1.
French Revolutionary Wars
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The French Revolutionary Wars were a series of sweeping military conflicts, lasting from 1792 until 1802, resulting from the French Revolution. They pitted the French First Republic against Britain, Austria and several other monarchies and they are divided in two periods, the War of the First Coalition and the War of the Second Coalition. Initially confined to Europe, the fighting gradually assumed a global dimension as the political ambitions of the Revolution expanded, French success in these conflicts ensured the spread of revolutionary principles over much of Europe. The Revolutionary Wars began from increasing political pressure on King Louis XVI of France to prove his loyalty to the new direction France was taking. In the spring of 1792, France declared war on Prussia and Austria, the victory rejuvenated the French nation and emboldened the National Convention to abolish the monarchy. A series of victories by the new French armies abruptly ended with defeat at Neerwinden in the spring of 1793, by 1795, the French had captured the Austrian Netherlands and knocked Spain and Prussia out of the war with the Peace of Basel. A hitherto unknown general called Napoleon Bonaparte began his first campaign in Italy in April 1796, in less than a year, French armies under Napoleon decimated the Habsburg forces and evicted them from the Italian peninsula, winning almost every battle and capturing 150,000 prisoners. With French forces marching towards Vienna, the Austrians sued for peace and agreed to the Treaty of Campo Formio, the War of the Second Coalition began with the French invasion of Egypt, headed by Napoleon, in 1798. The Allies took the opportunity presented by the French strategic effort in the Middle East to regain territories lost from the First Coalition. The war began well for the Allies in Europe, where they pushed the French out of Italy and invaded Switzerland—racking up victories at Magnano, Cassano. However, their efforts largely unraveled with the French victory at Zurich in September 1799, meanwhile, Napoleons forces annihilated a series of Egyptian and Ottoman armies at the battles of the Pyramids, Mount Tabor, and Abukir. These victories and the conquest of Egypt further enhanced Napoleons popularity back in France, however, the Royal Navy had managed to inflict a humiliating defeat on the French fleet at the Battle of the Nile in 1798, further strengthening British control of the Mediterranean. Napoleons arrival from Egypt led to the fall of the Directory in the Coup of 18 Brumaire, Napoleon then reorganized the French army and launched a new assault against the Austrians in Italy during the spring of 1800. This latest effort culminated in a decisive French victory at the Battle of Marengo in June 1800, another crushing French triumph at Hohenlinden in Bavaria forced the Austrians to seek peace for a second time, leading to the Treaty of Lunéville in 1801. With Austria and Russia out of the war, the United Kingdom found itself increasingly isolated and agreed to the Treaty of Amiens with Napoleons government in 1802, concluding the Revolutionary Wars. The lingering tensions proved too difficult to contain, however, in 1789–1792, the entire governmental structure of France was transformed to fall into line with the Revolutionary principles of Liberty, Equality and Fraternity. As a result, one of the first major elements of the French state to be restructured was the army, the transformation of the army was best seen in the officer corps. Before the revolution 90% had been nobility, compared to only 3% in 1794, Revolutionary fervour was high, and was closely monitored by the Committee of Public Safety, which assigned Representatives on Mission to keep watch on generals
2.
