1.
Iraq
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The capital, and largest city, is Baghdad. The main ethnic groups are Arabs and Kurds, others include Assyrians, Turkmen, Shabakis, Yazidis, Armenians, Mandeans, Circassians, around 95% of the countrys 36 million citizens are Muslims, with Christianity, Yarsan, Yezidism, and Mandeanism also present. The official languages of Iraq are Arabic and Kurdish, two major rivers, the Tigris and Euphrates, run south through Iraq and into the Shatt al-Arab near the Persian Gulf. These rivers provide Iraq with significant amounts of fertile land, the region between the Tigris and Euphrates rivers, historically known as Mesopotamia, is often referred to as the cradle of civilisation. It was here that mankind first began to read, write, create laws, the area has been home to successive civilisations since the 6th millennium BC. Iraq was the centre of the Akkadian, Sumerian, Assyrian and it was also part of the Median, Achaemenid, Hellenistic, Parthian, Sassanid, Roman, Rashidun, Umayyad, Abbasid, Ayyubid, Mongol, Safavid, Afsharid, and Ottoman empires. Iraqs modern borders were mostly demarcated in 1920 by the League of Nations when the Ottoman Empire was divided by the Treaty of Sèvres, Iraq was placed under the authority of the United Kingdom as the British Mandate of Mesopotamia. A monarchy was established in 1921 and the Kingdom of Iraq gained independence from Britain in 1932, in 1958, the monarchy was overthrown and the Iraqi Republic created. Iraq was controlled by the Arab Socialist Baath Party from 1968 until 2003, after an invasion by the United States and its allies in 2003, Saddam Husseins Baath Party was removed from power and multi-party parliamentary elections were held in 2005. The American presence in Iraq ended in 2011, but the Iraqi insurgency continued and intensified as fighters from the Syrian Civil War spilled into the country, the Arabic name العراق al-ʿIrāq has been in use since before the 6th century. There are several suggested origins for the name, one dates to the Sumerian city of Uruk and is thus ultimately of Sumerian origin, as Uruk was the Akkadian name for the Sumerian city of Urug, containing the Sumerian word for city, UR. An Arabic folk etymology for the name is rooted, well-watered. During the medieval period, there was a region called ʿIrāq ʿArabī for Lower Mesopotamia and ʿIrāq ʿajamī, for the region now situated in Central and Western Iran. The term historically included the south of the Hamrin Mountains. The term Sawad was also used in early Islamic times for the region of the plain of the Tigris and Euphrates rivers. In English, it is either /ɪˈrɑːk/ or /ɪˈræk/, the American Heritage Dictionary, the pronunciation /aɪˈræk/ is frequently heard in U. S. media. Since approximately 10,000 BC, Iraq was one of centres of a Caucasoid Neolithic culture where agriculture, the following Neolithic period is represented by rectangular houses. At the time of the pre-pottery Neolithic, people used vessels made of stone, gypsum, finds of obsidian tools from Anatolia are evidences of early trade relations
2.
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
3.
Upper Mesopotamia
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Upper Mesopotamia is the name used for the uplands and great outwash plain of northwestern Iraq, northeastern Syria and southeastern Turkey, in the northern Middle East. This region is approximately correspondent with what was Assyria from the 25th century BC through to the mid-7th century AD and it extends down the Tigris to Samarra and down the Euphrates to Hit. The Khabur River runs for over 400 km across the plain, from Turkey in the north, the major settlements are Mosul, Deir ez-Zor, Raqqa, Al Hasakah, Diyarbakır and Qamishli. The western, Syrian part, is contiguous with the Syrian Al-Hasakah Governorate and is described as Syrias breadbasket. The eastern, Iraqi part, includes and extends slightly beyond the Iraqi Ninewa Governorate, in the north it includes the Turkish provinces of Şanlıurfa, Mardin, and parts of Diyarbakır Province. The name al-Jazira has been used since the 7th century CE by Islamic sources to refer to the section of Mesopotamia. The name means island, and at one time referred to the land between the two rivers, which in Aramaic is Bit Nahren. Historically the name referred to as little as the Sinjar plain coming down from the Sinjar Mountains, in pre-Abbasid times the western and eastern boundaries seem to have fluctuated, sometimes including what is now northern Syria to the west and Adiabene in the east. Al-Jazira is characterised as an outwash or alluvial plain, quite distinct from the Syrian Desert and lower-lying central Mesopotamia, however the area includes eroded hills, the region has several parts to it. In the northwest is one of the largest salt flats in the world, further south, extending from Mosul to near Basra is a sandy desert not unlike the Empty Quarter. In the late 20th and early 21st centuries the region has been plagued by drought and this is the area where the earliest signs of agriculture and domestication of animals have been found, and thus the starting point leading to civilization and the modern world. Al-Jazirah includes the mountain Karaca Dağ in southern Turkey, where the closest relative to modern wheat still grows wild, domestication of goats and sheep followed within a few generations, but didnt become widespread for more than a millennium. Weaving and pottery followed about two years later. Further surprises followed in the 1990s with the finds of the megalithic structures at Göbekli Tepe in south-eastern Turkey. The earliest of these apparently ritual buildings are from before 9000 BC—over five thousand years older than Stonehenge—and thus the absolute oldest known megalithic structures anywhere, as far as we know today no well-established farming societies existed at the time. Farming seemed to be experimental and only a smallish supplement to continued hunting and gathering. After all, Göbekli Tepe lies just 32 km from Karaca Dağ, the questions raised by Göbekli Tepe have led to intense and creative discussions among archeologists of the Middle East. Excavations at Göbekli Tepe continues, only about 5 percent has been revealed so far, Upper Mesopotamia is the heartland of ancient Assyria, founded circa the 25th century BC
4.
