1.
Su Nuraxi (Barumini)
–
Su Nuraxi is a nuragic archaeological site in Barumini, Sardinia, Italy. It was included in the UNESCO list of World Heritage Sites in 1997 as Su Nuraxi di Barumini, Su Nuraxi simply means The Nuraghe in Campidanese, the southern variant of the Sardinian language. They are considered by scholars the most impressive expression of the Nuragic civilization and were included in the UNESCO list of World Heritage Sites in 1997. The oldest part of the Nuraghe consists of a tower with three superposed chambers, was built in blocks of basalt between the seventeenth and thirteenth centuries BCE. Later, during the Late Bronze Age, four towers joined by a wall with an upper balcony were built around the central tower. During the Iron Age, the complex was surrounded by a wall with seven lobes. The real function of the nuraghe is still debated, the discoverer of Su Nuraxi, the archaeologist Giovanni Lilliu, confirmed the traditional interpretation of fortress-site. A village, intended to accommodate the population, was built around the Nuraghe in the Late Bronze Age. The village consisted of fifty huts, and was built on a circular plan with large boulders covered with dry stone walls and conical roofs made of wood. Though the huts were structured in a unit in more remote periods, there was a later. Of the huts found, the most significant appear to have reserved for meetings of the local leaders. These huts were larger and more complex in structure, and the hut reserved for the inhabitants meetings contained symbols of the deities worshiped by locals, other rooms have been identified as workshops, kitchens, and agricultural processing centres. During the sixth century BCE, the buildings were destroyed and subsequently restored by Carthage before being occupied by the Romans. The nuraghe and the village were connected to the system of other Nuraghes. The archaeological site was excavated between 1950 and 1957 under the direction of Giovanni Lilliu, a local expert. Excavations brought to light important remains in the form of tools, weapons, pottery, Giovanni Lilliu used a combination of structural phases and pottery typology to construct a general Nuragic sequence. There is another important nuragic site at nearby Casa Zapata, the important finds of which are on display at the sites museum. Dyson Stephen L. Rowland Robert J. Shepherds, sailors, & conquerors - Archeology, philadelphia, University of Pennsylvania, Museum of Archeology and Anthropology
2.
Megalith
–
A megalith is a large stone that has been used to construct a structure or monument, either alone or together with other stones. The word megalithic describes structures made of large stones without the use of mortar or concrete. For later periods, the monolith, with an overlapping meaning, is more likely to be used. The word megalith comes from the Ancient Greek μέγας and λίθος, megalith also denotes an item consisting of rock hewn in definite shapes for special purposes. It has been used to describe buildings built by people from parts of the world living in many different periods. A variety of stones are seen as megaliths, with the most widely known megaliths not being sepulchral. The construction of these took place mainly in the Neolithic and continued into the Chalcolithic. At a number of sites in eastern Turkey, large ceremonial complexes from the 9th millennium BC have been discovered and they belong to the incipient phases of agriculture and animal husbandry. Large circular structures involving carved megalithic orthostats are a feature, e. g. at Nevalı Çori. Although these structures are the most ancient megalithic structures known so far, at Göbekli Tepe, four stone circles have been excavated from an estimated 20. Some measure up to 30 metres across, as well as human figures, the stones carry a variety of carved reliefs depicting boars, foxes, lions, birds, snakes and scorpions. Dolmens and standing stones have been found in areas of the Middle East starting at the Turkish border in the north of Syria close to Aleppo. They can be encountered in Lebanon, Syria, Iran, Israel, Jordan, the largest concentration can be found in southern Syria and along the Jordan Rift Valley, however they are being threatened with destruction. They date from the late Chalcolithic/Early Bronze Age, megaliths have also been found on Kharg Island and pirazmian in Iran, at Barda Balka in Iraq, and at Jaintapur in Bangladesh. A semicircular arrangement of megaliths was found in Israel at Atlit Yam and it is a very early example, dating from the 7th millennium BC. The most concentrated occurrence of dolmens in particular is in an area on both sides of the Jordan Rift Valley, with greater predominance on the eastern side. They occur first and foremost on the Golan Heights, the Hauran, and in Jordan, in Saudi Arabia, only very few dolmen have been identified so far in the Hejaz. They seem, however, to re-emerge in Yemen in small numbers, the standing stone has a very ancient tradition in the Middle East, dating back from Mesopotamian times
3.