Napoleonic Wars
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The wars resulted from the unresolved disputes associated with the French Revolution and the Revolutionary Wars, which had raged on for years before concluding with the Treaty of Amiens in 1802. Napoleon became the First Consul of France in 1799, then Emperor five years later, inheriting the political and military struggles of the Revolution, he created a state with stable finances, a strong central bureaucracy, and a well-trained army. The British frequently financed the European coalitions intended to thwart French ambitions, by 1805, they had managed to convince the Austrians and the Russians to wage another war against France. At sea, the Royal Navy destroyed a combined Franco-Spanish fleet at Trafalgar in October 1805, Prussian worries about increasing French power led to the formation of the Fourth Coalition in 1806. France then forced the defeated nations of the Fourth Coalition to sign the Treaties of Tilsit in July, although Tilsit signified the high watermark of the French Empire, it did not bring a lasting peace for Europe. Hoping to extend the Continental System and choke off British trade with the European mainland, Napoleon invaded Iberia, the Spanish and the Portuguese revolted with British support. The Peninsular War lasted six years, featured extensive guerrilla warfare, the Continental System caused recurring diplomatic conflicts between France and its client states, especially Russia. Unwilling to bear the consequences of reduced trade, the Russians routinely violated the Continental System. The French launched an invasion of Russia in the summer of 1812. The resulting campaign witnessed the collapse and retreat of the Grand Army along with the destruction of Russian lands. In 1813, Prussia and Austria joined Russian forces in a Sixth Coalition against France, a lengthy military campaign culminated in a large Allied army defeating Napoleon at the Battle of Leipzig in October 1813. The Allies then invaded France and captured Paris in the spring of 1814 and he was exiled to the island of Elba near Rome and the Bourbons were restored to power. However, Napoleon escaped from Elba in February 1815 and took control of France once again, the Allies responded by forming a Seventh Coalition, which defeated Napoleon at the Battle of Waterloo in June. The Congress of Vienna, which started in 1814 and concluded in 1815, established the new borders of Europe and laid out the terms, Napoleon seized power in 1799, creating a de facto military dictatorship. The Napoleonic Wars began with the War of the Third Coalition, Kagan argues that Britain was irritated in particular by Napoleons assertion of control over Switzerland. Furthermore, Britons felt insulted when Napoleon stated that their country deserved no voice in European affairs, for its part, Russia decided that the intervention in Switzerland indicated that Napoleon was not looking toward a peaceful resolution of his differences with the other European powers. The British quickly enforced a blockade of France to starve it of resources. Napoleon responded with economic embargoes against Britain, and sought to eliminate Britains Continental allies to break the coalitions arrayed against him, the so-called Continental System formed a league of armed neutrality to disrupt the blockade and enforce free trade with France
3.
English Channel
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The English Channel, also called simply the Channel, is the body of water that separates southern England from northern France, and links the southern part of the North Sea to the Atlantic Ocean. It is about 560 km long and varies in width from 240 km at its widest to 33.3 km in the Strait of Dover and it is the smallest of the shallow seas around the continental shelf of Europe, covering an area of some 75,000 km2. The International Hydrographic Organization defines the limits of the English Channel as follows, a line joining Isle Vierge to Lands End. The southwestern limit of the North Sea, the IHO defines the southwestern limit of the North Sea as a line joining the Walde Lighthouse and Leathercoat Point. The Walde Lighthouse is 6 km east of Calais, and Leathercoat Point is at the end of St Margarets Bay. The Strait of Dover, at the Channels eastern end, is its narrowest point and it is relatively shallow, with an average depth of about 120 m at its widest part, reducing to a depth of about 45 m between Dover and Calais. Eastwards from there the adjoining North Sea reduces to about 26 m in the Broad Fourteens where it lies over the watershed of the land bridge between East Anglia and the Low Countries. It reaches a depth of 180 m in the submerged valley of Hurds Deep,48 km west-northwest of Guernsey. The eastern region along the French coast between Cherbourg and the mouth of the Seine river at Le Havre is frequently referred to as the Bay of the Seine. There are several islands in the Channel, the most notable being the Isle of Wight off the English coast. The coastline, particularly on the French shore, is indented, several small islands close to the coastline, including Chausey. The Cotentin Peninsula in France juts out into the Channel, whilst on the English side there is a parallel channel known as the Solent between the Isle of Wight and the mainland. The Celtic Sea is to the west of the Channel, the time difference of about six hours between high water at the eastern and western limits of the Channel is indicative of the tidal range being amplified further by resonance. It was never defined as a border and the names were more or less descriptive. It was not considered as the property of a nation, strangely, before the development of the modern nations, British scholars very often referred to it as Gaulish and the French one as British or English. The name English Channel has been used since the early 18th century. In modern Dutch, however, it is known as Het Kanaal, later, it has also been known as the British Channel or the British Sea having been called the Oceanus Britannicus by the 2nd-century geographer Ptolemy. The same name is used on an Italian map of about 1450, the Anglo-Saxon texts often call it Sūð-sǣ as opposed to Norð-sǣ
4.