Tigris
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The Tigris is the eastern member of the two great rivers that define Mesopotamia, the other being the Euphrates. The river flows south from the mountains of southeastern Turkey through Iraq, the Tigris is 1,850 km long, rising in the Taurus Mountains of eastern Turkey about 25 km southeast of the city of Elazig and about 30 km from the headwaters of the Euphrates. The river then flows for 400 km through Turkish territory before becoming the border between Syria and Turkey and this stretch of 44 km is the only part of the river that is located in Syria. Close to its confluence with the Euphrates, the Tigris splits into several channels, First, the artificial Shatt al-Hayy branches off, to join the Euphrates near Nasiriyah. Second, the Shatt al-Muminah and Majar-al-Kabir branch off to feed the Central Marshes, further downstream, two other distributary channels branch off, which feed the Hawizeh Marshes. The main channel continues southwards and is joined by the Al-Kassarah, finally, the Tigris joins the Euphrates near al-Qurnah to form the Shatt-al-Arab. According to Pliny and other ancient historians, the Euphrates originally had its outlet into the sea separate from that of the Tigris, Baghdad, the capital of Iraq, stands on the banks of the Tigris. The port city of Basra straddles the Shatt al-Arab, in ancient times, many of the great cities of Mesopotamia stood on or near the Tigris, drawing water from it to irrigate the civilization of the Sumerians. Notable Tigris-side cities included Nineveh, Ctesiphon, and Seleucia, while the city of Lagash was irrigated by the Tigris via a canal dug around 2400 B. C, the Tigris has long been an important transport route in a largely desert country. Shallow-draft vessels can go as far as Baghdad, but rafts are needed for transport upstream to Mosul, General Francis Rawdon Chesney hauled two steamers overland through Syria in 1836 to explore the possibility of an overland and river route to India. One steamer, the Tigris, was wrecked in a storm which sank, Chesney proved the river navigable to powered craft. Later, the Euphrates and Tigris Steam Navigation Company was established in 1861 by the Lynch Brothers trading company and they had 2 steamers in service. By 1908 ten steamers were on the river, tourists boarded steam yachts to venture inland as this was the first age of archaeological tourism, and the sites of Ur and Ctesiphon became popular to European travelers. In the First World War, during the British conquest of Ottoman Mesopotamia, Indian, see Siege of Kut and the Fall of Baghdad. The Tigris Flotilla included vessels Clio, Espiegle, Lawrence, Odin, armed tug Comet, armed launches Lewis Pelly, Miner, Shaitan, Sumana, and stern wheelers Muzaffari/Mozaffir. These were joined by Royal Navy Fly-class gunboats Butterfly, Cranefly, Dragonfly, Mayfly, Sawfly, Snakefly, and Mantis, Moth, the Ancient Greek form Tigris was borrowed from Old Persian Tigrā, itself from Elamite Tigra, itself from Sumerian Idigna. The Sumerian form was borrowed into Akkadian as Idiqlat, and from there into the other Semitic languages, another name for the Tigris used in Middle Persian was Arvand Rud, literally swift river. Today, however, Arvand Rud refers to the confluence of the Euphrates, in Kurdish, it is also known as Ava Mezin, the Great Water
5.
Iraqi Kurdistan
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Iraqi Kurdistan, officially called the Kurdistan Region by the Iraqi constitution, is located in the north of Iraq and constitutes the countrys only autonomous region. The region is governed by the Kurdistan Regional Government, with the capital being Erbil. Kurdistan is a democracy with its own regional Parliament that consists of 111 seats. Masoud Barzani, who was elected as president in 2005, was re-elected in 2009. In August 2013 the parliament extended his presidency for two years. His presidency concluded on 19 August 2015 after the parties failed to reach an agreement over extending his term. The new Constitution of Iraq defines the Kurdistan Region as an entity of Iraq. The four governorates of Duhok, Hawler, Silemani, and Halabja comprise around 41,710 square kilometres and have a population of 5.5 million. In 2014, during the 2014 Iraq Crisis, Iraqi Kurdistans forces also took much of the disputed territories of Northern Iraq. The establishment of the Kurdistan Region dates back to the March 1970 autonomy agreement between the Kurdish opposition and the Iraqi government after years of heavy fighting, further, the 1980–88 Iran–Iraq War, especially the Iraqi Armys Al-Anfal Campaign, devastated the population and environment of Iraqi Kurdistan. As Kurds continued to fight government troops, Iraqi forces finally left Kurdistan in October 1991, in 1992, the major political parties in the region, the Kurdistan Democratic Party and the Patriotic Union of Kurdistan, established the semi-autonomous Kurdistan Regional Government. The 2003 invasion of Iraq and subsequent political changes led to the ratification of a new constitution in 2005, the name Kurdistan literally means Land of the Kurds. The suffix -stan is Iranian for place of or country, in English translations of the Constitution of Iraq, it is called Kurdistan, four times in the phrase region of Kurdistan and once in the phrase Kurdistan region. The regional government calls it the Kurdistan Region, the full name of the government is the Kurdistan Regional Government, abbreviated KRG. Kurds also refer to the region as Başûrê Kurdistanê or Başûrî Kurdistan, during the Baath Party administration in the 1970s and 1980s, the region was called the Kurdish Autonomous Region. The Kurdistan Region is largely mountainous, with the highest point being a 3,611 m point known locally as Cheekha Dar, the mountains are part of the larger Zagros mountain range which also extends into Iran. There are many rivers running through the region, which is distinguished by its fertile lands, plentiful water, the Great Zab and the Little Zab flow from the east to the west in the region. The Tigris river enters Iraqi Kurdistan from Turkish Kurdistan, the mountainous nature of Iraqi Kurdistan, the difference of temperatures in its various parts, and its wealth of waters make it a land of agriculture and tourism
6.
Lower Mesopotamia
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In the Iron Age, it was controlled by the Neo-Assyrian and Neo-Babylonian Empires. The Sumerians and Akkadians dominated Mesopotamia from the beginning of history to the fall of Babylon in 539 BC. It fell to Alexander the Great in 332 BC, and after his death, around 150 BC, Mesopotamia was under the control of the Parthian Empire. Mesopotamia became a battleground between the Romans and Parthians, with parts of Mesopotamia coming under ephemeral Roman control. In AD226, eastern part of it fell to the Sassanid Persians, division of Mesopotamia between Roman and Sassanid Empires lasted until the 7th century Muslim conquest of Persia of the Sasanian Empire and Muslim conquest of the Levant from Byzantines. A number of primarily neo-Assyrian and Christian native Mesopotamian states existed between the 1st century BC and 3rd century AD, including Adiabene, Osroene, and Hatra, Mesopotamia is the site of the earliest developments of the Neolithic Revolution from around 10,000 BC. The regional toponym Mesopotamia comes from the ancient Greek root words μέσος middle and ποταμός river and it is used throughout the Greek Septuagint to translate the Hebrew equivalent Naharaim. In the Anabasis, Mesopotamia was used to designate the land east of the Euphrates in north Syria, the Aramaic term biritum/birit narim corresponded to a similar geographical concept. The neighbouring steppes to the west of the Euphrates and the part of the Zagros Mountains are also often included under the wider term Mesopotamia. A further distinction is made between Northern or Upper Mesopotamia and Southern or Lower Mesopotamia. Upper Mesopotamia, also known as the Jazira, is the area between the Euphrates and the Tigris from their sources down to Baghdad, Lower Mesopotamia is the area from Baghdad to the Persian Gulf and includes Kuwait and parts of western Iran. In modern academic usage, the term Mesopotamia often also has a chronological connotation and it is usually used to designate the area until the Muslim conquests, with names like Syria, Jazirah, and Iraq being used to describe the region after that date. It has been argued that these later euphemisms are Eurocentric terms attributed to the region in the midst of various 19th-century Western encroachments, Mesopotamia encompasses the land between the Euphrates and Tigris rivers, both of which have their headwaters in the Armenian Highlands. Both rivers are fed by tributaries, and the entire river system drains a vast mountainous region. Overland routes in Mesopotamia usually follow the Euphrates because the banks of the Tigris are frequently steep and difficult. The climate of the region is semi-arid with a vast desert expanse in the north which gives way to a 15,000 square kilometres region of marshes, lagoons, mud flats, in the extreme south, the Euphrates and the Tigris unite and empty into the Persian Gulf. In the marshlands to the south of the area, a complex water-borne fishing culture has existed since prehistoric times, periodic breakdowns in the cultural system have occurred for a number of reasons. Alternatively, military vulnerability to invasion from marginal hill tribes or nomadic pastoralists has led to periods of trade collapse and these trends have continued to the present day in Iraq
7.
