1.
Turkey
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Turkey, officially the Republic of Turkey, is a transcontinental country in Eurasia, mainly in Anatolia in Western Asia, with a smaller portion on the Balkan peninsula in Southeast Europe. Turkey is a democratic, secular, unitary, parliamentary republic with a cultural heritage. The country is encircled by seas on three sides, the Aegean Sea is to the west, the Black Sea to the north, and the Mediterranean Sea to the south. The Bosphorus, the Sea of Marmara, and the Dardanelles, Ankara is the capital while Istanbul is the countrys largest city and main cultural and commercial centre. Approximately 70-80% of the countrys citizens identify themselves as ethnic Turks, other ethnic groups include legally recognised and unrecognised minorities. Kurds are the largest ethnic minority group, making up approximately 20% of the population, the area of Turkey has been inhabited since the Paleolithic by various ancient Anatolian civilisations, as well as Assyrians, Greeks, Thracians, Phrygians, Urartians and Armenians. After Alexander the Greats conquest, the area was Hellenized, a process continued under the Roman Empire. The Seljuk Sultanate of Rûm ruled Anatolia until the Mongol invasion in 1243, the empire reached the peak of its power in the 16th century, especially during the reign of Suleiman the Magnificent. During the war, the Ottoman government committed genocides against its Armenian, Assyrian, following the war, the conglomeration of territories and peoples that formerly comprised the Ottoman Empire was partitioned into several new states. Turkey is a member of the UN, an early member of NATO. Turkeys growing economy and diplomatic initiatives have led to its recognition as a regional power while her location has given it geopolitical, the name of Turkey is based on the ethnonym Türk. The first recorded use of the term Türk or Türük as an autonym is contained in the Old Turkic inscriptions of the Göktürks of Central Asia, the English name Turkey first appeared in the late 14th century and is derived from Medieval Latin Turchia. Similarly, the medieval Khazar Empire, a Turkic state on the shores of the Black. The medieval Arabs referred to the Mamluk Sultanate as al-Dawla al-Turkiyya, the Ottoman Empire was sometimes referred to as Turkey or the Turkish Empire among its European contemporaries. The Anatolian peninsula, comprising most of modern Turkey, is one of the oldest permanently settled regions in the world, various ancient Anatolian populations have lived in Anatolia, from at least the Neolithic period until the Hellenistic period. Many of these peoples spoke the Anatolian languages, a branch of the larger Indo-European language family, in fact, given the antiquity of the Indo-European Hittite and Luwian languages, some scholars have proposed Anatolia as the hypothetical centre from which the Indo-European languages radiated. The European part of Turkey, called Eastern Thrace, has also been inhabited since at least forty years ago. It is the largest and best-preserved Neolithic site found to date, the settlement of Troy started in the Neolithic Age and continued into the Iron Age
2.