Strait of Gibraltar
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The Strait of Gibraltar is a narrow strait that connects the Atlantic Ocean to the Mediterranean Sea and separates Gibraltar and Peninsular Spain in Europe from Morocco and Ceuta in Africa. The name comes from the Rock of Gibraltar, which in turn originates from the Arabic Jebel Tariq named after Tariq ibn Ziyad. It is also known as the Straits of Gibraltar, the Gut of Gibraltar, the STROG in naval use, and Bab Al Maghrib, Gate of the West. In the Middle Ages, Muslims called it Al-Zuqaq, The Passage, the Romans called it Fretum Gatitanum, Europe and Africa are separated by 7.7 nautical miles of ocean at the straits narrowest point. Ferries cross between the two every day in as little as 35 minutes. The Spanish side of the Strait is protected under El Estrecho Natural Park, on the northern side of the Strait are Spain and Gibraltar, while on the southern side are Morocco and Ceuta. Its boundaries were known in antiquity as the Pillars of Hercules, there are several islets, such as the disputed Isla Perejil, that are claimed by both Morocco and Spain. Due to its location, the Strait is commonly used for illegal immigration from Africa to Europe, the International Hydrographic Organization defines the limits of the Strait of Gibraltar as follows, On the West. A line joining Cape Trafalgar to Cape Spartel, a line joining Europa Point to P. Almina. The seabed of the Strait is composed of synorogenic Betic-Rif clayey flysch covered by Pliocene and/or Quaternary calcareous sediments, exposed bedrock surfaces, coarse sediments and local sand dunes attest to the strong bottom current conditions at the present time. The resultant accumulation of huge salt and mineral deposits about the Mediterranean basin are directly linked to this era. It is believed that this took a short time, by geological standards. The erosion produced by the incoming waters seems to be the cause for the present depth of the strait. The strait is expected to close again as the African Plate moves northward relative to the Eurasian Plate, for full articles on the history of the north Gibraltar shore, see History of Gibraltar or History of Spain. For the full article on the history of the south Gibraltar shore, evidence of the first human habitation of the area by Neanderthals dates back to 125,000 years ago. Archaeological evidence of Homo sapiens habitation of the dates back c.40,000 years. In that year, the last Muslim government north of the straits was overthrown by a Spanish force, the small British enclave of the city of Gibraltar presents a third cultural group found in the straits. This enclave was first established in 1704 and has since used by Britain to act as a surety for control of the sea lanes into
5.
Balearic Islands
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The Balearic Islands are an archipelago of Spain in the western Mediterranean Sea, near the eastern coast of the Iberian Peninsula. The four largest islands are Majorca, Minorca, Ibiza and Formentera, there are many minor islands and islets close to the larger islands, including Cabrera, Dragonera and SEspalmador. The islands have a Mediterranean climate, and the four islands are all popular tourist destinations. Ibiza in particular is known as a party destination, attracting many of the worlds most popular DJs to its nightclubs. The islands culture and cuisine are similar to that of the rest of Spain but have their own distinctive features, the archipelago forms an autonomous community and a province of Spain, with Palma de Mallorca as the capital. The 2007 Statute of Autonomy declares the Balearic Islands as one nationality of Spain, the co-official languages in the Balearic Islands are Catalan and Spanish. Though now a part of Spain, throughout history the Balearic Islands have been under the rule of a number of different kingdoms, the official name of the Balearic Islands in Catalan is Illes Balears, while in Spanish they are known as the Islas Baleares. The term Balearic derives from Greek, of the various theories on the origins of the two ancient Greek and Latin names for the islands—Gymnasiae and Baleares—classical sources provide two. According to the Lycophrons Alexandra verses, the islands were called Γυμνησίαι/Gymnesiae because its inhabitants were often nude, the Greek and Roman writers generally derive the name of the people from their skill as slingers, although Strabo regards the name as of Phoenician origin. He observed it was the Phoenician equivalent for lightly armoured soldiers the Greeks would have called γυμνῆτας/gymnetas, the root bal does point to a Phoenician origin, perhaps the islands were sacred to the god Baal and the resemblance to the Greek root ΒΑΛ is accidental. Indeed, it was usual Greek practice to assimilate local names into their own language, but the common Greek name of the islands is not Βαλεαρεῖς/Baleareis, but Γυμνησίαι/Gymnesiai. The former was the used by the natives, as well as by the Carthaginians and Romans. The Balearic Islands are on a platform called the Balearic Promontory. They are cut by a network of northwest to southeast faults, the main islands of the autonomous community are Majorca, Minorca, Ibiza and Formentera, all popular tourist destinations. Amongst the minor islands is Cabrera, the location of the Cabrera Archipelago Maritime-Terrestrial National Park, the islands can be further grouped, with Majorca, Minorca, and Cabrera as the Gymnesian Islands, and Ibiza and Formentera as the Pityusic Islands, also referred to as the Pityuses. Located in the middle of the Mediterranean Sea, the Balearic Islands unsurprisingly have typical mediterranean climates, the below-listed climatic data of the capital Palma is typical for the archipelago, with minor differences to other stations in Majorca, Ibiza and Menorca. Little is recorded on the earliest inhabitants of the islands, though many legends exist, the story, preserved by Lycophron, that certain shipwrecked Greek Boeotians were cast nude on the islands, was evidently invented to account for the name Gymnesiae. There is also a tradition that the islands were colonised by Rhodes after the Trojan War, the islands had a very mixed population, of whose habits several strange stories are told
6.