Persian Gulf
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The Persian Gulf is a mediterranean sea in Western Asia. The body of water is an extension of the Indian Ocean through the Strait of Hormuz, the Shatt al-Arab river delta forms the northwest shoreline. The Persian Gulf was a battlefield of the 1980–1988 Iran–Iraq War and it is the namesake of the 1991 Gulf War, the largely air- and land-based conflict that followed Iraqs invasion of Kuwait. The gulf has many fishing grounds, extensive coral reefs, and abundant pearl oysters, the body of water is historically and internationally known as the Persian Gulf. Some Arab governments refer to it as the Arabian Gulf or The Gulf, the name Gulf of Iran is used by the International Hydrographic Organization. The Persian Gulf is geologically young, having been formed around 15,000 years ago. Its length is 989 kilometres, with Iran covering most of the northern coast, the Persian Gulf is about 56 km wide at its narrowest, in the Strait of Hormuz. The waters are very shallow, with a maximum depth of 90 metres. Various small islands lie within the Persian Gulf, some of which are the subject of territorial disputes between the states of the region. The International Hydrographic Organization defines the Persian Gulfs southern limit as The Northwestern limit of Gulf of Oman and this limit is defined as A line joining Ràs Limah on the coast of Arabia and Ràs al Kuh on the coast of Iran. The Persian Gulf and its areas are the worlds largest single source of crude oil. Safaniya Oil Field, the worlds largest offshore oilfield, is located in the Persian Gulf, large gas finds have also been made, with Qatar and Iran sharing a giant field across the territorial median line. Using this gas, Qatar has built up a substantial liquefied natural gas, the oil-rich countries that have a coastline on the Persian Gulf are referred to as the Persian Gulf States. In 550 BC, the Achaemenid Empire established the first ancient empire in Persis, consequently, in the Greek sources, the body of water that bordered this province came to be known as the Persian Gulf. In the travel account of Pythagoras, several chapters are related to description of his travels accompanied by the Achaemenid king Darius the Great, to Susa and Persepolis, and the area is described. This water channel separates the Iran Plateau from the Arabia Plate, has enjoyed an Iranian Identity since at least 2200 years ago. Before being given its present name, the Persian Gulf was called many different names, the classical Greek writers, like Herodotus, called it the Red Sea. In Babylonian texts, it was known as the sea above Akkad, the name of the gulf, historically and internationally known as the Persian Gulf after the land of Persia, has been disputed by some Arab countries since the 1960s
8.
Balkans
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The Balkan Peninsula, or the Balkans, is a peninsula and a cultural area in Eastern and Southeastern Europe with various and disputed borders. The region takes its name from the Balkan Mountains that stretch from the Serbia-Bulgaria border to the Black Sea, the highest point of the Balkans is Mount Musala 2,925 metres in the Rila mountain range. In Turkish, Balkan means a chain of wooded mountains, the name is still preserved in Central Asia with the Balkan Daglary and the Balkan Province of Turkmenistan. A less popular hypothesis regarding its etymology is that it derived from the Persian Balā-Khāna, from Antiquity through the Middle Ages, the Balkan Mountains had been called by the local Thracian name Haemus. According to Greek mythology, the Thracian king Haemus was turned into a mountain by Zeus as a punishment, a reverse name scheme has also been suggested. D. Dechev considers that Haemus is derived from a Thracian word *saimon, a third possibility is that Haemus derives from the Greek word haema meaning blood. The myth relates to a fight between Zeus and the monster/titan Typhon, Zeus injured Typhon with a thunder bolt and Typhons blood fell on the mountains, from which they got their name. The earliest mention of the name appears in an early 14th-century Arab map, the Ottomans first mention it in a document dated from 1565. There has been no other documented usage of the word to refer to the region before that, there is also a claim about an earlier Bulgar Turkic origin of the word popular in Bulgaria, however it is only an unscholarly assertion. The word was used by the Ottomans in Rumelia in its meaning of mountain, as in Kod̲j̲a-Balkan, Čatal-Balkan, and Ungurus-Balkani̊. The concept of the Balkans was created by the German geographer August Zeune in 1808, during the 1820s, Balkan became the preferred although not yet exclusive term alongside Haemus among British travelers. Among Russian travelers not so burdened by classical toponymy, Balkan was the preferred term, zeunes goal was to have a geographical parallel term to the Italic and Iberian Peninsula, and seemingly nothing more. The gradually acquired political connotations are newer and, to a large extent, after the dissolution of Yugoslavia beginning in June 1991, the term Balkans again received a negative meaning, especially in Croatia and Slovenia, even in casual usage. A European Union initiative of 1999 is called the Stability Pact for South Eastern Europe, and its northern boundary is often given as the Danube, Sava and Kupa Rivers. The Balkan Peninsula has an area of about 470,000 km2. It is more or less identical to the known as Southeastern Europe. As of 1920 until World War II, Italy included Istria, the current territory of Italy includes only the small area around Trieste inside the Balkan Peninsula. However, the regions of Trieste and Istria are not usually considered part of the Balkans by Italian geographers, the Western Balkans is a neologism coined to describe the countries of ex-Yugoslavia and Albania
9.
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
10.