Eastern Anatolia Region
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The Eastern Anatolia Region is a geographical region of Turkey. The region and the name Doğu Anadolu Bölgesi were first defined at the First Geography Congress in 1941 and it has the highest average altitude, largest geographical area, and lowest population density of all regions of Turkey. Prior to getting its current name by the Turkish state, most of the region was part of the Six Armenian provinces in the known as the Armenian Highlands. After the Armenian Genocide, the geopolitical term Eastern Anatolia was created to replace what had historically been known as Western Armenia, starting from 1880 the name Armenia was forbidden to be used in official Ottoman documents. The government of Sultan Abdul Hamid II replaced the name Armenia with such terms as Kurdistan or Anatolia, the Sublime Porte was trying to cover up the Armenian Question, if there was no Armenia, then there was no Armenian Question. The process of “nationalization” of toponyms was continued by the Kemalists, who were the successors of the Young Turks. Starting from 1923 the entire territory of Western Armenia was officially renamed “Eastern Anatolia”, in the 17th century when the Armenian Question was not as yet included into the international diplomacy agenda, the terms Anatolia or Eastern Anatolia were never used to indicate Armenia. Furthermore, the Islamic World Map of the 16th century and other Ottoman maps of the 18th and 19th centuries have clearly indicated Armenia on a territory as well as its cities. Armenia, together with its boundaries, was mentioned in the works of earlier Ottoman historians. Kâtip Çelebi, a famous Ottoman chronicler of the 17th century, had a chapter titled “About the Country Called Armenia” in his book Jihan Numa. When, however, this book was republished in 1957, its modern Turkish editor H. Selen changed this title into “Eastern Anatolia”. Osman Nuri, a historian of the half of the 19th century, mentions Armenia repeatedly in his three-volume Abdul Hamid. The word Anatolia means “sunrise” or “east” in Greek and this name was given to the Asia Minor peninsula approximately in the 5th or 4th centuries B. C. During the Ottoman era, the term Anadolou included the vilayets of Asia Minor with Kyotahia as its center. The numerous European, Ottoman, Armenian, Russian, Persian, Arabic and this testifies, inter alia, to the fact that even after the loss of its statehood the Armenian nation still constituted a majority in its homeland, which was recognized by Ottoman occupiers as well. The area of the region is 146,330 km², which comprises 18. 7% of the area of Turkey. The total population of the region is 6,100,000 and 5,906,565, the region has the second most rural population of Turkey after the Black Sea region. The migration level is high and population density is lower than the average for Turkey, the migration toward other Turkeys regions and toward foreign countries is higher than the natural population increase, a fact which is leading to a slight decline of the Regions population
3.
Mount Ararat
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Mount Ararat is a snow-capped and dormant compound volcano in the eastern extremity of Turkey. It consists of two volcanic cones, Greater Ararat, the highest peak in Turkey and the Armenian plateau with an elevation of 5,137 m. The Ararat massif is about 40 km in diameter, scholars agree the biblical mountains of Ararat do not refer to specifically Mt. Ararat. Nevertheless, it has perceived as the traditional resting place of Noahs Ark since the 11th century. It is the national symbol of Armenia and has been considered a sacred mountain by Armenians. It is featured prominently in Armenian literature and art and is an icon for Armenian irredentism, along with Noahs Ark, it is depicted on the coat of arms of Armenia. The first efforts to reach Ararats summit were made in the Middle Ages, however, it was not until 1829 when Friedrich Parrot and Khachatur Abovian, accompanied with four others, made the first recorded ascent. Mount Ararat forms a near-quadripoint between Turkey, Armenia, Azerbaijan and Iran and its summit is located some 16 km west of both the Iranian border and the border of the Nakhchivan exclave of Azerbaijan, and 32 km south of the Armenian border. Following the 1826–28 Russo-Persian War and the Treaty of Turkmenchay, the Persian controlled territory was ceded to the Russian Empire, Little Ararat became the point where the Turkish, Persian, and Russian imperial frontiers converged. The current international boundaries were formed throughout the 20th century, the mountain came under Turkish control during the 1920 Turkish–Armenian War. It formally became part of Turkey according to the 1921 Treaty of Moscow, in the late 1920s, Turkey crossed the Iranian border and occupied the eastern flank of Lesser Ararat as part of its effort to quash the Kurdish Ararat rebellion. The Kurdish rebels were using the area as a haven against the state in their uprising, Iran eventually agreed to cede the area to Turkey in a territorial exchange. The Iran-Turkey boundary skirts east of Lesser Ararat, the peak of the Ararat massif. Ararat is the Hebrew spelling of Urartu, a kingdom existed in the Armenian plateau in the 9th-6th centuries BC. The mountain is known as Ararat in European languages, however, none of the native peoples have traditionally referred to the mountain by that name. The traditional Armenian name is Masis, which is transliterated as Massis. However, nowadays, the terms Masis and Ararat are both widely, often interchangeably, used in Armenian, the peaks are referred to in plural as Մասիսներ Masisner. Greater Ararat is known as simply Masis or Մեծ Մասիս, while Lesser Ararat is known as Sis or Փոքր Մասիս
4.
