Automobiles Ettore Bugatti was a French car manufacturer of high-performance automobiles, founded in 1909 in the then-German city of Molsheim, Alsace by the Italian-born industrial designer Ettore Bugatti. The cars were known for their many race victories. Famous Bugattis include the Type 35 Grand Prix cars, the Type 41 "Royale", the Type 57 "Atlantic" and the Type 55 sports car; the death of Ettore Bugatti in 1947 proved to be the end for the marque, the death of his son Jean Bugatti in 1939 ensured there was not a successor to lead the factory. No more than about 8,000 cars were made; the company struggled financially, released one last model in the 1950s, before being purchased for its airplane parts business in 1963. In the 1990s, an Italian entrepreneur revived it as a builder of limited production exclusive sports cars. Today, the name is owned by the Volkswagen Group. Founder Ettore Bugatti was born in Milan and the automobile company that bears his name was founded in 1909 in Molsheim located in the Alsace region, part of the German Empire from 1871 to 1919.
The company was known both for the level of detail of its engineering in its automobiles, for the artistic manner in which the designs were executed, given the artistic nature of Ettore's family. During the war Ettore Bugatti was sent away to Milan and to Paris, but as soon as hostilities had been concluded he returned to his factory at Molsheim. Less than four months after the Versailles Treaty formalised the transfer of Alsace from Germany to France, Bugatti was able to obtain, at the last minute, a stand at the 15th Paris motor show in October 1919, he exhibited three light cars, all of them based on their pre-war equivalents, each fitted with the same overhead camshaft 4-cylinder 1,368cc engine with four valves per cylinder. Smallest of the three was a "Type 13" with a racing body and using a chassis with a 2,000 mm wheelbase; the others were a "Type 22" and a "Type 23" with wheelbases of 2,400 mm respectively. The company enjoyed great success in early Grand Prix motor racing: in 1929 a entered Bugatti won the first Monaco Grand Prix.
Racing success culminated with driver Jean-Pierre Wimille winning the 24 hours of Le Mans twice. Bugatti cars were successful in racing; the little Bugatti Type 10 swept the top four positions at its first race. The 1924 Bugatti Type 35 is one of the most successful racing cars; the Type 35 was developed by Bugatti with master engineer and racing driver Jean Chassagne who drove it in the car’s first Grand Prix in 1924 Lyon. Bugattis swept to victory in the Targa Florio for five years straight from 1925 through 1929. Louis Chiron held the most podiums in Bugatti cars, the modern marque revival Bugatti Automobiles S. A. S. named the 1999 Bugatti 18/3 Chiron concept car in his honour. But it was the final racing success at Le Mans, most remembered—Jean-Pierre Wimille and Pierre Veyron won the 1939 race with just one car and meagre resources. In the 1930s, Ettore Bugatti got involved in the creation of a racer airplane, hoping to beat the Germans in the Deutsch de la Meurthe prize; this would be the Bugatti 100P.
It was designed by Belgian engineer Louis de Monge who had applied Bugatti Brescia engines in his "Type 7.5" lifting body. Ettore Bugatti designed a successful motorised railcar, the Autorail Bugatti; the death of Ettore Bugatti's son, Jean Bugatti, on 11 August 1939 marked a turning point in the company's fortunes. Jean died. World War II left the Molsheim factory in the company lost control of the property. During the war, Bugatti planned a new factory at a northwestern suburb of Paris. After the war, Bugatti designed and planned to build a series of new cars, including the Type 73 road car and Type 73C single seat racing car, but in all Bugatti built only five Type 73 cars. Development of a 375 cc supercharged car was stopped when Ettore Bugatti died on 21 August 1947. Following Ettore Bugatti's death, the business declined further and made its last appearance as a business in its own right at a Paris Motor Show in October 1952. After a long decline, the original incarnation of Bugatti ceased operations in 1952.
Bugattis are noticeably focused on design. Engine blocks were hand scraped to ensure that the surfaces were so flat that gaskets were not required for sealing, many of the exposed surfaces of the engine compartment featured guilloché finishes on them, safety wires had been threaded through every fastener in intricately laced patterns. Rather than bolt the springs to the axles as most manufacturers did, Bugatti's axles were forged such that the spring passed through a sized opening in the axle, a much more elegant solution requiring fewer parts, he famously described his arch competitor Bentley's cars as "the world's fastest lorries" for focusing on durability. According to Bugatti, "weight was the enemy". Relatives of Harold Carr found a rare 1937 Bugatti Type 57S Atalante when cataloguing the doctor's belongings after his death in 2009. Carr's Type 57S is notable because it was owned by British race car driver Earl Howe; because much of the car's original equipment is intact, it can be restored without relying on replacement parts.
