1.
Bronze
These additions produce a range of alloys that may be harder than copper alone, or have other useful properties, such as stiffness, ductility, or machinability. The archeological period where bronze was the hardest metal in use is known as the Bronze Age. In the ancient Near East this began with the rise of Sumer in the 4th millennium BC, with India and China starting to use bronze around the same time, everywhere it gradually spread across regions. The Bronze Age was followed by the Iron Age starting from about 1300 BC and reaching most of Eurasia by about 500 BC, the discovery of bronze enabled people to create metal objects which were harder and more durable than previously possible. Bronze tools, weapons and building such as decorative tiles were harder and more durable than their stone. It was only that tin was used, becoming the major ingredient of bronze in the late 3rd millennium BC. Tin bronze was superior to arsenic bronze in that the process could be more easily controlled. Also, unlike arsenic, metallic tin and fumes from tin refining are not toxic, the earliest tin-alloy bronze dates to 4500 BCE in a Vinča culture site in Pločnik.
Other early examples date to the late 4th millennium BC in Africa and some ancient sites in China, ores of copper and the far rarer tin are not often found together, so serious bronze work has always involved trade. Tin sources and trade in ancient times had a influence on the development of cultures. In Europe, a source of tin was the British deposits of ore in Cornwall. In many parts of the world, large hoards of bronze artefacts are found, suggesting that bronze represented a store of value, in Europe, large hoards of bronze tools, typically socketed axes, are found, which mostly show no signs of wear. With Chinese ritual bronzes, which are documented in the inscriptions they carry and from other sources and these were made in enormous quantities for elite burials, and used by the living for ritual offerings. Pure iron is soft, and the process of beating and folding sponge iron to wrought iron removes from the metal carbon. Careful control of the alloying and tempering eventually allowed for wrought iron with properties comparable to modern steel, Bronze was still used during the Iron Age, and has continued in use for many purposes to the modern day.
Among other advantages, it does not rust, the weaker wrought iron was found to be sufficiently strong for many uses. Archaeologists suspect that a disruption of the tin trade precipitated the transition. The population migrations around 1200–1100 BC reduced the shipping of tin around the Mediterranean, limiting supplies, there are many different bronze alloys, but typically modern bronze is 88% copper and 12% tin
2.
Granite
Granite is a common type of felsic intrusive igneous rock that is granular and phaneritic in texture. Granites can be white, pink, or gray in color. The word granite comes from the Latin granum, a grain, in reference to the structure of such a holocrystalline rock. By definition, granite is a rock with at least 20% quartz. The term granitic means granite-like and is applied to granite and a group of igneous rocks with similar textures and slight variations in composition. Occasionally some individual crystals are larger than the groundmass, in case the texture is known as porphyritic. A granitic rock with a texture is known as a granite porphyry. Granitoid is a general, 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, and therefore it has gained widespread use throughout human history, and more recently as a construction stone.
The average density of granite is between 2.65 and 2.75 g/cm3, its compressive strength usually lies above 200 MPa, and its viscosity near STP is 3–6 •1019 Pa·s. The melting temperature of dry granite at ambient pressure is 1215–1260 °C, it is reduced in the presence of water. Granite has poor primary permeability, but strong secondary permeability, true granite according to modern petrologic convention contains both plagioclase and 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 and amphibole are common in tonalite. A granite containing both muscovite and biotite micas is called a binary or two-mica granite, two-mica granites are typically high in potassium and low in plagioclase, and are usually S-type granites or A-type granites. A worldwide average of the composition of granite, by weight percent, based on 2485 analyses. Much of it was intruded during the Precambrian age, it is the most abundant basement rock that underlies the relatively thin veneer of the continents.
Outcrops of granite tend to form tors and rounded massifs, granites sometimes occur in circular depressions surrounded by a range of hills, formed by the metamorphic aureole or hornfels. Granite often occurs as small, less than 100 km² stock masses
3.
