1.
Ancient Agora of Athens
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Some of these included, The Middle stoa which was the most extensive monument built during the 100s B. C. E. A small Roman temple was added in front of the Middle stoa, an Altar of Zeus Agoraios was added just to the east of the Monument to the Eponymous Heroes. The Temple of Ares, dedicated to Ares, the god of war, was added in the north half agora, the Odeon of Agrippa and accompanying gymnasium were added in the centre of the agora. The substantial Stoa of Attalos was built along the edge of the agora. A collection of buildings were added to the south-east corner, the East stoa, the Library of Pantainos, the Nymphaeum, there is evidence of a Synagogue in the Agora of Athens in the 3rd century. A statue of the Roman emperor Hadrian was located near the metroon, the Temple of Zeus Phratrios and Athena Phratria dated to the 300s B. C. E. and is located near the Temple of Apollo Patroos. The south end of what is believed to be a Basilica has been uncovered near Hadrian Street and is dated to the mid 100s C. E, the Monopteros was located south of the Basilica and also dated to the mid 100s C. E. It had no walls, was a dome supported by columns and was about 8 meters in diameter, the Bema was a speakers platform and was located near the Stoa of Attalos. The ancient Athenian agora has been excavated by the American School of Classical Studies at Athens since 1931 under the direction of T and they continue to the present day, now under the direction of John McK Camp. The museum is housed in the Stoa of Attalos, and its exhibits are connected with the Athenian democracy. Ecclesia Roman Agora Church of the Holy Apostles Hellenic Ministry of Culture, The Ancient Agora of Athens – official site with a schedule of its hours, tickets. Agora Excavations – American School of Classical Studies Agora excavation project, map of the Agora of Athens in Socrates and Platos time Agora of Athens in 421 BC The Athenian Agora, A Short Guide in Color The Athenian Agora
2.
Greece
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Greece, officially the Hellenic Republic, historically also known as Hellas, is a country in southeastern Europe, with a population of approximately 11 million as of 2015. Athens is the capital and largest city, followed by Thessaloniki. Greece is strategically located at the crossroads of Europe, Asia, situated on the southern tip of the Balkan peninsula, it shares land borders with Albania to the northwest, the Republic of Macedonia and Bulgaria to the north, and Turkey to the northeast. Greece consists of nine regions, Macedonia, Central Greece, the Peloponnese, Thessaly, Epirus, the Aegean Islands, Thrace, Crete. The Aegean Sea lies to the east of the mainland, the Ionian Sea to the west, the Cretan Sea and the Mediterranean Sea to the south. Greece has the longest coastline on the Mediterranean Basin and the 11th longest coastline in the world at 13,676 km in length, featuring a vast number of islands, eighty percent of Greece is mountainous, with Mount Olympus being the highest peak at 2,918 metres. From the eighth century BC, the Greeks were organised into various independent city-states, known as polis, which spanned the entire Mediterranean region and the Black Sea. Greece was annexed by Rome in the second century BC, becoming a part of the Roman Empire and its successor. The Greek Orthodox Church also shaped modern Greek identity and transmitted Greek traditions to the wider Orthodox World, falling under Ottoman dominion in the mid-15th century, the modern nation state of Greece emerged in 1830 following a war of independence. Greeces rich historical legacy is reflected by its 18 UNESCO World Heritage Sites, among the most in Europe, Greece is a democratic and developed country with an advanced high-income economy, a high quality of life, and a very high standard of living. A founding member of the United Nations, Greece was the member to join the European Communities and has been part of the Eurozone since 2001. Greeces unique cultural heritage, large industry, prominent shipping sector. It is the largest economy in the Balkans, where it is an important regional investor, the names for the nation of Greece and the Greek people differ from the names used in other languages, locations and cultures. The earliest evidence of the presence of human ancestors in the southern Balkans, dated to 270,000 BC, is to be found in the Petralona cave, all three stages of the stone age are represented in Greece, for example in the Franchthi Cave. Neolithic settlements in Greece, dating from the 7th millennium BC, are the oldest in Europe by several centuries and these civilizations possessed writing, the Minoans writing in an undeciphered script known as Linear A, and the Mycenaeans in Linear B, an early form of Greek. The Mycenaeans gradually absorbed the Minoans, but collapsed violently around 1200 BC and this ushered in a period known as the Greek Dark Ages, from which written records are absent. The end of the Dark Ages is traditionally dated to 776 BC, the Iliad and the Odyssey, the foundational texts of Western literature, are believed to have been composed by Homer in the 7th or 8th centuries BC. With the end of the Dark Ages, there emerged various kingdoms and city-states across the Greek peninsula, in 508 BC, Cleisthenes instituted the worlds first democratic system of government in Athens
3.