On 10 July 2009, a 1925 Bugatti Brescia Type 22 which had lain at the bottom of Lake Maggiore on the border of Switzerland and Italy for 75 years was recovered from the lake. The Mullin Mu
Tuscany is a region in central Italy with an area of about 23,000 square kilometres and a population of about 3.8 million inhabitants. The regional capital is Florence. Tuscany is known for its landscapes, artistic legacy, its influence on high culture, it is regarded as the birthplace of the Italian Renaissance and has been home to many figures influential in the history of art and science, contains well-known museums such as the Uffizi and the Pitti Palace. Tuscany produces wines, including Chianti, Vino Nobile di Montepulciano, Morellino di Scansano and Brunello di Montalcino. Having a strong linguistic and cultural identity, it is sometimes considered "a nation within a nation". Tuscany is a popular destination in Italy, the main tourist spots are Florence, Lucca, Versilia and Chianti; the village of Castiglione della Pescaia is the most visited seaside destination in the region, with seaside tourism accounting for 40% of tourist arrivals. Additionally, Lucca, the Chianti region and Val d'Orcia are internationally renowned and popular spots among travellers.
Seven Tuscan localities have been designated World Heritage Sites: the historic centre of Florence. Tuscany has over 120 protected nature reserves, making Tuscany and its capital Florence popular tourist destinations that attract millions of tourists every year. In 2012, the city of Florence was the world's 89th most visited city, with over 1.834 million arrivals. Triangular in shape, Tuscany borders the regions of Liguria to the northwest, Emilia-Romagna to the north, Marche to the northeast, Umbria to the east and Lazio to the southeast; the comune of Badia Tedalda, in the Tuscan Province of Arezzo, has an exclave named Ca' Raffaello within Emilia-Romagna. Tuscany has a western coastline on the Ligurian Sea and the Tyrrhenian Sea, among, the Tuscan Archipelago, of which the largest island is Elba. Tuscany has an area of 22,993 square kilometres. Surrounded and crossed by major mountain chains, with few plains, the region has a relief, dominated by hilly country used for agriculture. Hills make up nearly two-thirds of the region's total area, covering 15,292 square kilometres, mountains, a further 25%, or 5,770 square kilometres.
Plains occupy 8.4% of the total area—1,930 square kilometres —mostly around the valley of the Arno. Many of Tuscany's largest cities lie on the banks of the Arno, including the capital Florence and Pisa; the climate is mild in the coastal areas, is harsher and rainy in the interior, with considerable fluctuations in temperature between winter and summer, giving the region a soil-building active freeze-thaw cycle, in part accounting for the region's once having served as a key breadbasket of ancient Rome. The pre-Etruscan history of the area in the late Bronze and Iron Ages parallels that of the early Greeks; the Tuscan area was inhabited by peoples of the so-called Apennine culture in the late second millennium BC who had trading relationships with the Minoan and Mycenaean civilizations in the Aegean Sea. Following this, the Villanovan culture saw Tuscany, the rest of Etruria, taken over by chiefdoms. City-states developed in the late Villanovan before "Orientalization" occurred and the Etruscan civilization rose.
The Etruscans created the first major civilization in this region, large enough to establish a transport infrastructure, to implement agriculture and mining and to produce vibrant art. The Etruscans lived in the area of Etruria well into prehistory; the civilization grew to fill the area between the Arno and Tiber from the eighth century BCE, reaching its peak during the seventh and sixth centuries B. C. succumbing to the Romans by the first century BCE. Throughout their existence, they lost territory to Magna Graecia and Celts. Despite being seen as distinct in its manners and customs by contemporary Greeks, the cultures of Greece, Rome, influenced the civilization to a great extent. One reason for its eventual demise was this increasing absorption by surrounding cultures, including the adoption of the Etruscan upper class by the Romans. Soon after absorbing Etruria, Rome established the cities of Lucca, Pisa and Florence, endowed the area with new technologies and development, ensured peace.