Sardinia
–
Sardinia is the second largest island in the Mediterranean Sea and an autonomous region of Italy. It is located in the Western Mediterranean, just south of the French island of Corsica, the regions official name is Regione Autonoma della Sardegna / Regione Autònoma de Sardigna, and its capital and largest city is Cagliari. It is divided into four provinces and a metropolitan city and its indigenous language and the other minority languages spoken by the Sardinians enjoy equal dignity with Italian under regional law. The name Sardinia is from the pre-Roman noun *srd-, later romanised as sardus and it makes its first appearance on the Nora Stone, where the word Šrdn testifies to the names existence when the Phoenician merchants first arrived. According to Timaeus, one of Platos dialogues, Sardinia and its people as well might have named after Sardò. There has also been speculation that identifies the ancient Nuragic Sards with the Sherden, in Classical antiquity, Sardinia was called Ichnusa, Σανδάλιον Sandal, Sardinia and Sardó. Sardinia is the second-largest island in the Mediterranean Sea, with an area of 24,100 square kilometres and it is situated between 38°51 and 41°18 latitude north and 8°8 and 9°50 east longitude. To the west of Sardinia is the Sea of Sardinia, a unit of the Mediterranean Sea, to Sardinias east is the Tyrrhenian Sea, the nearest land masses are the island of Corsica, the Italian Peninsula, Sicily, Tunisia, the Balearic Islands, and 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 island has an ancient geoformation and, unlike Sicily and mainland Italy, is not earthquake-prone and its rocks date in fact from the Palaeozoic Era. Due to long erosion processes, the highlands, formed of granite, schist, trachyte, basalt, sandstone and dolomite limestone. The highest peak is Punta La Marmora, part of the Gennargentu Ranges in the centre of the island. The islands ranges and plateaux are separated by wide valleys and flatlands. Sardinia has few rivers, the largest being the Tirso,151 km long, which flows into the Sea of Sardinia, the Coghinas. There are 54 artificial lakes and dams that supply water and electricity, the main ones are Lake Omodeo and Lake Coghinas. The only natural lake is Lago di Baratz. A number of large, shallow, 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. During the year there is a concentration of rainfall in the winter and autumn, some heavy showers in the spring
4.
Oxford English Dictionary
–
The Oxford English Dictionary is a descriptive dictionary of the English language, published by the Oxford University Press. The second edition came to 21,728 pages in 20 volumes, in 1895, the title The Oxford English Dictionary was first used unofficially on the covers of the series, and in 1928 the full dictionary was republished in ten bound volumes. In 1933, the title The Oxford English Dictionary fully replaced the name in all occurrences in its reprinting as twelve volumes with a one-volume supplement. More supplements came over the years until 1989, when the edition was published. Since 2000, an edition of the dictionary has been underway. The first electronic version of the dictionary was available in 1988. The online version has been available since 2000, and as of April 2014 was receiving two million hits per month. The third edition of the dictionary will probably appear in electronic form, Nigel Portwood, chief executive of Oxford University Press. As a historical dictionary, the Oxford English Dictionary explains words by showing their development rather than merely their present-day usages, therefore, it shows definitions in the order that the sense of the word began being used, including word meanings which are no longer used. The format of the OEDs entries has influenced numerous other historical lexicography projects and this influenced later volumes of this and other lexicographical works. As of 30 November 2005, the Oxford English Dictionary contained approximately 301,100 main entries, the dictionarys latest, complete print edition was printed in 20 volumes, comprising 291,500 entries in 21,730 pages. The longest entry in the OED2 was for the verb set, as entries began to be revised for the OED3 in sequence starting from M, the longest entry became make in 2000, then put in 2007, then run in 2011. Despite its impressive size, the OED is neither the worlds largest nor the earliest exhaustive dictionary of a language, the Dutch dictionary Woordenboek der Nederlandsche Taal is the worlds largest dictionary, has similar aims to the OED and took twice as long to complete. Another earlier large dictionary is the Grimm brothers dictionary of the German language, begun in 1838, the official dictionary of Spanish is the Diccionario de la lengua española, and its first edition was published in 1780. The Kangxi dictionary of Chinese was published in 1716, trench suggested that a new, truly comprehensive dictionary was needed. On 7 January 1858, the Society formally adopted the idea of a new dictionary. Volunteer readers would be assigned particular books, copying passages illustrating word usage onto quotation slips, later the same year, the Society agreed to the project in principle, with the title A New English Dictionary on Historical Principles. He withdrew and Herbert Coleridge became the first editor, on 12 May 1860, Coleridges dictionary plan was published and research was started
5.