Atlantic Ocean
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The Atlantic Ocean is the second largest of the worlds oceans with a total area of about 106,460,000 square kilometres. It covers approximately 20 percent of the Earths surface and about 29 percent of its surface area. It separates the Old World from the New World, the Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Eurasia and Africa to the east, and the Americas to the west. The Equatorial Counter Current subdivides it into the North Atlantic Ocean, in contrast, the term Atlantic originally referred specifically to the Atlas Mountains in Morocco and the sea off the Strait of Gibraltar and the North African coast. The Greek word thalassa has been reused by scientists for the huge Panthalassa ocean that surrounded the supercontinent Pangaea hundreds of years ago. The term Aethiopian Ocean, derived from Ancient Ethiopia, was applied to the Southern Atlantic as late as the mid-19th century, many Irish or British people refer to the United States and Canada as across the pond, and vice versa. The Black Atlantic refers to the role of ocean in shaping black peoples history. Irish migration to the US is meant when the term The Green Atlantic is used, the term Red Atlantic has been used in reference to the Marxian concept of an Atlantic working class, as well as to the Atlantic experience of indigenous Americans. Correspondingly, the extent and number of oceans and seas varies, the Atlantic Ocean is bounded on the west by North and South America. It connects to the Arctic Ocean through the Denmark Strait, Greenland Sea, Norwegian Sea, to the east, the boundaries of the ocean proper are Europe, the Strait of Gibraltar and Africa. In the southeast, the Atlantic merges into the Indian Ocean, the 20° East meridian, running south from Cape Agulhas to Antarctica defines its border. In the 1953 definition it extends south to Antarctica, while in later maps it is bounded at the 60° parallel by the Southern Ocean, the Atlantic has irregular coasts indented by numerous bays, gulfs, and seas. Including these marginal seas the coast line of the Atlantic measures 111,866 km compared to 135,663 km for the Pacific. Including its marginal seas, the Atlantic covers an area of 106,460,000 km2 or 23. 5% of the ocean and has a volume of 310,410,900 km3 or 23. 3%. Excluding its marginal seas, the Atlantic covers 81,760,000 km2 and has a volume of 305,811,900 km3, the North Atlantic covers 41,490,000 km2 and the South Atlantic 40,270,000 km2. The average depth is 3,646 m and the maximum depth, the bathymetry of the Atlantic is dominated by a submarine mountain range called the Mid-Atlantic Ridge. It runs from 87°N or 300 km south of the North Pole to the subantarctic Bouvet Island at 42°S, the MAR divides the Atlantic longitudinally into two halves, in each of which a series of basins are delimited by secondary, transverse ridges. The MAR reaches above 2000 m along most of its length, the MAR is a barrier for bottom water, but at these two transform faults deep water currents can pass from one side to the other
7.
Caribbean Sea
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The Caribbean Sea is a sea of the Atlantic Ocean in the tropics of the Western Hemisphere. The entire area of the Caribbean Sea, the islands of the West Indies. The Caribbean Sea is one of the largest seas and has an area of about 2,754,000 km2, the seas deepest point is the Cayman Trough, between the Cayman Islands and Jamaica, at 7,686 m below sea level. The Caribbean coastline has many gulfs and bays, the Gulf of Gonâve, Gulf of Venezuela, Gulf of Darién, Golfo de los Mosquitos, Gulf of Paria, the Caribbean Sea has the worlds second biggest barrier reef, the Mesoamerican Barrier Reef. It runs 1,000 km along the coasts of Mexico, Belize, Guatemala, the name Caribbean derives from the Caribs, one of the regions dominant Native American groups at the time of European contact during the late 15th century. During the first century of development, Spanish dominance in the region remained undisputed, from the 16th century, Europeans visiting the Caribbean region identified the South Sea as opposed to the North Sea. The Caribbean Sea had been unknown to the populations of Eurasia until 1492, at that time the Western Hemisphere in general was unknown to Europeans. Following the discovery of the islands by Columbus, the area was colonised by several Western cultures. As of 2015 the area is home to 22 island territories, the International Hydrographic Organization defines the limits of the Caribbean Sea as follows, On the North. In the Windward Channel – a line joining Caleta Point and Pearl Point in Haïti, in the Mona Passage – a line joining Cape Engano and the extreme of Agujereada in Puerto Rico. From Galera Point through Trinidad to Galeota Point and thence to