These developments included extensions of existing roads, introduction of aqueducts and sewers, the construction of many buildings, both public and private. However, many of these structures have been destroyed by erosion due to weather; the Roman civilization in the West of the Roman Republic and Roman Empire collapsed in the fifth century, the region fell to barbarians migrating through the Empire from Eastern Europe and Central Asia of the Goths was re-conquered by the revived Eastern Roman Empire under the strong Emperor Justinian. In the years following 572, the Lombards arrived and designated Lucca the capital of their subsequent Tuscia. Pilgrims travelling along the Via Francigena between Rome and France brought wealth and development during the medieval period; the food and shelter required by the
Italy the Italian Republic, is a country in Southern Europe. Located in the middle of the Mediterranean Sea, Italy shares open land borders with France, Austria and the enclaved microstates San Marino and Vatican City. Italy covers an area of 301,340 km2 and has a temperate seasonal and Mediterranean climate. With around 61 million inhabitants, it is the fourth-most populous EU member state and the most populous country in Southern Europe. Due to its central geographic location in Southern Europe and the Mediterranean, Italy has been home to a myriad of peoples and cultures. In addition to the various ancient peoples dispersed throughout modern-day Italy, the most famous of which being the Indo-European Italics who gave the peninsula its name, beginning from the classical era and Carthaginians founded colonies in insular Italy and Genoa, Greeks established settlements in the so-called Magna Graecia, while Etruscans and Celts inhabited central and northern Italy respectively; the Italic tribe known as the Latins formed the Roman Kingdom in the 8th century BC, which became a republic with a government of the Senate and the People.
The Roman Republic conquered and assimilated its neighbours on the peninsula, in some cases through the establishment of federations, the Republic expanded and conquered parts of Europe, North Africa and the Middle East. By the first century BC, the Roman Empire emerged as the dominant power in the Mediterranean Basin and became the leading cultural and religious centre of Western civilisation, inaugurating the Pax Romana, a period of more than 200 years during which Italy's technology, economy and literature flourished. Italy remained the metropole of the Roman Empire; the legacy of the Roman Empire endured its fall and can be observed in the global distribution of culture, governments and the Latin script. During the Early Middle Ages, Italy endured sociopolitical collapse and barbarian invasions, but by the 11th century, numerous rival city-states and maritime republics in the northern and central regions of Italy, rose to great prosperity through shipping and banking, laying the groundwork for modern capitalism.
These independent statelets served as Europe's main trading hubs with Asia and the Near East enjoying a greater degree of democracy than the larger feudal monarchies that were consolidating throughout Europe. The Renaissance began in Italy and spread to the rest of Europe, bringing a renewed interest in humanism, science and art. Italian culture flourished, producing famous scholars and polymaths such as Michelangelo, Leonardo da Vinci, Raphael and Machiavelli. During the Middle Ages, Italian explorers such as Marco Polo, Christopher Columbus, Amerigo Vespucci, John Cabot and Giovanni da Verrazzano discovered new routes to the Far East and the New World, helping to usher in the European Age of Discovery. Italy's commercial and political power waned with the opening of trade routes that bypassed the Mediterranean. Centuries of infighting between the Italian city-states, such as the Italian Wars of the 15th and 16th centuries, left the region fragmented, it was subsequently conquered and further divided by European powers such as France and Austria.
By the mid-19th century, rising Italian nationalism and calls for independence from foreign control led to a period of revolutionary political upheaval. After centuries of foreign domination and political division, Italy was entirely unified in 1871, establishing the Kingdom of Italy as a great power. From the late 19th century to the early 20th century, Italy industrialised, namely in the north, acquired a colonial empire, while the south remained impoverished and excluded from industrialisation, fuelling a large and influential diaspora. Despite being one of the main victors in World War I, Italy entered a period of economic crisis and social turmoil, leading to the rise of a fascist dictatorship in 1922. Participation in World War II on the Axis side ended in military defeat, economic destruction and the Italian Civil War. Following the liberation of Italy and the rise of the resistance, the country abolished the monarchy, reinstated democracy, enjoyed a prolonged economic boom and, despite periods of sociopolitical turmoil became a developed country.