Pergamon
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Pergamon /ˈpɜːrɡəmən/ or /ˈpɜːrɡəmɒn/ or Pergamum /ˈpɜːrɡəməm/ was a rich and powerful ancient Greek city in Aeolis. It is located 26 kilometres from the coastline of the Aegean Sea on a promontory on the north side of the river Caicus. Many remains of its monuments can still be seen and especially the outstanding masterpiece of the Pergamon Altar. It became the capital of the Kingdom of Pergamon during the Hellenistic period under the Attalid dynasty in 281–133 BC, Pergamon is cited in the Book of Revelation as one of the seven churches of Asia. Xenophon provides the earliest surviving mention of Pergamon. Captured by Xenophon in 399 BC and immediately recaptured by the Persians, in 261 BC he bequeathed his possessions to his nephew Eumenes I, who increased them greatly, leaving as heir his cousin Attalus I. The Attalids became some of the most loyal supporters of Rome in the Hellenistic world, for their support against the Seleucids, the Attalids were rewarded with all the former Seleucid domains in Asia Minor. As a consequence of its rise to power, the city expanded greatly, until 188 BC, it had not grown significantly since its founding by Philetaerus, and covered c.21 hectares. After this year, a new city wall was constructed,4 kilometres long and enclosing an area of approximately 90 hectares. The Attalids ruled with intelligence and generosity, many documents survive showing how the Attalids supported the growth of towns by sending in skilled artisans and by remitting taxes. They allowed the Greek cities in their domains to maintain nominal independence and they sent gifts to Greek cultural sites like Delphi, Delos, and Athens. They remodeled the Acropolis of Pergamon after the Acropolis in Athens, when Attalus III died without an heir in 133 BC, he bequeathed the whole of Pergamon to Rome in order to prevent a civil war. Not everyone in Pergamon accepted Romes rule, aristonicus, who claimed to be Attalus brother as well as the son of Eumenes II, an earlier king, led a revolt among the lower classes with the help of Blossius. The revolt was put down in 129 BC, and Pergamon was divided among Rome, Pontus, Pergamon was briefly the capital of the Roman province of Asia, before the capital was transferred to Ephesus. After a slow decline, the city was favoured by several imperial initiatives under Hadrian, in addition, at the city limits the shrine to Asclepius was expanded into a lavish spa. This sanctuary grew in fame and was considered one of the most famous therapeutic, galen, after Hippocrates the most famous physician of antiquity, was born at Pergamon and received his early training at the Asclepeion. Pergamon reached the height of its greatness under Roman Imperial rule and was home to about 200,000 inhabitants, the city was an early seat of Christianity and was granted a bishopric by the 2nd century. The city suffered badly during the century and was badly damaged by an earthquake in 262 and was sacked by the Goths shortly after
4.
Marble
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Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or dolomite. Geologists use the marble to refer to metamorphosed limestone, however. Marble is commonly used for sculpture and as a building material and this stem is also the basis for the English word marmoreal, meaning marble-like. In Hungarian it is called márvány, Marble is a rock resulting from metamorphism of sedimentary carbonate rocks, most commonly limestone or dolomite rock. Metamorphism causes variable recrystallization of the carbonate mineral grains. The resulting marble rock is composed of an interlocking mosaic of carbonate crystals. Primary sedimentary textures and structures of the carbonate rock have typically been modified or destroyed. Pure white marble is the result of metamorphism of a very pure limestone or dolomite protolith, green coloration is often due to serpentine resulting from originally magnesium-rich limestone or dolostone with silica impurities. These various impurities have been mobilized and recrystallized by the intense pressure, examples of historically notable marble varieties and locations, White marble has been prized for its use in sculptures since classical times. This preference has to do with its softness, which made it easier to carve, relative isotropy and homogeneity, construction marble is a stone which is composed of calcite, dolomite or serpentine which is capable of taking a polish. More generally in construction, specifically the dimension stone trade, the marble is used for any crystalline calcitic rock useful as building stone. For example, Tennessee marble is really a dense granular fossiliferous gray to pink to maroon Ordovician limestone that geologists call the Holston Formation. Ashgabat, the city of Turkmenistan, was recorded in the 2013 Guinness Book of Records as having the worlds highest concentration of white marble buildings. According to the United States Geological Survey, U. S. domestic marble production in 2006 was 46,400 tons valued at about $18.1 million, compared to 72,300 tons valued at $18.9 million in 2005. Crushed marble production in 2006 was 11.8 million tons valued at $116 million, of which 6.5 million tons was finely ground calcium carbonate and the rest was construction aggregate. For comparison,2005 crushed marble production was 7.76 million tons valued at $58.7 million, of which 4.8 million tons was finely ground calcium carbonate, U. S. dimension marble demand is about 1.3 million tons. The DSAN World Demand for Marble Index has shown a growth of 12% annually for the 2000–2006 period, the largest dimension marble application is tile. In 1998, marble production was dominated by 4 countries that accounted for almost half of production of marble
5.