Baja Point in Venezuela, note that, although Barbados is an island on the same continental shelf, it is considered to be in the Atlantic Ocean rather than the Caribbean Sea. The Caribbean Sea is an oceanic sea largely situated on the Caribbean Plate, the Caribbean Sea is separated from the ocean by several island arcs of various ages. The youngest stretches from the Lesser Antilles to the Virgin Islands to the north east of Trinidad, the larger islands in the northern part of the sea Cuba, Hispaniola, Jamaica and Puerto Rico lie on an older island arc. The geological age of the Caribbean Sea is estimated to be between 160 and 180 million years and was formed by a fracture that split the supercontinent called Pangea in the Mesozoic Era. It is assumed the proto-caribbean basin existed in the Devonian period, in the early Carboniferous movement of Gondwana to the north and its convergence with the Euramerica basin decreased in size. The next stage of the Caribbean Seas formation began in the Triassic, powerful rifting led to the formation of narrow troughs, stretching from modern Newfoundland to the west coast of the Gulf of Mexico which formed siliciclastic sedimentary rocks. In the early Jurassic due to powerful marine transgression, water broke into the present area of the Gulf of Mexico creating a vast shallow pool, the emergence of deep basins in the Caribbean occurred during the Middle Jurassic rifting. The emergence of these marked the beginning of the Atlantic Ocean
8.
Treaty of Amiens
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The Treaty of Amiens temporarily ended hostilities between the French Republic and Great Britain during the French Revolutionary Wars. It was signed in the city of Amiens on 25 March 1802, by Joseph Bonaparte, the consequent Peace of Amiens lasted only one year and engendered the only period of general peace in Europe between 1793 and 1814. Under the treaty, Britain recognised the French Republic, the British parliament had dropped Englands historical claim to the now-defunct French Kingdom only two years previously. Together with the Treaty of Lunéville, the Treaty of Amiens marked the end of the Second Coalition, the War of the Second Coalition started well for the coalition, with successes in Egypt, Italy and Germany. After Frances victories at the Battles of Marengo and Hohenlinden, Austria, Russia and Naples sued for peace, horatio Nelsons victory at the Battle of Copenhagen on 2 April 1801 halted the creation of the League of Armed Neutrality and led to a negotiated ceasefire. The French First Consul, Napoleon Bonaparte, first made truce proposals to British foreign secretary Lord Grenville as early as 1799. Because of the stance of Grenville and Prime Minister William Pitt the Younger, their distrust of Bonaparte. However, Pitt resigned in February 1801 over domestic issues and was replaced by the more accommodating Henry Addington, at this point, according to Schroeder, Britain was motivated by the danger of a war with Russia. Hawkesbury stated that he wanted to open discussions on terms for a peace agreement, Otto, generally under detailed instructions from Bonaparte, engaged in negotiations with Hawkesbury in mid-1801. Unhappy with the dialogue with Otto, Hawkesbury sent diplomat Anthony Merry to Paris, by mid-September, written negotiations had progressed to the point where Hawkesbury and Otto met to draft a preliminary agreement. On 30 September, they signed the agreement in London. Malta was to be restored to the Order of St. John, France was to restore Egypt to Ottoman control, withdraw from most of the Italian peninsula and agree to preserve Portuguese sovereignty. Ceylon, previously a Dutch territory, was to remain with the British, Britain was also to recognise the Seven Islands Republic established by France on islands in the Ionian Sea that are now part of Greece. Both sides were to be allowed access to the outposts on the Cape of Good Hope, in a blow to Spain, the preliminary agreement included a secret clause in which Trinidad was to remain with Britain. News of the peace was greeted in Britain with illuminations. Peace, it was thought in Britain, would lead to the withdrawal of the tax imposed by Pitt, a reduction of grain prices. In November 1801, the Marquess Cornwallis was sent to France with plenipotentiary powers to negotiate a final agreement, the expectation among the British populace that peace was at hand put enormous pressure on Cornwallis, something Bonaparte realised and capitalised on. The Dutch role in the negotiations was marked by a lack of respect on the part of the French, schimmelpenninck and Cornwallis negotiated agreements on the status of Ceylon, the Cape of Good Hope, and the indemnification of the deposed House of Orange-Nassau for its losses
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