Today, Italy is considered to be one of the world's most culturally and economically advanced countries, with the sixth-largest worldwide national wealth. Its advanced economy ranks eighth-largest in the world and third in the Eurozone by nominal GDP. Italy owns the third-largest central bank gold reserve, it has a high level of human development, it stands among the top countries for life expectancy. The country plays a prominent role in regional and global economic, military and diplomatic affairs. Italy is a founding and leading member of the European Union and a member of numerous international institutions, including the UN, NATO, the OECD, the OSCE, the WTO, the G7, the G20, the Union for the Mediterranean, the Council of Europe, Uniting for Consensus, the Schengen Area and many more; as a reflection
Granite is a common type of felsic intrusive igneous rock, granular and phaneritic in texture. Granites can be predominantly white, pink, or gray depending on their mineralogy; the word "granite" comes from the Latin granum, a grain, in reference to the coarse-grained structure of such a holocrystalline rock. Speaking, granite is an igneous rock with between 20% and 60% quartz by volume, at least 35% of the total feldspar consisting of alkali feldspar, although the term "granite" is used to refer to a wider range of coarse-grained igneous rocks containing quartz and feldspar; the term "granitic" means granite-like and is applied to granite and a group of intrusive igneous rocks with similar textures and slight variations in composition and origin. These rocks consist of feldspar, quartz and amphibole minerals, which form an interlocking, somewhat equigranular matrix of feldspar and quartz with scattered darker biotite mica and amphibole peppering the lighter color minerals; some individual crystals are larger than the groundmass, in which case the texture is known as porphyritic.
A granitic rock with a porphyritic texture is known as a granite porphyry. Granitoid is a descriptive field term for lighter-colored, coarse-grained igneous rocks. Petrographic examination is required for identification of specific types of granitoids; the extrusive igneous rock equivalent of granite is rhyolite. Granite is nearly always massive and tough; these properties have made granite a widespread construction stone throughout human history. The average density of granite is between 2.65 and 2.75 g/cm3, its compressive strength lies above 200 MPa, its viscosity near STP is 3–6·1019 Pa·s. The melting temperature of dry granite at ambient pressure is 1215–1260 °C. Granite has poor primary permeability overall, but strong secondary permeability through cracks and fractures if they are present. Granite is classified according to the QAPF diagram for coarse grained plutonic rocks and is named according to the percentage of quartz, alkali feldspar and plagioclase feldspar on the A-Q-P half of the diagram.
True granite contains both alkali feldspars. When a granitoid is devoid or nearly devoid of plagioclase, the rock is referred to as alkali feldspar granite; when a granitoid contains less than 10% orthoclase, it is called tonalite. A granite containing both muscovite and biotite micas is called two-mica granite. Two-mica granites are high in potassium and low in plagioclase, are S-type granites or A-type granites. A worldwide average of the chemical composition of granite, by weight percent, based on 2485 analyses: Granite containing rock is distributed throughout the continental crust. Much of it was intruded during the Precambrian age. Outcrops of granite tend to form rounded massifs. Granites sometimes occur in circular depressions surrounded by a range of hills, formed by the metamorphic aureole or hornfels. Granite occurs as small, less than 100 km2 stock masses and in batholiths that are associated with orogenic mountain ranges. Small dikes of granitic composition called aplites are associated with the margins of granitic intrusions.
In some locations coarse-grained pegmatite masses occur with granite. Granite is more common in continental crust than in oceanic crust, they are crystallized from felsic melts which are less dense than mafic rocks and thus tend to ascend toward the surface. In contrast, mafic rocks, either basalts or gabbros, once metamorphosed at eclogite facies, tend to sink into the mantle beneath the Moho. Granitoids have crystallized from felsic magmas that have compositions near a eutectic point. Magmas are composed of minerals in variable abundances. Traditionally, magmatic minerals are crystallized from the melts that have separated from their parental rocks and thus are evolved because of igneous differentiation. If a granite has a cooling process, it has the potential to form larger crystals. There are peritectic and residual minerals in granitic magmas. Peritectic minerals are generated through peritectic reactions, whereas residual minerals are inherited from parental rocks. In either case, magmas will evolve to the eutectic for crystallization upon cooling.