Iberians
–
The Iberians were a set of peoples that Greek and Roman sources identified with that name in the eastern and southern coasts of the Iberian peninsula, at least from the 6th century BC. The Roman sources also use the term Hispani to refer to the Iberians, the term Iberian, as used by the ancient authors, had two distinct meanings. One, more general, referred to all the populations of the Iberian peninsula without regard to ethnic differences and this non-Indo-European cultural group spoke the Iberian language from the 7th to the 1st century BC. Other peoples possibly related to the Iberians are the Vascones, though related to the Aquitani than to the Iberians. The Iberian culture developed from the 6th century BC, and perhaps as early as the fifth to the third millennium BC in the eastern and southern coasts of the Iberian peninsula, the Iberians lived in villages and oppida and their communities were based on a tribal organization. The Iberians in the Spanish Levant, were more urbanized than their neighbors in the central, the peoples in the central and northwest regions were mostly Celtic, semi-pastoral and lived in scattered villages, though they also had a few fortified towns like Numantia. They had a knowledge of writing, metalworking, including bronze, in the centuries preceding Carthaginian and Roman conquest, Iberian settlements grew in social complexity, exhibiting evidence of social stratification and urbanization. This process was aided by trading contacts with the Phoenicians, Greeks. The settlement of Castellet de Banyoles in Tivissa was one of the most important ancient Iberian settlements in Catalonia that was discovered in 1912, also, the Treasure of Tivissa, a unique collection of silver Iberian votive offerings was found here in 1927. Lucentum was another ancient Iberian settlement, as well as Castelldefels Castle, mausoleum of Pozo Moro near the town of Chinchilla de Monte-Aragón in Castile-La Mancha seems to mark the location of another big settlement. Sagunto is the location of an ancient Iberian and later Roman city of Saguntum, Greek colonists made the first historical reference to the Iberians in the 6th century BC. They defined Iberians as non-Celtic peoples south of the Ebro river, the Greeks also dubbed as Iberians another people in the Caucasus region, currently known as Caucasian Iberians. It is not known if there had any type of connection between the two peoples. The Iberians traded extensively with other Mediterranean cultures, Iberian pottery and metalwork has been found in France, Italy, and North Africa. The Iberians had extensive contact with Greek colonists in the Spanish colonies of Emporion, Rhode, Zakynthos, the Iberians may have adopted some of the Greeks artistic techniques. Statues such as the Lady of Baza and the Lady of Elx are thought to have made by Iberians relatively well acquainted with Greek art. Thucydides stated that one of the three tribes of Sicily, the Sicani, were of Iberian origin, though Iberian at the time could have included what we think of as Gaul. The Iberians also had contacts with the Phoenicians, who had established colonies in southern Andalucia
6.
Alluvium
–
Alluvium is loose, unconsolidated soil or sediments, which has been eroded, reshaped by water in some form, and redeposited in a non-marine setting. Alluvium is typically made up of a variety of materials, including fine particles of silt and clay and larger particles of sand, when this loose alluvial material is deposited or cemented into a lithological unit, or lithified, it is called an alluvial deposit. The term alluvium is not typically used in situations where the formation of the sediment can clearly be attributed to another process that is well described. This includes, lake sediments, river sediments, or glacially-derived sediments, sediments that are formed or deposited in a perennial stream or river are typically not referred to as alluvial. Most alluvium is very young, and is often referred to as cover because these sediments obscure the underlying bedrock. Most sedimentary material that fills a basin that is not lithified is typically lumped together as alluvial, alluvium of Pliocene age occurs, for example, in parts of Idaho. Alluvium of late Miocene age occurs, for example, in the valley of the San Joaquin River, alluvium can contain valuable ores such as gold and platinum and a wide variety of gemstones. Such a concentration of ores is termed a placer deposit
7.