Limestone
Limestone is a sedimentary rock, composed mainly of skeletal fragments of marine organisms such as coral and molluscs. Its major materials are the minerals calcite and aragonite, which are different crystal forms of calcium carbonate, about 10% of sedimentary rocks are limestones. The solubility of limestone in water and weak acid solutions leads to karst landscapes, most cave systems are through limestone bedrock. The first geologist to distinguish limestone from dolomite was Belsazar Hacquet in 1778, like most other sedimentary rocks, most limestone is composed of grains. Most grains in limestone are skeletal fragments of organisms such as coral or foraminifera. Other carbonate grains comprising limestones are ooids, peloids and these organisms secrete shells made of aragonite or calcite, and leave these shells behind when they die. Limestone often contains variable amounts of silica in the form of chert or siliceous skeletal fragment, some limestones do not consist of grains at all, and are formed completely by the chemical precipitation of calcite or aragonite, i. e. travertine.
Secondary calcite may be deposited by supersaturated meteoric waters and this produces speleothems, such as stalagmites and stalactites. Another form taken by calcite is oolitic limestone, which can be recognized by its granular appearance, the primary source of the calcite in limestone is most commonly marine organisms. Some of these organisms can construct mounds of rock known as reefs, below about 3,000 meters, water pressure and temperature conditions cause the dissolution of calcite to increase nonlinearly, so limestone typically does not form in deeper waters. Limestones may form in lacustrine and evaporite depositional environments, calcite can be dissolved or precipitated by groundwater, depending on several factors, including the water temperature, pH, and dissolved ion concentrations. Calcite exhibits a characteristic called retrograde solubility, in which it becomes less soluble in water as the temperature increases. Impurities will cause limestones to exhibit different colors, especially with weathered surfaces, Limestone may be crystalline, granular, or massive, depending on the method of formation.
Crystals of calcite, dolomite or barite may line small cavities in the rock, when conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together, or it can fill fractures. Travertine is a banded, compact variety of limestone formed along streams, particularly there are waterfalls. Calcium carbonate is deposited where evaporation of the leaves a solution supersaturated with the chemical constituents of calcite. Tufa, a porous or cellular variety of travertine, is found near waterfalls, coquina is a poorly consolidated limestone composed of pieces of coral or shells. During regional metamorphism that occurs during the building process, limestone recrystallizes into marble
4.
J. Paul Getty Museum
The J. Paul Getty Museum, commonly referred to as the Getty, is an art museum in California housed on two campuses, the Getty Center and Getty Villa. The Getty Center is in the Brentwood neighborhood of Los Angeles and is the location of the museum. The collection features Western art from the Middle Ages to the present and its estimated 1.3 million visitors annually make it one of the most visited museums in the United States. The museums second location, the Getty Villa, is in the Pacific Palisades neighborhood and displays art from ancient Greece and Etruria. In 1974, J. Paul Getty opened a museum in a re-creation of the Villa of the Papyri at Herculaneum on his property in Pacific Palisades, in 1982, the museum became the richest in the world when it inherited US$1.2 billion. In 1997, the moved to its current location in the Brentwood neighborhood of Los Angeles. Detailed information about the J. Paul Getty Museum’s collections is provided on GettyGuide, at the GettyGuide stations in the Museum, visitors can get information about exhibitions, interact with a timeline, watch videos on art-making techniques, and more.
Also available at the Museum, the GettyGuide multimedia player features commentary from curators and conservators on many works of art, with GettyGuide on the Web, one may browse the Museum’s collection and bookmark works of art to create a customized tour and printable map. In 1984, Frel was demoted, and in 1986, he resigned, the Getty is involved in a controversy regarding proper title to some of the artwork in its collection. The museums previous curator of antiquities, Marion True, was indicted in Italy in 2005 on criminal charges relating to trafficking in stolen antiquities, similar charges have been addressed by the Greek authorities. The primary evidence in the case came from the 1995 raid of a Geneva, Switzerland, in 2005 True was forced to tender her resignation by the Board of Trustees, which announced her early retirement. Italy allowed the statute of limitations of the charges filed against her to expire in October 2010, True is currently under investigation by Greek authorities over the acquisition of a 2, 500-year-old funerary wreath.