Iran
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Iran, also known as Persia, officially the Islamic Republic of Iran, is a sovereign state in Western Asia. Comprising a land area of 1,648,195 km2, it is the second-largest country in the Middle East, with 82.8 million inhabitants, Iran is the worlds 17th-most-populous country. It is the country with both a Caspian Sea and an Indian Ocean coastline. The countrys central location in Eurasia and Western Asia, and its proximity to the Strait of Hormuz, Tehran is the countrys capital and largest city, as well as its leading economic and cultural center. Iran is the site of to one of the worlds oldest civilizations, the area was first unified by the Iranian Medes in 625 BC, who became the dominant cultural and political power in the region. The empire collapsed in 330 BC following the conquests of Alexander the Great, under the Sassanid Dynasty, Iran again became one of the leading powers in the world for the next four centuries. Beginning in 633 AD, Arabs conquered Iran and largely displaced the indigenous faiths of Manichaeism and Zoroastrianism by Islam, Iran became a major contributor to the Islamic Golden Age that followed, producing many influential scientists, scholars, artists, and thinkers. During the 18th century, Iran reached its greatest territorial extent since the Sassanid Empire, through the late 18th and 19th centuries, a series of conflicts with Russia led to significant territorial losses and the erosion of sovereignty. Popular unrest culminated in the Persian Constitutional Revolution of 1906, which established a monarchy and the countrys first legislative body. Following a coup instigated by the U. K. Growing dissent against foreign influence and political repression led to the 1979 Revolution, Irans rich cultural legacy is reflected in part by its 21 UNESCO World Heritage Sites, the third-largest number in Asia and 11th-largest in the world. Iran is a member of the UN, ECO, NAM, OIC. Its political system is based on the 1979 Constitution which combines elements of a democracy with a theocracy governed by Islamic jurists under the concept of a Supreme Leadership. A multicultural country comprising numerous ethnic and linguistic groups, most inhabitants are Shia Muslims, the largest ethnic groups in Iran are the Persians, Azeris, Kurds and Lurs. Historically, Iran has been referred to as Persia by the West, due mainly to the writings of Greek historians who called Iran Persis, meaning land of the Persians. As the most extensive interactions the Ancient Greeks had with any outsider was with the Persians, however, Persis was originally referred to a region settled by Persians in the west shore of Lake Urmia, in the 9th century BC. The settlement was then shifted to the end of the Zagros Mountains. In 1935, Reza Shah requested the international community to refer to the country by its native name, opposition to the name change led to the reversal of the decision, and Professor Ehsan Yarshater, editor of Encyclopædia Iranica, propagated a move to use Persia and Iran interchangeably
11.
Afghanistan
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Afghanistan, officially the Islamic Republic of Afghanistan, is a landlocked country located within South Asia and Central Asia. It has a population of approximately 32 million, making it the 42nd most populous country in the world. It is bordered by Pakistan in the south and east, Iran in the west, Turkmenistan, Uzbekistan, and Tajikistan in the north and its territory covers 652,000 km2, making it the 41st largest country in the world. The land also served as the source from which the Kushans, Hephthalites, Samanids, Saffarids, Ghaznavids, Ghorids, Khiljis, Mughals, Hotaks, Durranis, the political history of the modern state of Afghanistan began with the Hotak and Durrani dynasties in the 18th century. In the late 19th century, Afghanistan became a state in the Great Game between British India and the Russian Empire. Following the Third Anglo-Afghan War in 1919, King Amanullah unsuccessfully attempted to modernize the country and it remained peaceful during Zahir Shahs forty years of monarchy. A series of coups in the 1970s was followed by a series of wars that devastated much of Afghanistan. The name Afghānistān is believed to be as old as the ethnonym Afghan, the root name Afghan was used historically in reference to a member of the ethnic Pashtuns, and the suffix -stan means place of in Persian. Therefore, Afghanistan translates to land of the Afghans or, more specifically in a historical sense, however, the modern Constitution of Afghanistan states that he word Afghan shall apply to every citizen of Afghanistan. An important site of historical activities, many believe that Afghanistan compares to Egypt in terms of the historical value of its archaeological sites. The country sits at a unique nexus point where numerous civilizations have interacted and it has been home to various peoples through the ages, among them the ancient Iranian peoples who established the dominant role of Indo-Iranian languages in the region. At multiple points, the land has been incorporated within large regional empires, among them the Achaemenid Empire, the Macedonian Empire, the Indian Maurya Empire, and the Islamic Empire. Archaeological exploration done in the 20th century suggests that the area of Afghanistan has been closely connected by culture and trade with its neighbors to the east, west. Artifacts typical of the Paleolithic, Mesolithic, Neolithic, Bronze, urban civilization is believed to have begun as early as 3000 BCE, and the early city of Mundigak may have been a colony of the nearby Indus Valley Civilization. More recent findings established that the Indus Valley Civilisation stretched up towards modern-day Afghanistan, making the ancient civilisation today part of Pakistan, Afghanistan, in more detail, it extended from what today is northwest Pakistan to northwest India and northeast Afghanistan. An Indus Valley site has found on the Oxus River at Shortugai in northern Afghanistan. There are several smaller IVC colonies to be found in Afghanistan as well, after 2000 BCE, successive waves of semi-nomadic people from Central Asia began moving south into Afghanistan, among them were many Indo-European-speaking Indo-Iranians. These tribes later migrated further into South Asia, Western Asia, the region at the time was referred to as Ariana
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Himalayas
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The Himalayas, or Himalaya, form a mountain range in Asia separating the plains of the Indian subcontinent from the Tibetan Plateau. The Himalayan range has the Earths highest peaks, including the highest, the Himalayas include over a hundred mountains exceeding 7,200 metres in elevation. By contrast, the highest peak outside Asia – Aconcagua, in the Andes – is 6,961 metres tall. The Himalayas are spread across five countries, Bhutan, India, Nepal, China, the Himalayan range is bordered on the northwest by the Karakoram and Hindu Kush ranges, on the north by the Tibetan Plateau, and on the south by the Indo-Gangetic Plain. Some of the major rivers, the Indus, the Ganges, and the Tsangpo-Brahmaputra, rise in the Himalayas. The Himalayas have profoundly shaped the cultures of South Asia, many Himalayan peaks are sacred in Hinduism and Buddhism. Lifted by the subduction of the Indian tectonic plate under the Eurasian Plate and its western anchor, Nanga Parbat, lies just south of the northernmost bend of Indus river. Its eastern anchor, Namcha Barwa, is just west of the bend of the Tsangpo river. The range varies in width from 400 kilometres in the west to 150 kilometres in the east, the name of the range derives from the Sanskrit Himā-laya, from himá and ā-laya. They are now known as the Himalaya Mountains, usually shortened to the Himalayas, formerly, they were described in the singular as the Himalaya. This was also previously transcribed Himmaleh, as in Emily Dickinsons poetry and Henry David Thoreaus essays. The mountains are known as the Himālaya in Nepali and Hindi, the Himalaya or The Land of Snow in Tibetan, the Hamaleh Mountain Range in Urdu, the flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice, the amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the high snow line supports a variety of distinct plant. The extremes of high altitude combined with extreme cold favor extremophile organisms, the unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations, the oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some species, especially rhododendron, apple. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet, the Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock
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Desert
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A desert is a barren area of land where little precipitation occurs and consequently living conditions are hostile for plant and animal life. The lack of vegetation exposes the unprotected surface of the ground to the processes of denudation, about one third of the land surface of the world is arid or semi-arid. This includes much of the regions where little precipitation occurs. Deserts can be classified by the amount of precipitation falls, by the temperature that prevails. Deserts are formed by weathering processes as large variations in temperature between day and night put strains on the rocks which consequently break in pieces, although rain seldom occurs in deserts, there are occasional downpours that can result in flash floods. Rain falling on hot rocks can cause them to shatter and the resulting fragments and this picks up particles of sand and dust and wafts them aloft in sand or dust storms. Wind-blown sand grains striking any solid object in their path can abrade the surface, rocks are smoothed down, and the wind sorts sand into uniform deposits. The grains end up as level sheets of sand or are piled high in billowing sand dunes, other deserts are flat, stony plains where all the fine material has been blown away and the surface consists of a mosaic of smooth stones. These areas are known as desert pavements and little further erosion takes place, other desert features include rock outcrops, exposed bedrock and clays once deposited by flowing water. Temporary lakes may form and salt pans may be left when waters evaporate, there may be underground sources of water in the form of springs and seepages from aquifers. Where these are found, oases can occur, plants and animals living in the desert need special adaptations to survive in the harsh environment. Plants tend to be tough and wiry with small or no leaves, water-resistant cuticles, some annual plants germinate, bloom and die in the course of a few weeks after rainfall while other long-lived plants survive for years and have deep root systems able to tap underground moisture. Animals need to cool and find enough food and water to survive. Many are nocturnal and stay in the shade or underground during the heat of the day and they tend to be efficient at conserving water, extracting most of their needs from their food and concentrating their urine. Some animals remain in a state of dormancy for long periods and they then reproduce rapidly while conditions are favorable before returning to dormancy. People have struggled to live in deserts and the surrounding lands for millennia. Nomads have moved their flocks and herds to wherever grazing is available, the cultivation of semi-arid regions encourages erosion of soil and is one of the causes of increased desertification. Many trade routes have been forged across deserts, especially across the Sahara Desert, large numbers of slaves were also taken northwards across the Sahara
14.
