of Lleida. In the 13th century, the Aragonese Christians conquered Valencia. Unlike in Aragon, the Mudéjar population in Valencia vastly outnumbered Christians in the area. In Valencia, the majority of communities were Muslim. Although there was a disparity between Christians and Muslims, it is important to note that a Christian king ruled over Valencia, not a sultan or an imam and this shaped the experience of Mudéjars in this regi
Philip II of Spain
Philip II was King of Spain, King of Portugal, King of Naples and Sicily, jure uxoris King of England and Ireland. He was Duke of Milan. From 1555 he was lord of the Seventeen Provinces of the Netherlands; the son of Holy Roman Emperor and King of Spain Charles V and Isabella of Portugal, Philip was called "Felipe el Prudente" in Spain. During his reign, Spain reached the height of its power; this is sometimes called the Spanish Golden Age. The expression "the empire on which the sun never sets" was coined during Philip's time to reflect the extent of his dominion. During Philip's reign there were separate state bankruptcies in 1557, 1560, 1569, 1575, 1596; this was the cause of the declaration of independence that created the Dutch Republic in 1581. On 31 December 1584 Philip signed the Treaty of Joinville, with Henry I, Duke of Guise signing on behalf of the Catholic League. A devout Catholic, Philip saw himself as the defender of Catholic Europe against the Ottoman Empire and the Protestant Reformation.
He sent a large armada to invade Protestant England in 1588, with the strategic aim of overthrowing Elizabeth I of England and the establishment of Protestantism in England. He hoped to stop both English interference in the Spanish Netherlands and the harm caused to Spanish interests by English and Dutch privateering. Philip was described by the Venetian ambassador Paolo Fagolo in 1563 as "slight of stature and round-faced, with pale blue eyes, somewhat prominent lip, pink skin, but his overall appearance is attractive"; the Ambassador went on to say "He dresses tastefully, everything that he does is courteous and gracious." Besides Mary I, Philip was married three other times and widowed four times. The son of Charles I and V, King of Spain and Holy Roman Emperor and his wife, Isabella of Portugal, Philip was born in the Spanish capital of Valladolid on 21 May 1527 at Palacio de Pimentel, owned by Don Bernardino Pimentel; the culture and courtly life of Spain were an important influence in his early life.
He was tutored by the future Archbishop of Toledo. Philip displayed reasonable aptitude in letters alike, he would study with more illustrious tutors, including the humanist Juan Cristóbal Calvete de Estrella. Though Philip had good command over Latin and Portuguese, he never managed to equal his father, Charles V, as a polyglot. While Philip was a German archduke of the House of Habsburg, he was seen as a foreigner in the Holy Roman Empire; the feeling was mutual. Philip felt himself to be culturally Spanish; this would impede his succession to the imperial throne. In April 1528, when Philip was eleven months old, he received the oath of allegiance as heir to the crown from the Cortes of Castile. From that time until the death of his mother Isabella in 1539, he was raised in the royal court of Castile under the care of his mother and one of her Portuguese ladies, Dona Leonor de Mascarenhas, to whom he was devotedly attached. Philip was close to his two sisters, María and Juana, to his two pages, the Portuguese nobleman Rui Gomes da Silva and Luis de Requesens, the son of his governor Juan de Zúñiga.
These men would serve Philip throughout their lives, as would Antonio Pérez, his secretary from 1541. Philip's martial training was undertaken by his governor, Juan de Zúñiga, a Castilian nobleman who served as the commendador mayor of Castile; the practical lessons in warfare were overseen by the Duke of Alba during the Italian Wars. Philip was present at the Siege of Perpignan in 1542 but did not see action as the Spanish army under Alba decisively defeated the besieging French forces under the Dauphin of France. On his way back to Castile, Philip received the oath of allegiance of the Aragonese Cortes at Monzón, his political training had begun a year under his father, who had found his son studious and prudent beyond his years, having decided to train and initiate him in the government of Spain. The king-emperor's interactions with his son during his stay in Spain convinced him of Philip's precocity in statesmanship, so he determined to leave in his hands the regency of Spain in 1543. Philip, made the Duke of Milan in 1540, began governing the most extensive empire in the world at the young age of sixteen.