The wreath, along with a 6th-century BC statue of a woman, have returned to Greece and are exhibited at the Archaeological Museum of Thessaloniki. The Getty Museum resisted the requests of the Italian government for two decades, only to admit that there might be problems attached to the acquisition. In 2006, Italian senior cultural official Giuseppe Proietti said, The negotiations havent made a step forward. Only after he suggested the Italian government to take cultural sanctions against the Getty, suspending all cultural cooperation, in another unrelated case in 1999, the Getty Museum had to hand over three antiquities to Italy after determining they were stolen. A Summary Catalogue of European Decorative Arts in the J. Paul Getty Museum was published in 2001, some discrete works are provided with annotations, e. g. In 2016, the head of the Greek god Hades was returned to Sicily
5.
Hellenistic Greece
During the Hellenistic period the importance of Greece proper within the Greek-speaking world declined sharply. The great centers of Hellenistic culture were Alexandria and Antioch, capitals of Ptolemaic Egypt, cities such as Pergamon, Ephesus and Seleucia were important, and increasing urbanization of the Eastern Mediterranean was characteristic of the time. The quests of Alexander had a number of consequences for the Greek city-states and it greatly widened the horizons of the Greeks, making the endless conflicts between the cities which had marked the 5th and 4th centuries BC seem petty and unimportant. It led to a steady emigration, particularly of the young and ambitious, the Greeks valued their local independence too much to consider actual unification, but they made several attempts to form federations through which they could hope to reassert their independence. Following Alexanders death a struggle for power broke out among his generals, which resulted in the break-up of his empire, Macedon fell to Cassander, son of Alexanders leading general Antipater, who after several years of warfare made himself master of most of the rest of Greece.
He founded a new Macedonian capital at Thessaloniki and was generally a constructive ruler, Cassanders power was challenged by Antigonus, ruler of Anatolia, who promised the Greek cities that he would restore their freedom if they supported him. This led to successful revolts against Cassanders local rulers, in 307 BC, Antigonuss son Demetrius captured Athens and restored its democratic system, which had been suppressed by Alexander. But in 301 BC a coalition of Cassander and the other Hellenistic kings defeated Antigonus at the Battle of Ipsus, after Cassanders death in 298 BC, Demetrius seized the Macedonian throne and gained control of most of Greece. He was defeated by a coalition of Greek rulers in 285 BC. Lysimachus was in turn defeated and killed in 280 BC, the Macedonian throne passed to Demetriuss son Antigonus II, who defeated an invasion of the Greek lands by the Gauls, who at this time were living in the Balkans. The battle against the Gauls united the Antigonids of Macedon and the Seleucids of Antioch, an alliance which was directed against the wealthiest Hellenistic power.
Antigonus II ruled until his death in 239 BC, and his family retained the Macedonian throne until it was abolished by the Romans in 146 BC. Their control over the Greek city states was intermittent, since other rulers, particularly the Ptolemies, Sparta remained independent, but generally refused to join any league. In 267 BC, Ptolemy II persuaded the Greek cities to revolt against Antigonus, in became the Chremonidian War. The cities were defeated and Athens lost her independence and her democratic institutions, the Aetolian League was restricted to the Peloponnese, but on being allowed to gain control of Thebes in 245 BC became a Macedonian ally. This marked the end of Athens as a actor, although it remained the largest and most cultivated city in Greece. In 255 BC, Antigonus defeated the Egyptian fleet at Cos and brought the Aegean islands, except Rhodes, in spite of their decreased political power and autonomy, the Greek city state or polis continued to be the basic form of political and social organization in Greece.
Classical city states such as Athens and Ephesus grew and even thrived in this period, the Aetolians and the Achaeans developed strong federal states or leagues, which were governed by councils of city representatives and assemblies of league citizens
6.
Calcite
Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate. The Mohs scale of hardness, based on scratch hardness comparison. Other polymorphs of calcium carbonate are the minerals aragonite and vaterite, aragonite will change to calcite at 380–470 °C, and vaterite is even less stable. Calcite is derived from the German Calcit, a term coined in the 19th century from the Latin word for lime and it is thus etymologically related to chalk. Calcite crystals are trigonal-rhombohedral, though actual calcite rhombohedra are rare as natural crystals, they show a remarkable variety of habits including acute to obtuse rhombohedra, tabular forms, prisms, or various scalenohedra. Calcite exhibits several twinning types adding to the variety of observed forms and it may occur as fibrous, lamellar, or compact. Cleavage is usually in three directions parallel to the rhombohedron form and its fracture is conchoidal, but difficult to obtain. It has a defining Mohs hardness of 3, a gravity of 2.71.