Saudi Arabia
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Saudi Arabia is bordered by Jordan and Iraq to the north, Kuwait to the northeast, Qatar, Bahrain and the United Arab Emirates to the east, Oman to the southeast and Yemen to the south. It is separated from Israel and Egypt by the Gulf of Aqaba and it is the only nation with both a Red Sea coast and a Persian Gulf coast and most of its terrain consists of arid desert and mountains. The area of modern-day Saudi Arabia formerly consisted of four regions, Hejaz, Najd and parts of Eastern Arabia. The Kingdom of Saudi Arabia was founded in 1932 by Ibn Saud and he united the four regions into a single state through a series of conquests beginning in 1902 with the capture of Riyadh, the ancestral home of his family, the House of Saud. Saudi Arabia has since been a monarchy, effectively a hereditary dictatorship governed along Islamic lines. The ultraconservative Wahhabi religious movement within Sunni Islam has been called the predominant feature of Saudi culture, with its global spread largely financed by the oil and gas trade. Saudi Arabia is sometimes called the Land of the Two Holy Mosques in reference to Al-Masjid al-Haram and Al-Masjid an-Nabawi, the state has a total population of 28.7 million, of which 20 million are Saudi nationals and 8 million are foreigners. The states official language is Arabic, petroleum was discovered on 3 March 1938 and followed up by several other finds in the Eastern Province. Saudi Arabia has since become the worlds largest oil producer and exporter, controlling the second largest oil reserves. The kingdom is categorized as a World Bank high-income economy with a high Human Development Index and is the only Arab country to be part of the G-20 major economies. However, the economy of Saudi Arabia is the least diversified in the Gulf Cooperation Council, the state has attracted criticism for its treatment of women and use of capital punishment. Saudi Arabia is an autocracy, has the fourth highest military expenditure in the world. Saudi Arabia is considered a regional and middle power, in addition to the GCC, it is an active member of the Organisation of Islamic Cooperation and OPEC. Following the unification of the Hejaz and Nejd kingdoms, the new state was named al-Mamlakah al-ʻArabīyah as-Suʻūdīyah by royal decree on 23 September 1932 by its founder, Abdulaziz Al Saud. Although this is translated as the Kingdom of Saudi Arabia in English it literally means the Saudi Arab kingdom. Its inclusion expresses the view that the country is the possession of the royal family. Al Saud is an Arabic name formed by adding the word Al, meaning family of or House of, in the case of the Al Saud, this is the father of the dynastys 18th century founder, Muhammad bin Saud. There is evidence that human habitation in the Arabian Peninsula dates back to about 125,000 years ago
15.
Arabian Peninsula
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The Arabian Peninsula, simplified Arabia is a peninsula of Western Asia situated northeast of Africa on the Arabian plate. From a geological perspective, it is considered a subcontinent of Asia and it is the largest peninsula in the world, at 3,237,500 km2. The Arabian Peninsula consists of the countries Yemen, Oman, Qatar, Bahrain, Kuwait, Saudi Arabia, the Arabian Peninsula plays a critical geopolitical role in the Middle East and the Arab world due to its vast reserves of oil and natural gas. Before the modern era, it was divided into four regions, Hejaz, Najd, Southern Arabia. Hejaz and Najd make up most of Saudi Arabia, Southern Arabia consists of Yemen and some parts of Saudi Arabia and Oman. Eastern Arabia consists of the coastal strip of the Persian Gulf. The most prominent feature of the peninsula is desert, but in the southwest there are mountain ranges, harrat ash Shaam is a large volcanic field that extends from the northwestern Arabian Peninsula into Jordan and southern Syria. The peninsulas constituent countries are Kuwait, Bahrain, Qatar, the island nation of Bahrain lies off the east coast of the peninsula. Six countries form the Gulf Cooperation Council, however, this is a disputed term. The Kingdom of Saudi Arabia covers the part of the peninsula. The majority of the population of the live in Saudi Arabia. The peninsula contains the worlds largest reserves of oil, Saudi Arabia and the UAE are economically the wealthiest in the region. Qatar, a peninsula in the Persian Gulf on the larger peninsula, is home of the Arabic-language television station Al Jazeera. Kuwait, on the border with Iraq, is an important country strategically, though historically lightly populated, political Arabia is noted for a high population growth rate - as the result of both very strong inflows of migrant labor as well as sustained high birth rates. The population tends to be young and heavily skewed gender ratio dominated by males. In many states, the number of South Asians exceeds that of the local citizenry, the four smallest states, which have their entire coastlines on the Persian Gulf, exhibit the worlds most extreme population growth, roughly tripling every 20 years. In 2014, the population of the Arabian Peninsula was 77,983,936. Listed here are the human Y-chromosome DNA haplogroups in Arabia Haplogroup J is the most abundant component in the Arabian peninsula and its two main subclades, show opposite latitudinal gradients in the Middle East
16.