Corbel arch
–
A corbel vault uses this technique to support the superstructure of a buildings roof. For a corbeled vault covering the technique is extended in three dimensions along the lengths of two opposing walls, unlike true arches, not all of the structures tensile stresses caused by the weight of the superstructure are transformed into compressive stresses. The Newgrange passage tomb has a corbel arch supporting the roof of the main chamber. Egyptian pyramids from around the time of Sneferu used corbel vaults in some of their chambers and these include the Bent Pyramid and the Red Pyramid. Corbel arches and vaults are found in places around the ancient Mediterranean. In particular, corbelled burial vaults constructed below the floor are found in Ebla in Syria, and in Tel Hazor, nuraghe constructions in ancient Sardinia, dating back to 1900 BC, use similar corbel techniques. The use of Beehive tombs on the Iberian peninsula and elsewhere around the Mediterranean, the Hittites in ancient Anatolia were also building corbelled vaults. The earliest ones date to the 16th century BC, some similarities are found between the Hittite and Mycenaean construction techniques. Yet the Hittite corbelled vaults are earlier by about 300 years, the ruins of ancient Mycenae feature many corbel arches and vaults, the Treasury of Atreus being a prominent example. Dating to the Greek Bronze Age, it is one of the oldest arch bridges still in existence, the well-preserved hellenistic Eleutherna Bridge on Crete has an unusually large span of nearly 4 m. Corbeled arches are a feature of certain pre-Columbian Mesoamerican constructions and historical/regional architectural styles. By the beginning of the Classic era corbeled vaults are a feature of building construction in the central Petén Basin region of the central Maya lowlands. Before the true arch was introduced by the Mughals, the arches in Indian buildings were trabeated or corbelled, the tomb of Sultan Ghari is an example of a corbelled arch from 1231 AD, located in New Delhi, India. The candi or temples of Indonesia which are constructed between 8th to 15th century, are made use of corbel arch technique to create an opening for gate or inner chamber of the temple. The notable example of corbel arch in Indonesian classic temple architecture is the arches of Borobudur, the interlocking andesite stone blocks creating the corbel arch, is notable for its T formed lock on the center top of the corbel arch. All the temples in Angkor made use of the corbel arch, Beehive house Beehive tomb Catenary arch Corbelling Parabolic arch Coe, Michael D. An illustrated glossary of the terms used masonry construction
8.
Beehive tomb
–
A beehive tomb, also known as a tholos tomb, is a burial structure characterized by its false dome created by the superposition of successively smaller rings of mudbricks or, more often, stones. The resulting structure resembles a beehive, hence the traditional English name, tholoi were used for burial in several cultures in the Mediterranean and West Asia, but in some cases they were used for different purposes such as homes, ritual, and even fortification. Although Max Mallowan used the name for the circular houses belonging to the Neolithic culture of Tell Halaf. In Greece, the vaulted tholoi are a monumental Late Bronze Age development, in concept, they are similar to the much more numerous Mycenaean chamber tombs which seem to have emerged at about the same time. Both have chamber, doorway stomion and entrance passage dromos but tholoi are largely built while chamber tombs are rock-cut, a few early examples of tholoi have been found in Messenia in the SW Peloponnese Greece, and recently near Troezen in the NE Peloponnese. These tholoi are built on ground and then enclosed by a mound of earth. A pair of tumuli at Marathon, Greece indicate how a built rectangular central chamber was extended with an entrance passage, after about 1500 BCE, beehive tombs became more widespread and are found in every part of the Mycenaean heartland. In contrast, however, to the early examples these are almost always cut into the slope of a hillside so that only the third of the vaulted chamber was above ground level. This masonry was then concealed with a small mound of earth. The tombs usually contain more than one burial, in places in the tomb either on the floor, in pits and cists or on stone-built or rock-cut benches. After a burial, the entrance to the tomb was filled in with soil, the chamber is always built in masonry, even in the earliest examples, as is the stomion or entrance-way. The dromos in early examples was usually just cut from the bedrock, in later examples such as the Treasury of Atreus and Tomb of Clytemnestra, all three parts were constructed of fine ashlar masonry. The chambers were built as corbelled vaults, with layers of stone placed closer together as the vault tapers toward the top of the tomb, the entrances provided an opportunity for conspicuous demonstration of wealth. That of the Treasury of Atreus, for example, was decorated with columns of red, the larger tombs contained amongst the richest finds to have come from the Late Bronze Age of Mainland Greece, despite the tombs having been pillaged both in antiquity and more recently. Although the Vapheio tholos, south of Sparta, had been robbed and these contained, among other valuable items, the two gold “Vapheio cups” decorated with scenes of bull taming which are among the best known of Mycenaean treasures. Circular structures were built in the Near East, including the examples known as tholoi found in the Neolithic Halaf culture of Iraq, Syria. They were probably used as houses and as storage structures, but ritual use may also have occurred. Other, later examples are found in Cyprus, where they were used as homes, there is no clear connection between these domestic, circular buildings and later tholos tombs
9.