Charles left Philip with experienced advisors—notably the secretary Francisco de los Cobos and the general Duke of Alba. Philip was left with extensive written instructions that emphasised "piety, patience and distrust." These principles of Charles were assimilated by his son, who would grow up to become grave, self-possessed and cautious. Philip spoke and had an icy self-mastery. After living in the Netherlands in the early years of his reign, Philip II decided to return to Spain. Although sometimes described as an absolute monarch, Philip faced many constitutional constraints on his authority, influenced by the growing strength of the bureaucracy; the Spanish Empire was not a single monarchy with one legal system but a federation of separate r
The Mediterranean Sea is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and completely enclosed by land: on the north by Southern Europe and Anatolia, on the south by North Africa and on the east by the Levant. Although the sea is sometimes considered a part of the Atlantic Ocean, it is identified as a separate body of water. Geological evidence indicates that around 5.9 million years ago, the Mediterranean was cut off from the Atlantic and was or desiccated over a period of some 600,000 years, the Messinian salinity crisis, before being refilled by the Zanclean flood about 5.3 million years ago. It covers an approximate area of 2.5 million km2, representing 0.7 % of the global ocean surface, but its connection to the Atlantic via the Strait of Gibraltar-the narrow strait that connects the Atlantic Ocean to the Mediterranean Sea and separates Spain in Europe from Morocco in Africa- is only 14 km wide. In oceanography, it is sometimes called the Eurafrican Mediterranean Sea or the European Mediterranean Sea to distinguish it from mediterranean seas elsewhere.
The Mediterranean Sea has an average depth of 1,500 m and the deepest recorded point is 5,267 m in the Calypso Deep in the Ionian Sea. The sea is bordered on the north by Europe, the east by Asia, in the south by Africa, it is located between latitudes 30° and 46° N and longitudes 6° W and 36° E. Its west-east length, from the Strait of Gibraltar to the Gulf of Iskenderun, on the southwestern coast of Turkey, is 4,000 km; the sea's average north-south length, from Croatia's southern shore to Libya, is 800 km. The sea was an important route for merchants and travellers of ancient times that allowed for trade and cultural exchange between emergent peoples of the region; the history of the Mediterranean region is crucial to understanding the origins and development of many modern societies. The countries surrounding the Mediterranean in clockwise order are Spain, Monaco, Slovenia, Croatia and Herzegovina, Albania, Turkey, Lebanon, Egypt, Tunisia and Morocco. In addition, the Gaza Strip and the British Overseas Territories of Gibraltar and Akrotiri and Dhekelia have coastlines on the sea.
The Ancient Greeks called the Mediterranean ἡ θάλασσα or sometimes ἡ μεγάλη θάλασσα, ἡ ἡμέτερα θάλασσα, or ἡ θάλασσα ἡ καθ'ἡμᾶς. The Romans called it Mare Mare Internum and, starting with the Roman Empire, Mare Nostrum; the term Mare Mediterrāneum appears later: Solinus used it in the 3rd century, but the earliest extant witness to it is in the 6th century, in Isidore of Seville. It means'in the middle of land, inland' in Latin, a compound of medius, -āneus; the Latin word is a calque of Greek μεσόγειος, from μέσος and γήινος, from γῆ. The original meaning may have been'the sea in the middle of the earth', rather than'the sea enclosed by land'; the Carthaginians called it the "Syrian Sea". In ancient Syrian texts, Phoenician epics and in the Hebrew Bible, it was known as the "Great Sea" or as "The Sea". Another name was the "Sea of the Philistines", from the people inhabiting a large portion of its shores near the Israelites. In Modern Hebrew, it is called HaYam HaTikhon'the Middle Sea'. In Modern Arabic, it is known as al-Baḥr al-Mutawassiṭ'the Middle Sea'.
In Islamic and older Arabic literature, it was Baḥr al-Rūm'the Sea of the Romans' or'the Roman Sea'. At first, that name referred to only the Eastern Mediterranean, but it was extended to the whole Mediterranean. Other Arabic names were Baḥr al-šām'the Sea of Syria' and Baḥr al-Maghrib'the Sea of the West'. In Turkish, it is the Akdeniz'the White Sea'; the origin of the name is not clear, as it is not known in earlier Greek, Byzantine or Islamic sources. It may be to contrast with the Black Sea. In Persian, the name was translated as Baḥr-i Safīd, used in Ottoman Turkish, it is the origin of the colloquial Greek phrase Άσπρη Θάλασσα. Johann Knobloch claims that in Classical Antiquity, cultures in the Levant used colours to refer to the cardinal points: black referred to the north, yellow or blue to east, red to south, white to west; this would explain both the Turkish Akdeniz and the Arab nomenclature described above. Several ancient civilizations were located around the Mediterranean shores and were influenced by their proximity to the sea.
It provided routes for trade and war, as well as food for numerous communities throughout the ages. Due to the shared climate and access to the sea, c