Color is white or none, though shades of gray, orange, green, violet, calcite is transparent to opaque and may occasionally show phosphorescence or fluorescence. A transparent variety called Iceland spar is used for optical purposes, acute scalenohedral crystals are sometimes referred to as dogtooth spar while the rhombohedral form is sometimes referred to as nailhead spar. Single calcite crystals display an optical property called birefringence and this strong birefringence causes objects viewed through a clear piece of calcite to appear doubled. The birefringent effect was first described by the Danish scientist Rasmus Bartholin in 1669, at a wavelength of ~590 nm calcite has ordinary and extraordinary refractive indices of 1.658 and 1.486, respectively. Between 190 and 1700 nm, the refractive index varies roughly between 1.9 and 1.5, while the extraordinary refractive index varies between 1.6 and 1.4. Calcite, like most carbonates, will dissolve with most forms of acid, calcite can be either dissolved by groundwater or precipitated by groundwater, depending on several factors including the water temperature, pH, and dissolved ion concentrations.
Although calcite is fairly insoluble in water, acidity can cause dissolution of calcite. Ambient carbon dioxide, due to its acidity, has a slight solubilizing effect on calcite, calcite exhibits an unusual characteristic called retrograde solubility in which it becomes less soluble in water as the temperature increases. When conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together or it can fill fractures. On a landscape scale, continued dissolution of calcium carbonate-rich rocks can lead to the expansion and eventual collapse of cave systems, high-grade optical calcite was used in World War II for gun sights, specifically in bomb sights and anti-aircraft weaponry
7.
Acid rain
Acid rain is a rain or any other form of precipitation that is unusually acidic, meaning that it possesses elevated levels of hydrogen ions. It can have effects on plants, aquatic animals and infrastructure. Acid rain is caused by emissions of sulfur dioxide and nitrogen oxide, some governments have made efforts since the 1970s to reduce the release of sulfur dioxide and nitrogen oxide into the atmosphere with positive results. Nitrogen oxides can be produced naturally by lightning strikes, Acid rain is a popular term referring to the deposition of a mixture from wet and dry acidic components. Distilled water, once carbon dioxide is removed, has a neutral pH of 7, liquids with a pH less than 7 are acidic, and those with a pH greater than 7 are alkaline. Clean or unpolluted rain has an acidic pH, but usually no lower than 5, a common example is nitric acid produced by electric discharge in the atmosphere such as lightning. Acid deposition as an issue would include additional acids other than H2CO3.
The corrosive effect of polluted, acidic city air on limestone and marble was noted in the 17th century by John Evelyn, since the Industrial Revolution, emissions of sulfur dioxide and nitrogen oxides into the atmosphere have increased. In 1852, Robert Angus Smith was the first to show the relationship between rain and atmospheric pollution in Manchester, England. Though acidic rain was discovered in 1853, it was not until the late 1960s that scientists began widely observing and studying the phenomenon, the term acid rain was coined in 1872 by Robert Angus Smith. Canadian Harold Harvey was among the first to research a dead lake, occasional pH readings in rain and fog water of well below 2.4 have been reported in industrialized areas. Industrial acid rain is a problem in China and Russia. These areas all burn sulfur-containing coal to heat and electricity. The problem of acid rain has not only increased with population and industrial growth, the use of tall smokestacks to reduce local pollution has contributed to the spread of acid rain by releasing gases into regional atmospheric circulation.
Often deposition occurs a considerable distance downwind of the emissions, with mountainous regions tending to receive the greatest deposition, an example of this effect is the low pH of rain which falls in Scandinavia. The earliest report about acid rain in the United States was from the evidence from Hubbard Brook Valley. In 1972, a group of scientists including Gene Likens discovered the rain that was deposited at White Mountains of New Hampshire was acidic, the pH of the sample was measured to be 4.03 at Hubbard Brook. The Hubbard Brook Ecosystem Study followed up with a series of research that analyzed the effects of acid rain
8.