City-state
–
A city-state is a sovereign state that consists of a city and its dependent territories. A great deal of consensus exists that the term applies to Singapore, Monaco. A number of small states share similar characteristics, and therefore are sometimes also cited as modern city-states. Occasionally, other states with high population densities, such as San Marino, are also cited. Several non-sovereign cities enjoy a degree of autonomy, and are sometimes considered city-states. Hong Kong and Macau, along with independent members of the United Arab Emirates, most notably Dubai, scholars have classed the Viking colonial cities in medieval Ireland, most importantly Dublin, as city-states. In Cyprus, the Phoenician settlement of Kition was a city-state that existed from around 800 BC until the end of the 4th century BC. The success of regional units coexisting as autonomous actors in loose geographical and cultural unity, as in Italy and Greece. However, such small political entities often survived only for short periods because they lacked the resources to defend themselves against incursions by larger states, thus they inevitably gave way to larger organisations of society, including the empire and the nation-state. In the history of Mainland Southeast Asia, aristocratic groups, Buddhist leaders, the system existed until the 19th century when colonization by European powers, and Thailands resulted in the adoption of the modern concept of statehood. In the Holy Roman Empire the Free Imperial Cities enjoyed a considerable autonomy, some, like the three Hanseatic cities of Bremen, Hamburg and Lübeck, pooled their economic relations with foreign powers and were able to wield considerable diplomatic clout. Under Habsburg rule the city of Fiume had the status of a Corpus separatum, a later city-state, though lacking sovereignty, was West Berlin, being a state legally not belonging to any other state, but ruled by the Western Allies. They allowed – notwithstanding their overlordship as occupant powers – its internal organisation as one state simultaneously being a city, though West Berlin maintained close ties to the West German Federal Republic of Germany, it was legally never part of it. But the idea of leaving the United States proved too radical even in the turmoil of 1861 and was poorly received, the war, and especially conscription, was nevertheless often unpopular in the city, sparking the deadly New York Draft Riots. The neighboring City of Brooklyn, in contrast, was staunchly Unionist, the Free City of Danzig was a semi-autonomous city-state that existed between 1920 and 1939, consisting of the Baltic Sea port of Danzig and nearly 200 towns in the surrounding areas. It was created on 15 November 1920 under the terms of Article 100 of the 1919 Treaty of Versailles after the end of World War I. Its territory of 28 km2 comprised the city of Fiume and rural areas to its north, with a corridor to its west connecting it to Italy, the Shanghai International Settlement was an international zone with its own legal system, postal service, and currency. The Klaipėda Region or Memel Territory was defined by the Treaty of Versailles in 1920 when it was put under the administration of the Council of Ambassadors
10.
Solstice
–
The Solstice occurs twice each year as the Sun reaches its most northerly or southerly excursion relative to the celestial equator on the celestial sphere. The seasons of the year are directly connected to both the solstices and the equinoxes, the term solstice can also be used in a broader sense, as the day when this occurs. The day of the solstice has either the most sunlight of the year or the least sunlight of the year for any other than the equator. Alternative terms, with no ambiguity as to which hemisphere is the context, are June solstice and December solstice, at latitudes outside the tropics, the summer solstice marks the day when the sun appears highest in the sky. Within the tropics, the sun directly overhead from days to months before the solstice and again after the solstice. For an observer on the North Pole, the sun reaches the highest position in the sky once a year in June, the day this occurs is called the June solstice day. Similarly, for an observer on the South Pole, the sun reaches the highest position on December solstice day, when it is the summer solstice at one Pole, it is the winter solstice on the other. The suns westerly motion never ceases as the Earth is continually in rotation, however, the suns motion in declination comes to a stop at the moment of solstice. In that sense, solstice means sun-standing and this modern scientific word descends from a Latin scientific word in use in the late Roman republic of the 1st century BC, solstitium. Pliny uses it a number of times in his Natural History with a meaning that it has today. It contains two Latin-language morphemes, sol, sun, and -stitium, stoppage, the Romans used standing to refer to a component of the relative velocity of the Sun as it is observed in the sky. Relative velocity is the motion of an object from the point of view of an observer in a frame of reference, from a fixed position on the ground, the sun appears to orbit around the Earth. To an observer in a frame of reference, the planet Earth is seen to rotate about an axis. The Earths axis is tilted with respect to the plane of the Earths orbit, an observer on Earth therefore sees a solar path that is the result of both rotation and revolution. At maximum or minimum elevation, the relative motion of the Sun perpendicular to the horizon stops. Outside of the tropics, the maximum occurs at the summer solstice. The path of the Sun, or ecliptic, sweeps north and south between the northern and southern hemispheres, the days are longer around the summer solstice and shorter around the winter solstice. When the Suns path crosses the equator, the length of the nights at latitudes +L° and -L° are of equal length and this is known as an equinox
.JPG)
.JPG)
.JPG)
.JPG)
.JPG)
.jpg)
.JPG)
.jpg)
.jpg)
.JPG)
.JPG)