Lake Van
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Lake Van, the largest lake in Turkey, lies in the far east of that country in the provinces of Van and Bitlis. It is a soda lake, receiving water from numerous small streams that descend from the surrounding mountains. Lake Van is one of the worlds largest endorheic lakes - a volcanic eruption blocked the outlet from the basin in ancient times. Although Lake Van has an altitude of 1,640 m in a region with harsh winters, its high salinity prevents most of it from freezing, and even the shallow northern section freezes only rarely. Lake Van is 119 kilometres across at its widest point, averaging a depth of 171 metres with a recorded depth of 451 metres. The lake surface lies 1,640 metres above sea level, Lake Van has an area of 3,755 km2 and a volume of 607 cubic kilometres. The western portion of the lake is deepest, with a large basin deeper than 400 m lying northeast of Tatvan, the eastern arms of the lake are shallower. The Van-Ahtamar portion shelves gradually, with a depth of about 250 m on its northwest side where it joins the rest of the lake. The Erciş arm is much shallower, mostly less than 50 m, the lake water is strongly alkaline and rich in sodium carbonate and other salts, which are extracted by evaporation and used as detergents. The lakes outlet was blocked at some time during the Pleistocene, now dormant, Nemrut Dağı is close to the western shore of the lake, and another dormant stratovolcano, Süphan Dağı dominates the northern side of the lake. The water level of the lake has often altered dramatically, near Tatvan, investigation by Degens and others in the early 1980s determined that the highest lake levels had been during the last ice age, about 18,000 years ago. Approximately 9,500 years ago there was a drop to more than 300 metres below the present level. This was followed by an equally-dramatic rise around 6,500 years ago, similar-but-smaller fluctuations have been seen recently. The level of the rose by at least three metres during the 1990s, drowning much agricultural land, and seems to be rising again. The level rose approximately two meters in the ten years prior to 2004. As a deep lake with no outlet, Lake Van has accumulated great amounts of sediment washed in from surrounding plains and valleys, and occasionally deposited as ash from eruptions of nearby volcanoes. This layer of sediment is estimated to be up to 400 metres thick in places, in 1989 and 1990, an international team of geologists led by Dr. Stephan Kempe from the University of Hamburg retrieved ten sediment cores from depths up to 446 m. Although these cores only penetrated the first few meters of sediment, litt expects to find that Lake Van stores the climate history of the last 800,000 years—an incomparable treasure house of data which we want to tap for at least the last 500,000 years
5.
River mouth
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A river mouth is the part of a river where the river flows into a larger river, a lake, a reservoir or an ocean. The water from a river can enter the body in a variety of different ways. The motion of the river mainly depends on the density of the river compared to the receiving water and any ambient motion in the receiving water. If the river water is denser than the surface of the receiving water, the river water will then either form an underflow or an interflow within the lake. Alongside these advective transports, inflowing water will also diffuse, at the mouth of a river, the change in flow condition can cause the river to drop any sediment it is carrying. This sediment deposition can generate a variety of landforms, such as deltas, sand bars, spits, many places in England take their names from their positions at the mouths of rivers, for example Plymouth, Sidmouth and Great Yarmouth. Confluence River delta Estuary Liman Aber and Inver
6.