History of geography
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The history of geography includes many histories of geography which have differed over time and between different cultural and political groups. In more recent developments, geography has become an academic discipline. Geography derives from the Greek γεωγραφία – geographia, a translation of which would be to describe or write about the Earth. The first person to use the word geography was Eratosthenes, however, there is evidence for recognizable practices of geography, such as cartography prior to the use of the term geography. The known world of Ancient Egypt saw the Nile as the centre, various oases were known to the east and west, and were considered locations of various gods 12. To the South lay the Kushitic region, known as far as the 4th cataract, punt was a region south along the shores of the Red Sea. Various Asiatic peoples were known as Retenu, Kanaan, Que, Harranu, at various times especially in the Late Bronze Age Egyptians had diplomatic and trade relationships with Babylonia and Elam. The Mediterranean was called the Great Green and was believed to be part of a world encircling ocean, Europe was unknown although may have become part of the Egyptian world view in Phoenician times. The oldest known world maps date back to ancient Babylon from the 9th century BC, the best known Babylonian world map, however, is the Imago Mundi of 600 BC. The accompanying text mentions seven outer regions beyond the encircling ocean, the descriptions of five of them have survived. The ancient Greeks saw the poet Homer as the founder of geography and his works the Iliad and the Odyssey are works of literature, but both contain a great deal of geographical information. Homer describes a circular world ringed by a massive ocean. The works show that the Greeks by the 8th century BC had considerable knowledge of the geography of the eastern Mediterranean. The poems contain a number of place names and descriptions. Thales of Miletus is one of the first known philosophers known to have wondered about the shape of the world and he proposed that the world was based on water, and that all things grew out of it. He also laid down many of the astronomical and mathematical rules that would allow geography to be studied scientifically and his successor Anaximander is the first person known to have attempted to create a scale map of the known world and to have introduced the gnomon to Ancient Greece. From these accounts he wrote a prose account of what was known of the world. A similar work, and one that survives today, is Herodotus Histories
17.
Clay tablet
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In the Ancient Near East, clay tablets were used as a writing medium, especially for writing in cuneiform, throughout the Bronze Age and well into the Iron Age. Cuneiform characters were imprinted on a wet clay tablet with a stylus often made of reed, once written upon, many tablets were dried in the sun or air, remaining fragile. Later, these clay tablets could be soaked in water. Other tablets, once written, were fired in hot kilns making them hard, collections of these clay documents made up the very first archives. They were at the root of first libraries, tens of thousands of written tablets, including many fragments, have been found in the Middle East. In the Minoan/Mycenaean civilizations, writing has not been observed for any use other than accounting, tablets serving as labels, with the impression of the side of a wicker basket on the back, and tablets showing yearly summaries, suggest a sophisticated accounting system. In this cultural region the tablets were never fired deliberately, as the clay was recycled on an annual basis, however, some of the tablets were fired as a result of uncontrolled fires in the buildings where they were stored. The rest are still tablets of unfired clay, and extremely fragile, some scholars are investigating the possibility of firing them now. Writing was not as we see it today, in that way, recorded accounts of amounts of goods involved in a transaction could be made. The clay tablet was thus being used by scribes to take down the events of what was happening during his time, Sumerians used what are known as pictograms. Pictograms are symbols that express a concept, a logogram. Early writing also began in Ancient Egypt using hieroglyphs, early hieroglyphs and some of the modern Chinese characters are other examples of pictographs. The Sumerians later shifted their writing to Cuneiform, defined as Wedge writing in Latin, clay tablets took the forms of myths, fables, essays, hymns, proverbs, epic poetry, laws, plants, and animals. What these clay tablets allowed was for individuals to record who, an example of these great stories was The Story of Gilgamesh. This story would tell of the flood that destroyed Sumer. Remedies and recipes that would have been unknown were then possible because of the clay tablet, some of the recipes were stew, which was made with goat, garlic, onions and sour milk. Communication grew faster as now there was a way to get messages across just like mail, important and private clay tablets were coated with an extra layer of clay, that no one else would read it. This means of communicating was used for over 3000 years in fifteen different languages, Sumerians, Babylonians and Eblaites all had their own clay tablet libraries
18.
Yorghan Tepe
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Nuzi was an ancient Mesopotamian city southwest of Kirkuk in modern Al Taamim Governorate of Iraq, located near the Tigris river. The site consists of one medium-sized multiperiod tell and two small single period mounds, the town of Gasur was apparently founded during the Akkadian Empire in the late third millennium BC. In the middle second millennium Hurrians absorbed the town and renamed it Nuzi, the history of the site during the intervening period is unclear, though the presence of a few cuneiform tables from Old Assyria indicates that trade with nearby Assur was taking place. After the fall of the Hurrian kingdom of Mitanni to the Hittites, Nuzi fell to the Assyrians, note that while Hurrian period is well known because those levels of the site were fully excavated, the earlier history is less firm because of only scanty digging. The history of Nuzi is closely interrelated with that of the towns of Eshnunna. While tablets from Yorghan Tepe began appearing back as far as 1896, the site has 15 occupation levels. The hundreds of tablets and other finds recovered were published in a series of volumes, more finds continue to be published to this day. To date, around 5000 tablets are known, mostly held at the Oriental Institute, the Harvard Semitic Museum, many are routine legal and business documents and about one quarter concern the business transactions of a single family. The vast majority of finds are from the Hurrian period during the second millennium BC with the remainder dating back to the towns founding during the Akkadian Empire. An archive contemporary to the Hurrian archive at Nuzi has been excavated from the Green Palace at the site of Tell al-Fakhar,35 kilometres southwest of Nuzi, perhaps the most famous item found is the Nuzi map, which is the oldest known map ever discovered. It is unknown exactly what the Nuzi map charts, even though the majority of the tablet is preserved, the Nuzi map is actually one of the so-called Gasur texts, and predates the invasion of the city of Gasur by the Hurrians, who renamed it Nuzi. The cache of economic and business documents among which the map was found date to the Old Akkadian period, Gasur was a thriving commercial center, and the texts reveal a varied business community with far reaching enterprises. It is possible that Ebla was a partner, and that the tablet, rather than a record of land-holdings. The tablet, which is approximately 6 x 6.5 cm. is inscribed only on the obverse and it shows the city of Maskan-dur-ebla in the lower left corner, as well and a canal/river and two mountain ranges. The best-known period in the history of Yorghan Tepe is by far one of the city of Nuzi in the 15th-14th centuries BC, Nuzi was a provincial town in the kingdom of Arrapha. It was administered by a governor from the palace, the palace, situated in the center of the mound, had many rooms arranged around a central courtyard. The functions of some of those rooms have been identified, reception areas, apartments, offices, kitchens, the walls were painted, as was seen in fragments unearthed in the ruins of the building. Junior officers of the administration are sukkallu, the district manager
19.