Anatectic melts are produced by peritectic reactions, but they are much less evolved than magmatic melts because they have not separated from their parental rocks. The composition of anatectic melts may change toward the magmatic melts through high-degree fractional crystallization. Fractional crystallisation serves to reduce a melt in iron, titanium and sodium, enrich the melt in potassium and silicon – alkali feldspar and quartz, are two of the defining constituents of granite; this process operates regardless of the origin of parental magmas to granites, regardless of their chemistry. The composition and origin of any magma that differentiates into granite leave certain petrological evidence as to what the granite's parental rock was; the final texture and composition of a granite are distinctive as to its parental rock. For instance, a granite, derived from partial melting of meta
The Nuragic civilization known as the Nuragic culture was a civilization or culture on the island of Sardinia, the second largest island in the Mediterranean Sea, which lasted from the 18th century BCE to 238 BCE when the Romans colonized the island. Others date the culture as lasting at least until the 2nd century CE or even to the 6th century CE; the adjective "Nuragic" derives from the island's most characteristic monument, the nuraghe, a tower-fortress type of construction the ancient Sardinians built in large numbers starting from about 1800 BCE. Today more than 7,000 nuraghes dot the Sardinian landscape. No written records of this civilization have been discovered, apart from a few possible short epigraphic documents belonging to the last stages of the Nuragic civilization; the only written information there comes from classical literature of the Greeks and Romans, may be considered more mythological than historical. In the Stone Age the island was first inhabited by people who had arrived there in the Paleolithic and Neolithic ages from Europe and the Mediterranean area.
The most ancient settlements have been discovered both in northern Sardinia. Several cultures developed on the island, such as the Ozieri culture; the economy was based on agriculture, animal husbandry and trading with the mainland. With the diffusion of metallurgy and copper objects and weapons appeared on the island. Remains from this period include hundreds of menhirs and dolmens, more than 2,400 hypogeum tombs called domus de Janas, the statue menhirs, representing warriors or female figures, the stepped pyramid of Monte d'Accoddi, near Sassari, which show some similarities with the monumental complex of Los Millares and the talaiots in the Balearic Islands. According to some scholars, the similarity between this structure and those found in Mesopotamia are due to cultural influxes coming from the Eastern Mediterranean; the altar of Monte d'Accoddi fell out of use starting from c. 2000 BCE, when the Beaker culture, which at the time was widespread in all western Europe, appeared on the island.
The beakers arrived in Sardinia from two different regions: firstly from Spain and southern France, secondly from Central Europe, through the Italian Peninsula. The Bonnanaro culture was the last evolution of the Beaker culture in Sardinia, displayed several similarities with the contemporary Polada culture of northern Italy; these two cultures shared common features in the material culture such as undecorated pottery with axe-shaped handles. These influences may have spread to Sardinia via Corsica, where they absorbed new architectural techniques that were widespread on the island. New peoples coming from the mainland arrived on the island at that time, bringing with them new religious philosophies, new technologies and new ways of life, making obsolete the previous ones or reinterpreting them, it is in virtue of stimuli and models from the Central European and Polada-Rhone areas, that the culture of Bonnanaro I gives a jolt to the known and produces in step with the times. From the severe, practical character and essentiality of the material equipment, we understand the nature and the warlike habit of the newcomers and the conflictual thrust that they give to life on the island.
This is confirmed by the presence of metal weapons. The metal spreads in objects of use, ornamental objects It seems to feel a fall of ideologies of the old pre-nuragic world corresponding to a new historical turning point The widespread diffusion of bronze brought numerous improvements. With the new alloy of copper and tin, or arsenic, a harder and more resistant metal was obtained, suitable for manufacturing tools used in agriculture and warfare. From this period dates the construction of the so-called proto-nuraghe, a platformlike structure that marks the first phase of the Nuragic Age; these buildings are different from the classical nuraghe having an irregular planimetry and a stocky appearance. Dating to the middle of the 2nd millennium BCE, the nuraghe, which evolved from the previous proto-nuraghe, are megalithic towers with a truncated cone shape, they are widespread in the whole of Sardinia, about one nuraghe every three square kilometers. Early Greek historians and geographers speculated about their builders.