Jackhammer
A jackhammer is a pneumatic or electro-mechanical tool that combines a hammer directly with a chisel. It was invented by William Mcreavy, who sold the patent to Charles Brady King. Hand-held jackhammers are generally powered by compressed air, but some are powered by electric motors. Larger jackhammers, such as rig mounted hammers used on machinery, are usually hydraulically powered. They are typically used to break up rock, pavement, a jackhammer operates by driving an internal hammer up and down. The hammer is first driven down to strike the back and back up to return the hammer to the position to repeat the cycle. The effectiveness of the jackhammer is dependent on how much force is applied to the tool and it is generally used like a hammer to break the hard surface or rock in construction works and it is not consider under earth moving equipment, along with its accessories. In British English, electromechanical versions are known as Kangos. Pneumatic drills were developed in response to the needs of mining, excavating, in 1838 Isaac Singer invented a steam driven drill.
A pneumatic drill was proposed by a C, the first percussion drill was made in 1848 and patented in 1849 by Jonathan J. Couch of Philadelphia, Pennsylvania. In this drill, the drill bit passed through the piston of a steam engine, the piston snagged the drill bit and hurled it against the rock face. In 1849, Couchs assistant, Joseph W. Fowle, filed a patent caveat for a drill of his own design. In Fowle’s drill, the bit was connected directly to the piston in the steam cylinder, specifically. The drill had a mechanism for turning the drill bit around its axis between strokes and for advancing the drill as the hole deepened, by 1850 or 1851, Fowle was using compressed air to drive his drill, making it the first true pneumatic drill. By contrast, compressed air could be conveyed over distances without loss of its energy. The need for a rock drill was obvious and this sparked research on pneumatic rock drills in Europe. A Frenchman, Cavé, and in 1851 patented, a drill that used compressed air. In 1854, in England, Thomas Bartlett made and patented a rock drill whose drill bit was connected directly to the piston of a steam engine, in 1855 Bartlett demonstrated his drill, powered by compressed air, to officials of the Mt.
Fréjus tunnel project
9.
National Roman Museum
The National Roman Museum is a museum, with several branches in separate buildings throughout the city of Rome, Italy. Founded in 1889 and inaugurated in 1890, the museums first aim was to collect, the collection was appropriated by the state in 1874, after the suppression of the Society of Jesus. Renamed initially as the Royal Museum, the collection was intended to be moved to a Museo Tiberino, in 1901 the State granted the National Roman Museum the recently acquired Collection Ludovisi as well as the important national collection of Ancient Sculpture. Findings during the renewal of the late 19th century added to the collections. The palace was built on the site occupied by the Villa Montalto-Peretti, named after Pope Sixtus V. The present building was commissioned by Prince Massimiliano Massimo, so as to give a seat to the Jesuit Collegio Romano, originally within the convent of the church of SantIgnazio. In 1871, the Collegio had been ousted from the convent by the State which converted it into the Liceo Visconti, erected between 1883 and 1887 by the architect Camillo Pistrucci in a neo-cinquecentesco style, it was one of the most prestigious schools of Rome until 1960.
During World War II, it was used as a military hospital, but it returned to scholastic functions until the 60s. In 1981, lying in a state of neglect, the Italian State acquired it for 19 billion lire, the museum houses the Ancient Art as well as the Numismatic Collection, housed in the Medagliere, i. e. the Coin Cabinet. One room is devoted to the mummy that was found in 1964 on the Via Cassia, inside a richly decorated sarcophagus with several artefacts in amber. It begins with the triclinium of Livias Villa “ad Gallinas Albas”. The frescoes, discovered in 1863 and dating back to the 1st century BC, show a garden with ornamental plants. The Museums numismatic collection is the largest in Italy, among the coins on exhibit are Theodoric’s medallion, the four ducats of Pope Paul II with the navicella of St Peter, and the silver piastre of the Pontifical State with views of the city of Rome. The Palazzo Altemps is located in the modern rione Ponte, part of the Campus Martius, in the ancient Rome, this site was only 160 meters from the Ponte Elio, and was one of the two main marble ports on the Tiber River in Rome.