Drainage basin
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A drainage basin or catchment area is any area of land where precipitation collects and drains off into a common outlet, such as into a river, bay, or other body of water. Drainage basins connect into other drainage basins at elevations in a hierarchical pattern, with smaller sub-drainage basins. Other terms used to describe drainage basins are catchment, catchment basin, drainage area, river basin and water basin. In closed drainage basins the water converges to a point inside the basin, known as a sink, which may be a permanent lake. The drainage basin acts as a funnel by collecting all the water within the covered by the basin. Each drainage basin is separated topographically from adjacent basins by a perimeter, drainage basins are similar but not identical to hydrologic units, which are drainage areas delineated so as to nest into a multi-level hierarchical drainage system. Hydrologic units are defined to allow multiple inlets, outlets, or sinks, in a strict sense, all drainage basins are hydrologic units but not all hydrologic units are drainage basins. Drainage basins of the oceans and seas of the world. Grey areas are endorheic basins that do not drain to the oceans, the following is a list of the major ocean basins, About 48. 7% of the worlds land drains to the Atlantic Ocean. The two major mediterranean seas of the world also flow to the Atlantic, The Caribbean Sea and Gulf of Mexico basin includes most of the U. S. The Mediterranean Sea basin includes much of North Africa, east-central Africa, Southern, Central, and Eastern Europe, Turkey, and the areas of Israel, Lebanon. Just over 13% of the land in the world drains to the Pacific Ocean, the Indian Oceans drainage basin also comprises about 13% of Earths land. It drains the eastern coast of Africa, the coasts of the Red Sea and the Persian Gulf, the Indian subcontinent, Burma, antarctica comprises approximately eight percent of the Earths land. The five largest river basins, from largest to smallest, are the basins of the Amazon, the Río de la Plata, the Congo, the Nile, and the Mississippi. The three rivers that drain the most water, from most to least, are the Amazon, Ganga, endorheic drainage basins are inland basins that do not drain to an ocean. Around 18% of all land drains to endorheic lakes or seas or sinks, the largest of these consists of much of the interior of Asia, which drains into the Caspian Sea, the Aral Sea, and numerous smaller lakes. Some of these, such as the Great Basin, are not single drainage basins but collections of separate, in endorheic bodies of standing water where evaporation is the primary means of water loss, the water is typically more saline than the oceans. An extreme example of this is the Dead Sea, drainage basins have been historically important for determining territorial boundaries, particularly in regions where trade by water has been important
7.
Euphrates
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The Euphrates is the longest and one of the most historically important rivers of Western Asia. Together with the Tigris, it is one of the two defining rivers of Mesopotamia, originating in eastern Turkey, the Euphrates flows through Syria and Iraq to join the Tigris in the Shatt al-Arab, which empties into the Persian Gulf. The Ancient Greek form Euphrátēs was borrowed from Old Persian Ufrātu, the Elamite name is ultimately derived from the Sumerian Buranuna, possibly through the Akkadian name. In Akkadian the river was similarly called Purattu, which has been perpetuated in Semitic languages, the Elamite, Akkadian, and possibly Sumerian forms are suggested to be from an unrecorded substrate language. The earliest references to the Euphrates come from texts found in Shuruppak and pre-Sargonic Nippur in southern Iraq. In these texts, written in Sumerian, the Euphrates is called Buranuna, the name could also be written KIB. NUN. or dKIB. NUN, with the prefix d indicating that the river was a divinity. In Sumerian, the name of the city of Sippar in modern-day Iraq was also a written UD. KIB. NUN, the Euphrates is the longest river of Western Asia. It emerges from the confluence of the Kara Su or Western Euphrates, the same figures are given by Isaev and Mikhailova. The length of the Shatt al-Arab, which connects the Euphrates, both the Kara Su and the Murat Su rise northwest from Lake Van at elevations of 3,290 metres and 3,520 metres amsl, respectively. At the location of the Keban Dam, the two rivers, now combined into the Euphrates, have dropped to an elevation of 693 metres amsl, from Keban to the Syrian–Turkish border, the river drops another 368 metres over a distance of less than 600 kilometres. The Euphrates receives most of its water in the form of rainfall and melting snow, discharge in these two months accounts for 36 percent of the total annual discharge of the Euphrates, or even 60–70 percent according to one source, while low runoff occurs in summer and autumn. The discharge regime of the Euphrates has changed dramatically since the construction of the first dams in the 1970s, data on Euphrates discharge collected after 1990 show the impact of the construction of the numerous dams in the Euphrates and of the increased withdrawal of water for irrigation. Average discharge at Hīt after 1990 has dropped to 356 cubic metres per second, the seasonal variability has equally changed. The pre-1990 peak volume recorded at Hīt was 7,510 cubic metres per second, the minimum volume at Hīt remained relatively unchanged, rising from 55 cubic metres per second before 1990 to 58 cubic metres per second afterward. In Syria, three rivers add their water to the Euphrates, the Sajur, the Balikh and the Khabur and these rivers rise in the foothills of the Taurus Mountains along the Syro–Turkish border and add comparatively little water to the Euphrates. The Sajur is the smallest of these tributaries, emerging from two streams near Gaziantep and draining the plain around Manbij before emptying into the reservoir of the Tishrin Dam. The Balikh receives most of its water from a spring near Ayn al-Arus. In terms of length, drainage basin and discharge, the Khabur is the largest of these three and its main karstic springs are located around Ras al-Ayn, from where the Khabur flows southeast past Al-Hasakah, where the river turns south and drains into the Euphrates near Busayrah
8.