Limestone
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Limestone is a sedimentary rock, composed mainly of skeletal fragments of marine organisms such as coral, forams 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, intraclasts 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 also 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, clastic, granular, or massive, depending on the method of formation. Crystals of calcite, quartz, 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
6.
Doric order
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The Doric order was one of the three orders of ancient Greek and later Roman architecture, the other two canonical orders were the Ionic and the Corinthian. The Doric is most easily recognised by the simple circular capitals at the top of columns and it was the earliest and in its essence the simplest of the orders, though still with complex details in the entablature above. The Greek Doric column was fluted or smooth-surfaced, and had no base, the capital was a simple circular form, with some mouldings, under a square cushion that is very wide in early versions, but later more restrained. In stone they are purely ornamental, the relatively uncommon Roman and Renaissance Doric retained these, and often introduced thin layers of moulding or further ornament, as well as often using plain columns. The Doric order was used in Greek Revival architecture from the 18th century onwards, often earlier Greek versions were used, with wider columns. Since at least Vitruvius it has been customary for writers to associate the Doric with masculine virtues and it is also normally the cheapest of the orders to use. In their original Greek version, Doric columns stood directly on the pavement of a temple without a base. The Parthenon has the Doric design columns and it was most popular in the Archaic Period in mainland Greece, and also found in Magna Graecia, as in the three temples at Paestum. These are in the Archaic Doric, where the capitals spread wide from the column compared to later Classical forms, pronounced features of both Greek and Roman versions of the Doric order are the alternating triglyphs and metopes. The triglyphs are decoratively grooved with two vertical grooves and represent the original wooden end-beams, which rest on the plain architrave that occupies the half of the entablature. Under each triglyph are peglike stagons or guttae that appear as if they were hammered in from below to stabilize the post-and-beam construction and they also served to organize rainwater runoff from above. The spaces between the triglyphs are the metopes and they may be left plain, or they may be carved in low relief. The spacing of the triglyphs caused problems which some time to resolve. The architecture followed rules of harmony, since the original design probably came from wooden temples and the triglyphs were real heads of wooden beams, every column had to bear a beam which lay across the centre of the column. Triglyphs were arranged regularly, the last triglyph was centred upon the last column and this was regarded as the ideal solution which had to be reached. Changing to stone instead of wooden beams required full support of the architrave load at the last column. At the first temples the final triglyph was moved, still terminating the sequence, even worse, the last triglyph was not centered with the corresponding column. That “archaic” manner was not regarded as a harmonious design, the resulting problem is called the doric corner conflict
7.