The other was located in what is now Testaccio, in 1891, during the construction works to build the embankments that now hold back the Tiber River, the remains of this dock were uncovered. A few of these ancient shops bear signs of hasty abandonment after the time of the emperor Trajan, there was likely a temple to Apollo located in this area, over which has been built the church of SantApollinare. The division was abandoned after the Great Schism in the 15th century. The building was designed in the 15th century by Melozzo da Forlì for Girolamo Riario, when the Soderini family fell on hard times, he in turn sold it in 1568 to the Austrian-born cardinal Mark Sittich von Hohenems Altemps, the son of the sister of Pope Pius IV
10.
Ancient Rome
In its many centuries of existence, the Roman state evolved from a monarchy to a classical republic and to an increasingly autocratic empire. Through conquest and assimilation, it came to dominate the Mediterranean region and Western Europe, Asia Minor, North Africa and it is often grouped into classical antiquity together with ancient Greece, and their similar cultures and societies are known as the Greco-Roman world. Ancient Roman civilisation has contributed to modern government, politics, art, architecture, warfare, religion and society. Rome professionalised and expanded its military and created a system of government called res publica, the inspiration for modern republics such as the United States and France. By the end of the Republic, Rome had conquered the lands around the Mediterranean and beyond, its domain extended from the Atlantic to Arabia, the Roman Empire emerged with the end of the Republic and the dictatorship of Augustus Caesar. 721 years of Roman-Persian Wars started in 92 BC with their first war against Parthia and it would become the longest conflict in human history, and have major lasting effects and consequences for both empires.
Under Trajan, the Empire reached its territorial peak, Republican mores and traditions started to decline during the imperial period, with civil wars becoming a prelude common to the rise of a new emperor. Splinter states, such as the Palmyrene Empire, would divide the Empire during the crisis of the 3rd century. Plagued by internal instability and attacked by various migrating peoples, the part of the empire broke up into independent kingdoms in the 5th century. This splintering is a landmark historians use to divide the ancient period of history from the pre-medieval Dark Ages of Europe. King Numitor was deposed from his throne by his brother, while Numitors daughter, Rhea Silvia, because Rhea Silvia was raped and impregnated by Mars, the Roman god of war, the twins were considered half-divine. The new king, feared Romulus and Remus would take back the throne, a she-wolf saved and raised them, and when they were old enough, they returned the throne of Alba Longa to Numitor. Romulus became the source of the citys name, in order to attract people to the city, Rome became a sanctuary for the indigent and unwanted.
This caused a problem for Rome, which had a large workforce but was bereft of women, Romulus traveled to the neighboring towns and tribes and attempted to secure marriage rights, but as Rome was so full of undesirables they all refused. Legend says that the Latins invited the Sabines to a festival and stole their unmarried maidens, leading to the integration of the Latins, after a long time in rough seas, they landed at the banks of the Tiber River. Not long after they landed, the men wanted to take to the sea again, one woman, named Roma, suggested that the women burn the ships out at sea to prevent them from leaving. At first, the men were angry with Roma, but they realized that they were in the ideal place to settle. They named the settlement after the woman who torched their ships, the Roman poet Virgil recounted this legend in his classical epic poem the Aeneid
11.
Louvre
The Louvre or the Louvre Museum is the worlds largest museum and a historic monument in Paris, France. A central landmark of the city, it is located on the Right Bank of the Seine in the citys 1st arrondissement, approximately 38,000 objects from prehistory to the 21st century are exhibited over an area of 72,735 square metres. The Louvre is the second most visited museum after the Palace Museum in China. The museum is housed in the Louvre Palace, originally built as a fortress in the late 12th century under Philip II, remnants of the fortress are visible in the basement of the museum. Due to the expansion of the city, the fortress eventually lost its defensive function and. The building was extended many times to form the present Louvre Palace, in 1692, the building was occupied by the Académie des Inscriptions et Belles Lettres and the Académie Royale de Peinture et de Sculpture, which in 1699 held the first of a series of salons. The Académie remained at the Louvre for 100 years, during the French Revolution, the National Assembly decreed that the Louvre should be used as a museum to display the nations masterpieces.