Turkish language
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Outside of Turkey, significant smaller groups of speakers exist in Germany, Bulgaria, Macedonia, Northern Cyprus, Greece, the Caucasus, and other parts of Europe and Central Asia. Cyprus has requested that the European Union add Turkish as an official EU language, in 1928, as one of Atatürks Reforms in the early years of the Republic of Turkey, the Ottoman Turkish alphabet was replaced with a Latin alphabet. The distinctive characteristics of Turkish are vowel harmony and extensive agglutination, the basic word order of Turkish is subject–object–verb. Turkish has no classes or grammatical gender. Turkish has a strong T–V distinction and usage of honorifics, Turkish uses second-person pronouns that distinguish varying levels of politeness, social distance, age, courtesy or familiarity toward the addressee. The plural second-person pronoun and verb forms are used referring to a person out of respect. Turkic languages belong to the Altaic language group, the Turkic family comprises some 30 living languages spoken across Eastern Europe, Central Asia, and Siberia. Turkish is a member of the Oghuz group of languages, a subgroup of the Turkic language family, there is a high degree of mutual intelligibility between Turkish and the other Oghuz Turkic languages, including Azerbaijani, Turkmen, Qashqai, Gagauz, and Balkan Gagauz Turkish. The earliest known Old Turkic inscriptions are the three monumental Orkhon inscriptions found in modern Mongolia, erected in honour of the prince Kul Tigin and his brother Emperor Bilge Khagan, these date back to the second Turk Kaghanate. The Seljuqs of the Oghuz Turks, in particular, brought their language, following the adoption of Islam c. Turkish literature during the Ottoman period, particularly Divan poetry, was influenced by Persian, including the adoption of poetic meters. One of the tasks of the newly established association was to initiate a reform to replace loanwords of Arabic. By banning the usage of imported words in the press, the association succeeded in removing several hundred words from the language. While most of the words introduced to the language by the TDK were newly derived from Turkic roots, owing to this sudden change in the language, older and younger people in Turkey started to differ in their vocabularies. While the generations born before the 1940s tend to use the terms of Arabic or Persian origin. The past few decades have seen the work of the TDK to coin new Turkish words to express new concepts and technologies as they enter the language. Many of these new words, particularly information technology terms, have received widespread acceptance, however, the TDK is occasionally criticized for coining words which sound contrived and artificial. Some earlier changes—such as bölem to replace fırka, political party—also failed to meet with popular approval, some words restored from Old Turkic have taken on specialized meanings, for example betik is now used to mean script in computer science
9.