Ionic order
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The Ionic order forms one of the three classical orders of classical architecture, the other two canonic orders being the Doric and the Corinthian. There are two orders, the Tuscan, and the rich variant of Corinthian called the composite order. The Ionic columns are the thinnest and smallest columns out of the three canonic orders, the Ionic capital is characterized by the use of volutes. The Ionic columns normally stand on a base which separates the shaft of the column from the stylobate or platform, since Vitruvius a female character has been ascribed to the Ionic, in contrast to the masculine Doric. The major features of the Ionic order are the volutes of its capital, the only tools required to design these features were a straight-edge, a right angle, string and a compass. Originally the volutes lay in a plane, then it was seen that they could be angled out on the corners. Ionic columns are most often fluted, after a little early experimentation, the number of hollow flutes in the shaft settled at 24. This standardization kept the fluting in a proportion to the diameter of the column at any scale. Roman fluting leaves a little of the surface between each hollow, Greek fluting runs out to a knife edge that was easily scarred. In some instances, the fluting has been omitted, mohr included 8 unfluted Ionic frontal columns on his 1928 design for the railroads St. Louis suburban stop Delmar Station. Pictorial often narrative bas-relief frieze carving provides a feature of the Ionic order. Roman and Renaissance practice condensed the height of the entablature by reducing the proportions of the architrave, the Ionic order originated in the mid-6th century BC in Ionia, the southwestern coastland and islands of Asia Minor settled by Ionian Greeks, where an Ionian dialect was spoken. The Ionic order column was being practiced in mainland Greece in the 5th century BC and it was most popular in the Archaic Period in Ionia. The first of the great Ionic temples was the Temple of Hera on Samos and it stood for only a decade before it was leveled by an earthquake. A longer-lasting 6th century Ionic temple was the Temple of Artemis at Ephesus, the Parthenon, although it conforms mainly to the Doric order, also has some Ionic elements. A more purely Ionic mode to be seen on the Athenian Acropolis is exemplified in the Erechtheum, following the conquests of Alexander the Great in the east, a few examples of the Ionic order can be found as far as Pakistan with the Jandial temple near Taxila. Several examples of capitals displaying Ionic influences can seen as far away as Patna, especially with the Pataliputra capital. Renaissance architectural theorists took his hints, to interpret the Ionic order as matronly in comparison to the Doric order, the Ionic is a natural order for post-Renaissance libraries and courts of justice, learned and civilized
8.
American School of Classical Studies at Athens
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The American School of Classical Studies at Athens is one of 17 foreign archaeological institutes in Athens, Greece. The center is a member of the Council of American Overseas Research Centers, the ASCSA offers graduate students enrolled in member universities an unparalleled immersion into the sites and monuments of Greek civilization. The program for Regular Members is a participatory program over nine months. Regular Members are expected to be in attendance for the full nine-month program, students receive comprehensive training through visits to the principal archaeological sites and museums of Greece as well as in seminars led by resident and visiting scholars. They also take part in the program at the Corinth excavations. The School accepts 15 to 20 students in this program, in these sessions, the School condenses its academic year program into an intensive introduction to the sites, museums, and monuments of Greece. The Summer programs are open to 20 participants each session, the School welcomes scholars to its libraries year-round for research. Throughout its existence, the ASCSA has been involved in a number of archaeological projects. It is responsible for two of the most important archaeological sites in Greece, the Athenian Agora and Ancient Corinth, the Corinth Excavations commenced in 1896 and have continued to present day with little interruption, and the Athenian Agora excavations first broke ground in 1932. At both sites, the ASCSA operates important museums and extensive facilities for the study of the archaeological record, excavation records and artifacts are made available to wider audiences via ASCSA. Lykaion, Nichoria and the Palace of Nestor at Pylos, Haghia Irini, as well as Azoria, Mochlos, Gournia, Kavousi and these books range in format from large hardbacks to slim paperback guides. William W. Goodwin, first director Lewis R. Packard Frank B, tarbell Henry S. Robonson Henry R. Immerwahr Stephen V. Tracy Jack L. Davis James C. Wright, current incumbent E. Korka et al, foreign Archaeological Schools in Greece,160 Years, Athens, Hellenic Ministry of Culture,2006, p. 18-29. L. Lord, A History of the American School of Classical Studies at Athens, An Intercollegiate Experiment, L. Shoe Meritt, A History of the American School of Classical Studies at Athens, 1939-1980
9.