The museum opened on 10 August 1793 with an exhibition of 537 paintings, because of structural problems with the building, the museum was closed in 1796 until 1801. The collection was increased under Napoleon and the museum renamed Musée Napoléon, the collection was further increased during the reigns of Louis XVIII and Charles X, and during the Second French Empire the museum gained 20,000 pieces. Holdings have grown steadily through donations and bequests since the Third Republic, whether this was the first building on that spot is not known, it is possible that Philip modified an existing tower. According to the authoritative Grand Larousse encyclopédique, the name derives from an association with wolf hunting den, in the 7th century, St. Fare, an abbess in Meaux, left part of her Villa called Luvra situated in the region of Paris to a monastery. This territory probably did not correspond exactly to the modern site, the Louvre Palace was altered frequently throughout the Middle Ages. In the 14th century, Charles V converted the building into a residence and in 1546, Francis acquired what would become the nucleus of the Louvres holdings, his acquisitions including Leonardo da Vincis Mona Lisa.
After Louis XIV chose Versailles as his residence in 1682, constructions slowed, however, on 14 October 1750, Louis XV agreed and sanctioned a display of 96 pieces from the royal collection, mounted in the Galerie royale de peinture of the Luxembourg Palace. Under Louis XVI, the museum idea became policy. The comte dAngiviller broadened the collection and in 1776 proposed conversion of the Grande Galerie of the Louvre – which contained maps – into the French Museum, many proposals were offered for the Louvres renovation into a museum, none was agreed on. Hence the museum remained incomplete until the French Revolution, during the French Revolution the Louvre was transformed into a public museum. In May 1791, the Assembly declared that the Louvre would be a place for bringing together monuments of all the sciences, on 10 August 1792, Louis XVI was imprisoned and the royal collection in the Louvre became national property
12.
Michelangelo
Michelangelo di Lodovico Buonarroti Simoni was an Italian sculptor, painter and poet of the High Renaissance who exerted an unparalleled influence on the development of Western art. Considered to be the greatest living artist during his lifetime, he has since described as one of the greatest artists of all time. A number of Michelangelos works of painting and architecture rank among the most famous in existence and he sculpted two of his best-known works, the Pietà and David, before the age of thirty. As an architect, Michelangelo pioneered the Mannerist style at the Laurentian Library, at the age of 74, he succeeded Antonio da Sangallo the Younger as the architect of St. Peters Basilica. Michelangelo transformed the plan so that the end was finished to his design, as was the dome, with some modification. Michelangelo was unique as the first Western artist whose biography was published while he was alive, in his lifetime he was often called Il Divino. One of the qualities most admired by his contemporaries was his terribilità, the attempts by subsequent artists to imitate Michelangelos impassioned and highly personal style resulted in Mannerism, the next major movement in Western art after the High Renaissance.
Michelangelo was born on 6 March 1475 in Caprese near Arezzo, at the time of Michelangelos birth, his father was the Judicial administrator of the small town of Caprese and local administrator of Chiusi. Michelangelos mother was Francesca di Neri del Miniato di Siena, the Buonarrotis claimed to descend from the Countess Mathilde of Canossa, this claim remains unproven, but Michelangelo himself believed it. Several months after Michelangelos birth, the returned to Florence. There Michelangelo gained his love for marble, as Giorgio Vasari quotes him, If there is good in me. Along with the milk of my nurse I received the knack of handling chisel and hammer, as a young boy, Michelangelo was sent to Florence to study grammar under the Humanist Francesco da Urbino. The young artist, showed no interest in his schooling, preferring to copy paintings from churches, the city of Florence was at that time the greatest centre of the arts and learning in Italy. Art was sponsored by the Signoria, by the merchant guilds and by patrons such as the Medici.
The Renaissance, a renewal of Classical scholarship and the arts, had its first flowering in Florence, the sculptor Lorenzo Ghiberti had laboured for fifty years to create the bronze doors of the Baptistry, which Michelangelo was to describe as The Gates of Paradise. The exterior niches of the Church of Orsanmichele contained a gallery of works by the most acclaimed sculptors of Florence – Donatello, Andrea del Verrocchio, and Nanni di Banco. The interiors of the churches were covered with frescos, begun by Giotto. During Michelangelos childhood, a team of painters had been called from Florence to the Vatican, among them was Domenico Ghirlandaio, a master in fresco painting, figure drawing, and portraiture who had the largest workshop in Florence at that period
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