Armenian language
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The Armenian language is an Indo-European language spoken by the Armenians. Like Hellenic Greek, it has its own branch in the language tree. It is the language of Armenia and Nagorno-Karabakh Republic. It has historically been spoken throughout the Armenian Highlands and today is spoken in the Armenian diaspora. Armenian has its own script, the Armenian alphabet, introduced in 405 AD by Mesrop Mashtots. Armenian is an independent branch of the Indo-European languages and it is of interest to linguists for its distinctive phonological developments within that family. Armenian exhibits more satemization than centumization, although it is not classified as belonging to either of these subgroups, Armenia was a monolingual country by the 2nd century BC at the latest. Its language has a literary history, with a 5th-century Bible translation as its oldest surviving text. Its vocabulary has been influenced by Western Middle Iranian languages, particularly Parthian, and to an extent by Greek, Persian. There are two standardized modern literary forms, Eastern Armenian and Western Armenian, with which most contemporary dialects are mutually intelligible and he is also credited by some with the creation of the Caucasian Albanian alphabet. In The Anabasis, Xenophon describes many aspects of Armenian village life and he relates that the Armenian people spoke a language that to his ear sounded like the language of the Persians. W. M. However, unlike shared innovations, the retention of archaisms is not considered conclusive evidence of a period of common isolated development. Some of the terms he gives admittedly have an Akkadian or Sumerian provenance, loan words from Iranian languages, along with the other ancient accounts such as that of Xenophon above, initially led linguists to erroneously classify Armenian as an Iranian language. Scholars such as Paul de Lagarde and F. Müller believed that the similarities between the two meant that Iranian and Armenian were the same language. The distinctness of Armenian was recognized when philologist Heinrich Hübschmann used the method to distinguish two layers of Iranian loans from the older Armenian vocabulary. Meillets hypothesis became popular in the wake of his Esquisse, eric P. Hamp supports the Graeco-Armenian thesis, anticipating even a time when we should speak of Helleno-Armenian. Nevertheless, as Fortson comments, by the time we reach our earliest Armenian records in the 5th century AD, graeco--Aryan is a hypothetical clade within the Indo-European family, ancestral to the Greek language, the Armenian language, and the Indo-Iranian languages. Graeco-Aryan unity would have divided into Proto-Greek and Proto-Indo-Iranian by the mid-third millennium BC
10.
Greek language
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Greek is an independent branch of the Indo-European family of languages, native to Greece and other parts of the Eastern Mediterranean. It has the longest documented history of any living language, spanning 34 centuries of written records and its writing system has been the Greek alphabet for the major part of its history, other systems, such as Linear B and the Cypriot syllabary, were used previously. The alphabet arose from the Phoenician script and was in turn the basis of the Latin, Cyrillic, Armenian, Coptic, Gothic and many other writing systems. Together with the Latin texts and traditions of the Roman world, during antiquity, Greek was a widely spoken lingua franca in the Mediterranean world and many places beyond. It would eventually become the official parlance of the Byzantine Empire, the language is spoken by at least 13.2 million people today in Greece, Cyprus, Italy, Albania, Turkey, and the Greek diaspora. Greek roots are used to coin new words for other languages, Greek. Greek has been spoken in the Balkan peninsula since around the 3rd millennium BC, the earliest written evidence is a Linear B clay tablet found in Messenia that dates to between 1450 and 1350 BC, making Greek the worlds oldest recorded living language. Among the Indo-European languages, its date of earliest written attestation is matched only by the now extinct Anatolian languages, the Greek language is conventionally divided into the following periods, Proto-Greek, the unrecorded but assumed last ancestor of all known varieties of Greek. The unity of Proto-Greek would have ended as Hellenic migrants entered the Greek peninsula sometime in the Neolithic era or the Bronze Age, Mycenaean Greek, the language of the Mycenaean civilisation. It is recorded in the Linear B script on tablets dating from the 15th century BC onwards, Ancient Greek, in its various dialects, the language of the Archaic and Classical periods of the ancient Greek civilisation. It was widely known throughout the Roman Empire, after the Roman conquest of Greece, an unofficial bilingualism of Greek and Latin was established in the city of Rome and Koine Greek became a first or second language in the Roman Empire. The origin of Christianity can also be traced through Koine Greek, Medieval Greek, also known as Byzantine Greek, the continuation of Koine Greek in Byzantine Greece, up to the demise of the Byzantine Empire in the 15th century. Much of the written Greek that was used as the language of the Byzantine Empire was an eclectic middle-ground variety based on the tradition of written Koine. Modern Greek, Stemming from Medieval Greek, Modern Greek usages can be traced in the Byzantine period and it is the language used by the modern Greeks, and, apart from Standard Modern Greek, there are several dialects of it. In the modern era, the Greek language entered a state of diglossia, the historical unity and continuing identity between the various stages of the Greek language is often emphasised. Greek speakers today still tend to regard literary works of ancient Greek as part of their own rather than a foreign language and it is also often stated that the historical changes have been relatively slight compared with some other languages. According to one estimation, Homeric Greek is probably closer to demotic than 12-century Middle English is to modern spoken English, Greek is spoken by about 13 million people, mainly in Greece, Albania and Cyprus, but also worldwide by the large Greek diaspora. Greek is the language of Greece, where it is spoken by almost the entire population
11.