Harran
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Harran was a major ancient city in Upper Mesopotamia whose site is near the modern village of Altınbaşak, Turkey,44 kilometers southeast of Şanlıurfa. The location is in a district of Şanlıurfa Province that is also named Harran. It was known as Ḫarrānu in the Assyrian period, Ḫaran in the Hebrew Bible, Carrhae under the Roman and Byzantine empires, Hellenopolis in the Early Christian period, the earliest records of Harran come from Ebla tablets. From these, it is known that a king or mayor of Harran had married an Eblaite princess, Zugalum, who then became queen of Harran. It appears that Harran remained a part of the regional Eblaite kingdom for some time thereafter, royal letters from the city of Mari on the middle of the Euphrates, have confirmed that the area around the Balikh river remained occupied in c. the 19th century BCE. A confederation of tribes was especially active around the region near Harran at that time. By the 19th century BCE, Harran was established as a merchant outpost due to its ideal location, the community, well established before then, was situated along a trade route between the Mediterranean and the plains of the middle Tigris. It lay directly on the road from Antioch eastward to Nisibis, the Tigris could be followed down to the delta to Babylon. Not only did Harran have easy access to both the Assyrian and Babylonian roads, but also to north road to the Euphrates that provided access to Malatiyah. According to Roman authors such as Pliny the Elder, even through the classical period, in its prime Harran was a major Assyrian city which controlled the point where the road from Damascus joins the highway between Nineveh and Carchemish. This location gave Harran strategic value from an early date, because Harran had an abundance of goods that passed through its region, it became a target for raids. In the 18th century, Assyrian king Shamshi-Adad I launched an expedition to secure the Harranian trade route, after the Suppiluliuma I–Shattiwaza treaty between the Hittite Empire and Mitanni, Harran was burned by a Hittite army under Piyashshili in the course of the conquest of Mitanni. In the 13th century BCE, Assyrian king Adad-Nirari I reported that he conquered the fortress of Kharani and it is frequently mentioned in Assyrian inscriptions as early as the time of Tiglath-Pileser I, about 1100 BCE, under the name Harranu. Tiglath-Pileser had a fortress there, and mentioned that he was pleased with the abundance of elephants in the region, 10th-century BCE inscriptions reveal that Harran had some privileges of fiscal exemption and freedom from certain forms of military obligations. It had even been termed as the city of Harran. However, in 763 BCE, it was sacked by a Harranian rebellion against Assyrian control that resulted in the loss of those privileges, not until Sargon II restored order, in the late 8th century BCE, were those privileges restored. Harran was besieged and conquered by Nabopolassar and Cyaxares in 610 BCE and it was briefly retaken by Ashur-uballit II and his Egyptian allies in 609 BCE, before it finally fell to the Medes and Babylonians in 605 BCE. Harran became part of the Median Empire after the fall of Assyria and it became part of the Persian province of Athura, the Persian word for Assyria
20.
Babylon
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Babylon was a major city of ancient Mesopotamia in the fertile plain between the Tigris and Euphrates rivers. The city was built upon the Euphrates and divided in parts along its left and right banks. Babylon was originally a small Semitic Akkadian city dating from the period of the Akkadian Empire c.2300 BC, the town attained independence as part of a small city-state with the rise of the First Amorite Babylonian Dynasty in 1894 BC. Babylon grew and South Mesopotamia came to be known as Babylonia, the empire quickly dissolved after Hammurabis death and Babylon spent long periods under Assyrian, Kassite and Elamite domination. After being destroyed and then rebuilt by the Assyrians, Babylon became the capital of the Neo-Babylonian Empire from 609 to 539 BC, the Hanging Gardens of Babylon was one of the Seven Wonders of the Ancient World. After the fall of the Neo-Babylonian Empire, the city came under the rule of the Achaemenid, Seleucid, Parthian, Roman, and Sassanid empires. It has been estimated that Babylon was the largest city in the world from c.1770 to 1670 BC and it was perhaps the first city to reach a population above 200,000. Estimates for the extent of its area range from 890 to 900 hectares. The remains of the city are in present-day Hillah, Babil Governorate, Iraq, about 85 kilometres south of Baghdad, comprising a large tell of broken mud-brick buildings, the English Babylon comes from Greek Babylṓn, a transliteration of the Akkadian Babili. The Babylonian name in the early 2nd millennium BC had been Babilli or Babilla, by the 1st millennium BC, it had changed to Babili under the influence of the folk etymology which traced it to bāb-ili. The Gate of God or Gate of El being from the Aramaic Hebrew Bab for Gate and El for God and this being similar to the Hebrew word for confusion Balal. In the Bible, the name appears as Babel, interpreted in the Hebrew Scriptures Book of Genesis to mean confusion, the modern English verb, to babble, or to speak meaningless words, is popularly thought to derive from this name, but there is no direct connection. The remains of the city are in present-day Hillah, Babil Governorate, Iraq, about 85 kilometers south of Baghdad, comprising a large tell of broken mud-brick buildings and debris. The site at Babylon consists of a number of mounds covering an area of about 2 by 1 kilometer, oriented north to south, along the Euphrates to the west. Originally, the river roughly bisected the city, but the course of the river has since shifted so that most of the remains of the western part of the city are now inundated. Some portions of the city wall to the west of the river also remain, remains of the city include, Kasr—also called Palace or Castle, it is the location of the Neo-Babylonian ziggurat Etemenanki and lies in the center of the site. Amran Ibn Ali—the highest of the mounds at 25 meters, to the south and it is the site of Esagila, a temple of Marduk which also contained shrines to Ea and Nabu. Homera—a reddish colored mound on the west side, most of the Hellenistic remains are here
21.
Sargon of Akkad
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Sargon of Akkad was the first ruler of the Semitic-speaking Akkadian Empire, known for his conquests of the Sumerian city-states in the 24th to 23rd centuries BC. He was the founder of the Sargonic or Old Akkadian dynasty, the Sumerian king list makes him the cup-bearer to king Ur-Zababa of Kish. His empire is thought to have included most of Mesopotamia, parts of the Levant, besides incursions into Hurrite and Elamite territory, ruling from his capital, Sargon appears as a legendary figure in Neo-Assyrian literature of the 8th to 7th centuries BC. Tablets with fragments of a Sargon Birth Legend were found in the Library of Ashurbanipal, the Akkadian name is normalized as either Šarru-ukīn or Šarru-kēn. The names cuneiform spelling is variously LUGAL-ú-kin, šar-ru-gen6, šar-ru-ki-in, šar-ru-um-ki-in, in Late Assyrian references, the name is mostly spelled as LUGAL-GI. NA or LUGAL-GIN, i. e. identical to the name of the Neo-Assyrian king Sargon II. The spelling Sargon is derived from the mention of the name in the Hebrew Bible, as סַרְגוֹן. The first element in the name is šarru, the Akkadian for king, the second element derived from the root kūn to confirm, establish. A possible interpretation of the reading Šarru-ukīn is the king has established stability, such a name would however be unusual, other names in -ukīn always include both a subject and an object, as in Šamaš-šuma-ukīn Shamash has established an heir. There is some debate whether the name was an adopted regnal name or a birth name. The reading Šarru-kēn has been interpreted adjectivally, as the king is established, legitimate, the terms Pre-Sargonic and Post-Sargonic were used in Assyriology based on the chronologies of Nabonidus before the historical existence of Sargon of Akkad was confirmed. The form Šarru-ukīn was known from the Assyrian Sargon Legend discovered in 1867 in Ashurbanipals library at Nineveh, the first contemporary reference to Sargon was found on the cylinder seal of Ibni-sharru, a high-ranking official serving under Sargon. Ménant published a description of this seal in 1877, reading the name as Shegani-shar-lukh. In 1883, the British Museum acquired the mace-head of Shar-Gani-sharri and this Shar-Gani was identified with the Sargon of Agade of Assyrian legend. The identification of Shar-Gani-sharri with Sargon was recognised as mistaken in the 1910s, Shar-Gani-sharri is in fact Sargons great-grandson, the successor of Naram-Sin. It is not entirely clear whether the Neo-Assyrian king Sargon II was directly named for Sargon of Akkad, primary sources pertaining to Sargon are very sparse, the main near-contemporary reference is that in the various versions of the Sumerian king list. Here, Sargon is mentioned as the son of a gardener, former cup-bearer of Ur-Zababa of Kish and he usurped the kingship from Lugal-zage-si of Uruk and took it to his own city of Akkad. Various copies of the king list give the duration of his reign as either 54,55 or 56 years, in absolute years, his reign would correspond to ca. 2340–2284 BC in the Middle Chronology and his successors until the Gutian conquest of Sumer are also known as the Sargonic Dynasty and their rule as the Sargonic Period of Mesopotamian history
22.