Rockefeller family
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The family is also known for its long association with and control of Chase Manhattan Bank. They are considered to be one of the most powerful families, if not the most powerful family, one of the founding members of the Rockefeller family was businessman William Rockefeller Sr. born in Granger, New York, to a Protestant family. He had six children with his first wife Eliza Davison, the most prominent of which were oil tycoons John Davison Rockefeller and William Rockefeller, Oil baron John D. Rockefeller was a devout Northern Baptist, and he supported many church-based institutions. The family was involved in numerous real estate construction projects in the U. S. during the 20th century. In Manhattan by fourteen major institutions that were based in the area, the result, in 1951, was the six-building apartment complex known as Morningside Gardens. Seniors donations led to the formation of the University of Chicago in 1889, the Central Philippine University in the Philippines and this was one instance of a long family and Rockefeller Foundation tradition of financially supporting Ivy League and other major colleges and universities over the generations—seventy-five in total. John D Jr. established International House at Berkeley, beginning with John Sr. the family has been a major force in land conservation. John Jr. and his son Laurance were particularly prominent in this area, at the event, the societys president, John Flicker, notably stated, Cumulatively, no other family in America has made the contribution to conservation that the Rockefeller family has made. Nelson, John D. III, John D. IV, Peggy Dulany, Rockefeller Foundation, the Trilateral Commission -David, Rockefeller Brothers Fund. The Bilderberg Group - David, John D. IV, the Asia Society - John D. III, John D. IV, Charles, David. The Population Council - John D. III, the Council of the Americas - David. The Group of Thirty - The Rockefeller Foundation, the World Economic Forum - David. The Peterson Institute - David, Monica, the International Executive Service Corps - David. The Institute for Pacific Relations - Junior, the League of Nations - Junior. The United Nations - Junior, John D. III, Nelson, David, Peggy Dulany, the United Nations Association - David. These include, the Commonwealth Fund, Charles E. Culpeper Foundation, Lucille P. Markey Charitable Trust, in total, it holds over 70 million pages of documents and contains the collections of forty-two scientific, cultural, educational and philanthropic organizations. Only the expurgated records of deceased family members are available to scholars and researchers. He reports that it will be years before all the papers will be open to the public
10.
Cyprus
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Cyprus, officially the Republic of Cyprus, is an island country in the Eastern Mediterranean and the third largest and third most populous island in the Mediterranean. It is located south of Turkey, west of Syria and Lebanon, northwest of Israel and Palestine, north of Egypt, the earliest known human activity on the island dates to around the 10th millennium BC. Archaeological remains from this include the well-preserved Neolithic village of Khirokitia. Cyprus was settled by Mycenaean Greeks in two waves in the 2nd millennium BC, Cyprus was placed under British administration based on Cyprus Convention in 1878 and formally annexed by Britain in 1914. While Turkish Cypriots made up 18% of the population, the partition of Cyprus and creation of a Turkish state in the north became a policy of Turkish Cypriot leaders, following nationalist violence in the 1950s, Cyprus was granted independence in 1960. On 15 July 1974, a coup détat was staged by Greek Cypriot nationalists and elements of the Greek military junta in an attempt at enosis and these events and the resulting political situation are matters of a continuing dispute. The Cyprus Republic has de jure sovereignty over the island of Cyprus, as well as its territorial sea and exclusive economic area, another nearly 4% of the islands area is covered by the UN buffer zone. The international community considers the part of the island as territory of the Republic of Cyprus occupied by Turkish forces. The occupation is viewed as illegal under law, amounting to illegal occupation of EU territory since Cyprus became a member of the European Union. Cyprus is a major tourist destination in the Mediterranean, on 1 January 2008, the Republic of Cyprus joined the eurozone. The earliest attested reference to Cyprus is the 15th century BC Mycenaean Greek
11.
Czech Republic
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The Czech Republic, also known as Czechia, is a nation state in Central Europe bordered by Germany to the west, Austria to the south, Slovakia to the east and Poland to the northeast. The Czech Republic covers an area of 78,866 square kilometres with mostly temperate continental climate and it is a unitary parliamentary republic, has 10.5 million inhabitants and the capital and largest city is Prague, with over 1.2 million residents. The Czech Republic includes the territories of Bohemia, Moravia. The Czech state was formed in the late 9th century as the Duchy of Bohemia under the Great Moravian Empire, after the fall of the Empire in 907, the centre of power transferred from Moravia to Bohemia under the Přemyslid dynasty. In 1002, the duchy was formally recognized as part of the Holy Roman Empire, becoming the Kingdom of Bohemia in 1198 and reaching its greatest territorial extent in the 14th