Keban Dam
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The Keban Dam is a hydroelectric dam on the Euphrates, located in the Elazığ Province of Turkey. The dam was the first and uppermost of several dams to be built on the Euphrates by Turkey. Construction of the dam commenced in 1966 and was completed in 1974, construction of the Keban Dam was first proposed in 1936 by the newly established Electric Affairs Survey Administration, but not started before 1966. Construction was carried out by the French-Italian consortium SCI-Impreglio and completed in 1974, estimates of the total construction cost vary between US$85 million and US$300 million. At that time, archaeological rescue missions had also carried out at important sites that were to be flooded. Flooding of the started in 1974 and led to the displacement of 25,000 people. During the flooding of the Keban Reservoir, Turkey maintained the discharge of the Euphrates at 450 cubic metres per second, as agreed with the countries of Syria. This dispute, exacerbated by drought which reduced the amount of water even further, was solved by mediation of Saudi Arabia. Reportedly, Keban Dam was the worlds eighteenth-tallest dam at completion, creating Turkeys largest man-made reservoir, the construction of the dam and its subsequent reservoir resulted in involuntary resettlement of approximately 25,0000 people. From 1968 to 1974, the Euphrates and Murat river valleys were the scene of intense archaeological survey, the lake formed by the dam is mostly narrow, hemmed in by deep rock valleys. No archaeological sites were found in the survey of these valleys, the Murat valley opens up in two places, and it is here that archaeological settlement was concentrated. The Aşvan region, covering about 115 square kilometres, contained eleven archaeological sites, the other broadening of the valley, at the Altınova plain, was a well-defined area of thick and fertile alluvial soil. Archaeological survey located 36 sites, of one, Norşuntepe, covered 8.2 hectares. It was excavated by a German team led by Harald Hauptmann, the Altınova plain contained other relatively large mounds, including Tepecik, Korucutepe, Değirmentepe and Körtepe. The late Roman Karamagara Bridge, an example of an early pointed arch bridge, has been permanently submerged by the dam. The Keban Dam is a rockfill and concrete gravity hydroelectric dam operated by the State Hydraulic Works. The dam is 1,097 metres long and its crest is 207 metres above the level of the river-bed and its eight water turbines are capable of producing 1,330 MW. The storage capacity of Lake Keban is 30.6 cubic kilometres, apart from the Euphrates Valley directly upstream of the dam, the lake has also flooded parts of valleys of the Murat River and the Karasu, the two rivers from which the Euphrates emerges
12.