They described the presence of fabulous edifices, called daidaleia, from the name of Daedalus, after building his labyrinth in Crete, would have moved to Sicily and to Sardinia. Modern theories about their use have included social, religious, or astronomical roles, as furnaces, or as tombs. Although the question has long been contentious among scholars, the modern consensus is that they were built as defensible homesites, that included barns and silos. In the second half of the 2nd millennium BCE, archaeological studies have proved the increasing size of the settlements built around some of these structures, which were located at the summit of hills. For protection reasons, new towers were added to the original ones, connected by walls provided with slits forming a complex nuraghe. Among the most famous of the numerous existing nuraghe, are the Su Nuraxi at Barumini, Santu Antine at Torralba, Nuraghe Losa at Abbasanta, Nuraghe Palmavera at Alghero, Nuraghe Genna Maria at Villanovaforru, Nuraghe
Sardinia is the second-largest island in the Mediterranean Sea. It is located west of the Italian Peninsula and to the immediate south of the French island of Corsica. Sardinia is politically a region of Italy, whose official name is Regione Autonoma della Sardegna / Regione Autònoma de Sardigna, enjoys some degree of domestic autonomy granted by a specific Statute, it is divided into four provinces and a metropolitan city, with Cagliari being the region's capital and its largest city. Sardinia's indigenous language and the other minority languages spoken on the island are recognized by the regional law and enjoy "equal dignity" with Italian. Due to the variety of its ecosystems, which include mountains, plains uninhabited territories, rocky coasts and long sandy beaches, the island has been defined metaphorically as a micro-continent. In the modern era, many travelers and writers have extolled the beauty of its untouched landscape, which houses the vestiges of the Nuragic civilization; the name Sardinia is from the pre-Roman noun *srd- romanised as sardus.
It makes its first appearance on the Nora Stone, where the word Šrdn testifies to the name's existence when the Phoenician merchants first arrived. According to Timaeus, one of Plato's dialogues and its people as well might have been named after a legendary woman going by Sardò, born in Sardis, capital of the ancient Kingdom of Lydia. There has been speculation that identifies the ancient Nuragic Sards with the Sherden, one of the Sea Peoples, it is suggested that the name had a religious connotation from its use as the adjective for the ancient Sardinian mythological hero-god Sardus Pater, as well as being the stem of the adjective "sardonic". In Classical antiquity, Sardinia was called a number of names besides Sardò or Sardinia, like Ichnusa and Argirofleps. Sardinia is the second-largest island in the Mediterranean Sea, with an area of 24,100 square kilometres, it is situated between 8 ° 8' and 9 ° 50' east longitude. To the west of Sardinia is the Sea of Sardinia, a unit of the Mediterranean Sea.
The nearest land masses are the island of Corsica, the Italian Peninsula, Tunisia, the Balearic Islands, Provence. The Tyrrhenian Sea portion of the Mediterranean Sea is directly to the east of Sardinia between the Sardinian east coast and the west coast of the Italian mainland peninsula; the Strait of Bonifacio is directly north of Sardinia and separates Sardinia from the French island of Corsica. The coasts of Sardinia are high and rocky, with long straight stretches of coastline, many outstanding headlands, a few wide, deep bays, many inlets and with various smaller islands off the coast; the island has an ancient geoformation and, unlike Sicily and mainland Italy, is not earthquake-prone. Its rocks date in fact from the Palaeozoic Era. Due to long erosion processes, the island's highlands, formed of granite, trachyte, basalt and dolomite limestone, average at between 300 to 1,000 metres; the highest peak is part of the Gennargentu Ranges in the centre of the island. Other mountain chains are Monte Limbara in the northeast, the Chain of Marghine and Goceano running crosswise for 40 kilometres towards the north, the Monte Albo, the Sette Fratelli Range in the southeast, the Sulcis Mountains and the Monte Linas.
The island's ranges and plateaux are separated by wide alluvial valleys and flatlands, the main ones being the Campidano in the southwest between Oristano and Cagliari and the Nurra in the northwest. Sardinia has few major rivers, the largest being the Tirso, 151 km long, which flows into the Sea of Sardinia, the Coghinas and the Flumendosa. There are 54 artificial dams that supply water and electricity; the main ones are Lake Coghinas. The only natural freshwater lake is Lago di Baratz. A number of large, salt-water lagoons and pools are located along the 1,850 km of the coastline; the climate of the island is variable from area to area, due to several factors including the extension in latitude and the elevation. It can be classified in two different macrobioclimates, one macrobioclimatic variant, called Submediterranean, four classes of continentality, eight thermotypic horizons and seven ombrotypic horizons, resulting in a combination of 43 different isobioclimates. During the year there is a major concentration
North Africa is a region encompassing the northern portion of the African continent. There is no singularly accepted scope for the region, it is sometimes defined as stretching from the Atlantic shores of Morocco in the west, to Egypt's Suez Canal and the Red Sea in the east. Others have limited it to top North-Western countries like Algeria and Tunisia, a region, known by the French during colonial times as "Afrique du Nord" and is known by all Arabs as the Maghreb; the most accepted definition includes Algeria, Morocco, Tunisia and Egypt, the 6 countries that shape the top North of the African continent. Meanwhile, "North Africa" when used in the term North Africa and the Middle East refers only to the countries of the Maghreb and Libya. Egypt, being part of the Middle East, is considered separately, due to being both North African and Middle Eastern at the same time. North Africa includes a number of Spanish and Portuguese possessions, Plazas de soberanía, Ceuta and Melilla and the Canary Islands and Madeira.