century. Following the Battle of Mohács in 1526, the whole Crown of Bohemia was gradually integrated into the Habsburg Monarchy alongside the Archduchy of Austria, the Protestant Bohemian Revolt against the Catholic Habsburgs led to the Thirty Years War. After the Battle of the White Mountain, the Habsburgs consolidated their rule, reimposed Roman Catholicism, the Czech part of Czechoslovakia was occupied by Germany in World War II, and was liberated in 1945 by the armies of the Soviet Union and the United States. The Czech country lost the majority of its German-speaking inhabitants after they were expelled following the war, the Communist Party of Czechoslovakia won the 1946 elections. Following the 1948 coup détat, Czechoslovakia became a one-party communist state under Soviet influence, in 1968, increasing dissatisfaction with the regime culminated in a reform movement known as the Prague Spring, which ended in a Soviet-led invasion. Czechoslovakia remained occupied until the 1989 Velvet Revolution, when the communist regime collapsed, on 6 March 1990, the Czech Socialistic Republic was renamed to the Czech Republic. On 1 January 1993, Czechoslovakia peacefully dissolved, with its constituent states becoming the independent states of the Czech Republic and the Slovak Republic. The Czech Republic joined NATO in 1999 and the European Union in 2004, it is a member of the United Nations, the OECD, the OSCE, and it is a developed country with an advanced, high income economy and high living standards. The UNDP ranks the country 14th in inequality-adjusted human development, the Czech Republic also ranks as the 6th most peaceful country, while achieving strong performance in democratic governance. It has the lowest unemployment rate in the European Union, the traditional English name Bohemia derives from Latin Boiohaemum, which means home of the Boii. The current name comes from the endonym Čech, spelled Cžech until the reform in 1842. The name comes from the Slavic tribe and, according to legend, their leader Čech, the etymology of the word Čech can be traced back to the Proto-Slavic root *čel-, meaning member of the people, kinsman, thus making it cognate to the Czech word člověk. The country has traditionally divided into three lands, namely Bohemia in the west, Moravia in the southeast, and Czech Silesia in the northeast. Following the dissolution of Czechoslovakia at the end of 1992, the Czech part of the former nation found itself without a common single-word geographical name in English, the name Czechia /ˈtʃɛkiə/ was recommended by the Czech Ministry of Foreign Affairs
12.
Estonia
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Estonia, officially the Republic of Estonia, is a country in the Baltic region of Northern Europe. It is bordered to the north by the Gulf of Finland, to the west by the Baltic Sea, to the south by Latvia, across the Baltic Sea lies Sweden in the west and Finland in the north. The territory of Estonia consists of a mainland and 2,222 islands and islets in the Baltic Sea, covering 45,339 km2 of land and water, and is influenced by a humid continental climate. The territory of Estonia has been inhabited since at least 6500 BC, in 1988, during the Singing Revolution, the Estonian Supreme Soviet issued the Estonian Sovereignty Declaration in defiance of Soviet rule, and independence was restored on 20 August 1991. Estonia is a parliamentary republic divided into fifteen counties. Its capital and largest city is Tallinn, with a population of 1.3 million, it is one of the least-populous member states of the European Union, Eurozone, North Atlantic Treaty Organization, OECD and Schengen Area. Estonia is a country with an advanced, high-income economy that is among the fastest growing in the EU. Its Human Development Index ranks very highly, and it performs favourably in measurements of economic freedom, civil liberties, the 2015 PISA test places Estonian high school students 3rd in the world, behind Singapore and Japan. Citizens of Estonia are provided with health care, free education. Since independence the country has developed its IT sector, becoming one of the worlds most digitally advanced societies. In 2005 Estonia became the first nation to hold elections over the Internet, in the Estonian language, the oldest known endonym of the Estonians was maarahvas, meaning country people or people of the land. The land inhabited by Estonians was called Maavald meaning Country Parish or Land Parish, one hypothesis regarding the modern name of Estonia is that it originated from the Aesti, a people described by the Roman historian Tacitus in his Germania. The historic Aesti were allegedly Baltic people, whereas the modern Estonians are Finno-Ugric, the geographical areas between Aesti and Estonia do not match, with Aesti being further down south. Ancient Scandinavian sagas refer to a land called Eistland, as the country is called in Icelandic. Early Latin and other ancient versions of the name are Estia and Hestia, esthonia was a common alternative English spelling prior to 1921. Human settlement in Estonia became possible 13,000 to 11,000 years ago, the oldest known settlement in Estonia is the Pulli settlement, which was on the banks of the river Pärnu, near the town of Sindi, in south-western Estonia. According to radiocarbon dating it was settled around 11,000 years ago, the earliest human inhabitation during the Mesolithic period is connected to Kunda culture, which is named after the town of Kunda in northern Estonia. At that time the country was covered with forests, and people lived in communities near bodies of water