Classical Armenian
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Classical Armenian is the oldest attested form of the Armenian language. It was first written down at the beginning of the 5th century, many ancient manuscripts originally written in Ancient Greek, Persian, Hebrew, Syriac and Latin survive only in Armenian translation. Classical Armenian continues to be the language of the Armenian Apostolic Church and is often learned by Biblical, Intertestamental. Classical Armenian is also important for the reconstruction of the Proto-Indo-European language, there are seven monophthongs, /a/, /i/, /ə/ or schwa, /ɛ/ or open e, /e/ or closed e, /o/, and /u/. The vowel transcribed u is spelled using the Armenian letters for ow, there are also traditionally six diphthongs, ay, aw, ea, ew, iw, oy. In the following table is the Classical Armenian consonantal system, each phoneme has three symbols in the table. The letter f was introduced in the Medieval Period to represent the foreign sound /f/, list of Armenian writers Proto-Armenian language Armenian alphabet Adjarian, Hrachia. Etymological Root Dictionary of the Armenian Language, esquisse d’une grammaire comparée de l’arménien classique. An Introduction to the Study of Classical Armenian, wiesbaden, Dr. Ludwig Reichert Verlag,1975 Classical Armenian Online New Dictionary of the Armenian Language, Venice 1836-1837. The seminal dictionary of Classical Armenian, includes Armenian to Latin, and Armenian to Greek. Pocket Dictionary of the Armenian Language, Venice 1865, grabar Dictionary, Ruben Ghazarian, Yerevan,2000. Grabar Thesaurus, Ruben Ghazarian, Yerevan,2006, a grammar, Armenian and English by Paschal Aucher and Lord Byron
13.
Neo-Assyrian Empire
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The Neo-Assyrian Empire was an Iron Age Mesopotamian empire, in existence between 911 and 612 BC. The Assyrians perfected early techniques of imperial rule, many of which became standard in later empires, the Neo-Assyrian Empire succeeded the Old Assyrian Empire, and the Middle Assyrian Empire of the Late Bronze Age. During this period, Aramaic was also made a language of the empire. Upon the death of Ashurbanipal in 627 BC, the empire began to due to a brutal. In 616 BC, Cyaxares king of the Medes and Persians made alliances with Nabopolassar ruler of the Babylonians and Chaldeans, Assyria was originally an Akkadian kingdom which evolved in the 25th to 24th centuries BC. The urbanised Akkadian speaking nation of Assyria emerged in the mid 21st century BC, during the 20th century BC, it established colonies in Asia Minor, and under the 20th century BC King Ilushuma, Assyria conducted many successful raids against the states of the south. Ashur-uballit extended Assyrian control over the farming lands of Nineveh. Tiglath-Pileser controlled the caravan routes that crossed the fertile crescent from the Mediterranean to the Persian Gulf. Much campaigning by Tiglath-Pileser and succeeding kings was directed against Aramaean pastoralist groups in Syria, by the end of the 2nd millennium BC, the Aramaean expansion had resulted in the loss of much Assyrian territory in Upper Mesopotamia. After the death of Tiglath-Pileser I in 1076 BC, Assyria was in decline for the next 150 years. The period from 1200 BC to 900 BC was an age for the entire Near East, North Africa, Caucasus, Mediterranean and Balkan regions, with great upheavals. Adad-nirari II and his successors campaigned on a basis for part of every year with an exceptionally well-organized army. He subjugated the areas previously under only nominal Assyrian vassalage, conquering and deporting Aramean and Hurrian populations in the north to far-off places. Adadinirari II then twice attacked and defeated Shamash-mudammiq of Babylonia, annexing an area of land north of the Diyala river. He made further gains over Babylonia under Nabu-shuma-ukin I later in his reign and he was succeeded by Tukulti-Ninurta II in 891 BC, who further consolidated Assyrias position and expanded northwards into Asia Minor and the Zagros Mountains during his short reign. The next king, Ashurnasirpal II, embarked on a vast program of expansion, during his rule, Assyria recovered much of the territory that it had lost around 1100 BC at the end of the Middle Assyrian period. Ashurnasirpal II also campaigned in the Zagros Mountains in modern Iran, repressing a revolt against Assyrian rule by the Lullubi, the Assyrians began boasting in their ruthlessness around this time. Ashurnasirpal II also moved his capital to the city of Kalhu, the palaces, temples and other buildings raised by him bear witness to a considerable development of wealth and art
14.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