The countries of North Africa share a common ethnic and linguistic identity, unique to this region. Northwest Africa has been inhabited by Berbers since the beginning of recorded history, while the eastern part of North Africa has been home to the Egyptians. Between the A. D. 600s and 1000s, Arabs from the Middle East swept across the region in a wave of Muslim conquest. These peoples, physically quite similar, formed a single population in many areas, as Berbers and Egyptians merged into Arabic and Muslim culture; this process of Arabization and Islamization has defined the cultural landscape of North Africa since. The distinction between North Africa, the Sahel and the rest of the continent is as follows: Nineteenth century European explorers, attracted by the accounts of Ancient geographers or Arab geographers of the classical period, followed the routes by the nomadic people of the vast "empty" space, they documented the names of the stopping places they discovered or rediscovered, described landscapes, took a few climate measurements and gathered rock samples.
A map began to fill in the white blotch. The Sahara and the Sahel entered the geographic corpus by way of naturalist explorers because aridity is the feature that circumscribes the boundaries of the ecumene; the map details included topographical relief and location of watering holes crucial to long crossings. The Arabic word "Sahel" and "Sahara" made its entry into the vocabulary of geography. Latitudinally, the "slopes" of the arid desert, devoid of continuous human habitation, descend in step-like fashion toward the northern and southern edges of the Mediterranean that opens to Europe and the Sahel that opens to "Trab al Sudan." Longitudinally, a uniform grid divides the central desert shrinks back toward the Atlantic Ocean and the Red Sea. The Sahara-Sahel is further divided into a total of twenty sub-areas: central, southern, eastern, etc. In this way, "standard" geography has determined aridity to be the boundary of the ecumene, it identifies settlements based on visible activity without regard for social or political organizations of space in vast, purportedly “empty” areas.
It gives only cursory acknowledgement to what makes Saharan geography, for that matter, world geography unique: mobility and the routes by which it flows. The Sahel or "African Transition Zone" has been affected by many formative epochs in North African history ranging from Ottoman occupation to the Arab-Berber control of the Andalus; as a result, many modern African nation-states that are included in the Sahel evidence cultural similarities and historical overlap with their North African neighbours. In the present day, North Africa is associated with West Asia in the realm of geopolitics to form a Middle East-North Africa region; the Islamic influence in the area is significant and North Africa is a major part of the Muslim world. Some researchers have postulated that North Africa rather than East Africa served as the exit point for the modern humans who first trekked out of the continent in the Out of Africa migration. North Africa has three main geographic features: the Sahara desert in the south, the Atlas Mountains in the west, the Nile River and delta in the east.
The Atlas Mountains extend across much of northern Algeria and Tunisia. These mountains are part of the fold mountain system that runs through much of Southern Europe, they recede to the south and east, becoming a steppe landscape before meeting the Sahara desert, which covers more than 75 percent of the region. The tallest peaks are in the High Atlas range in south-central Morocco, which has many snow-capped peaks. South of the Atlas Mountains is the dry and barren expanse of the Sahara desert, the largest sand desert in the world. In places the desert is cut by irregular watercourses called wadis—streams that flow only after rainfalls but are dry; the Sahara's major landforms include large seas of sand that sometimes form into huge dunes. The Sahara covers the southern part of Algeria and Tunisia, most of Libya. Only two regions of Libya are outside the desert: Tripolitania in the northwest and Cyrenaica in the northeast. Most of Egypt is desert, with the exception of the Nile River and the irrigated land along its banks.
The Nile Valley forms a narrow fertile thread. Sheltered valleys in the Atlas Mountains, the Nile Valley and Delta, the Mediterranean coast are the main sources of fertile farming land. A wide variety of valuable crops including ce