Agade
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The empire united all the Akkadian and Sumerian speakers under one rule. The Akkadian Empire controlled Mesopotamia, the Levant, and eastern and southern parts of Anatolia and Iran, sending military expeditions as far south as Dilmun and Magan in the Arabian Peninsula. During the 3rd millennium BC, there developed an intimate cultural symbiosis between the Sumerians and the Akkadians, which included widespread bilingualism. Akkadian gradually replaced Sumerian as a spoken language somewhere between the 3rd and the 2nd millennia BC, the Akkadian Empire reached its political peak between the 24th and 22nd centuries BC, following the conquests by its founder Sargon of Akkad. Under Sargon and his successors, the Akkadian language was imposed on neighboring conquered states such as Elam. Akkad is sometimes regarded as the first empire in history, though there are earlier Sumerian claimants, the Bible refers to Akkad in Genesis 10,10, which states that the beginning of Nimrods kingdom was in the land of Akkad. Nimrod is a Hebrew name not attested in Mesopotamians sources, many have pointed out similarities with the legend of Gilgamesh who founded Uruk, which is said to be the city Nimrod came to power. Today, some 7,000 texts from the Akkadian period alone are known, many later texts from the successor states of Assyria and Babylonia also deal with the Akkadian Empire. Understanding of the Akkadian Empire continues to be hampered by the fact that its capital Akkad has not yet been located, likewise, material that is thought to be Akkadian continues to be in use into the Ur III period. Many of the recent insights on the Akkadian Empire have come from excavations in the Upper Khabur area in modern northeastern Syria which was to become a part of Assyria after the fall of Akkad. For example, excavations at Tell Mozan brought to light a sealing of Taram-Agade, an unknown daughter of Naram-Sin. The excavators at nearby Tell Leilan have used the results from their investigations to argue that the Akkadian Empire came to an end due to a sudden drought, the so-called 4.2 kiloyear event. The impact of this event on Mesopotamia in general, and on the Akkadian Empire in particular. The Akkadian Period is contemporary with, EB IV, EB IVA and EJ IV, the absolute dates of their reigns are approximate. The Akkadian Empire takes its name from the region and city of Akkad, although the city of Akkad has not yet been identified on the ground, it is known from various textual sources. Among these is at least one text predating the reign of Sargon, together with the fact that the name Akkad is of non-Akkadian origin, this suggests that the city of Akkad may have already been occupied in pre-Sargonic times. Sargon of Akkad defeated and captured Lugal-Zage-Si in the Battle of Uruk, the earliest records in the Akkadian language date to the time of Sargon. Sargon was claimed to be the son of Laibum or Itti-Bel, a humble gardener, One legend related of Sargon in Assyrian times says that My mother was a changeling, my father I knew not
23.
United States Department of State
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The Department was created in 1789 and was the first executive department established. The Department is headquartered in the Harry S Truman Building located at 2201 C Street, NW, the Department operates the diplomatic missions of the United States abroad and is responsible for implementing the foreign policy of the United States and U. S. diplomacy efforts. The Department is also the depositary for more than 200 multilateral treaties, the Department is led by the Secretary of State, who is nominated by the President and confirmed by the Senate and is a member of the Cabinet. The current Secretary of State is Rex Tillerson, beginning 1 February 2017, the Secretary of State is the first Cabinet official in the order of precedence and in the presidential line of succession, after the President pro tempore of the Senate. This legislation remains the law of the Department of State. In September 1789, additional legislation changed the name of the agency to the Department of State and these responsibilities grew to include management of the United States Mint, keeper of the Great Seal of the United States, and the taking of the census. President George Washington signed the new legislation on September 15, most of these domestic duties of the Department of State were eventually turned over to various new Federal departments and agencies that were established during the 19th century. On September 29,1789, President Washington appointed Thomas Jefferson of Virginia, then Minister to France, from 1790 to 1800, the State Department had its headquarters in Philadelphia, the capital of the United States at the time. It occupied a building at Church and Fifth Streets, in 1800, it moved from Philadelphia to Washington, D. C. where it first occupied the Treasury Building and then the Seven Buildings at 19th Street and Pennsylvania Avenue. It moved into the Six Buildings in September 1800, where it remained until May 1801 and it moved into the War Office Building due west of the White House in May 1801. It occupied the Treasury Building from September 1819 to November 1866 and it then occupied the Washington City Orphan Home from November 1866 to July 1875. It moved to the State, War, and Navy Building in 1875, since May 1947, it has occupied the Harry S. Truman Building in the Foggy Bottom neighborhood of Washington, the State Department is therefore sometimes metonymically referred to as Foggy Bottom. Madeleine Albright became the first woman to become the United States Secretary of State, condoleezza Rice became the second female secretary of state in 2005. Hillary Rodham Clinton became the female secretary of state when she was appointed in 2009. In 2014, the State Department began expanding into the Navy Hill Complex across 23rd Street NW from the Truman Building, the Executive Branch and the U. S. Congress have constitutional responsibilities for U. S. foreign policy. Within the Executive Branch, the Department of State is the lead U. S, the Department advances U. S. objectives and interests in the world through its primary role in developing and implementing the Presidents foreign policy. It also provides an array of important services to U. S. citizens, the total Department of State budget, together with Other International Programs, costs about 45 cents a day for each resident of the United States. Keeping the public informed about U. S. foreign policy and relations with other countries, providing automobile registration for non-diplomatic staff vehicles and the vehicles of diplomats of foreign countries having diplomatic immunity in the United States
24.
Samarra
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Sāmarrā is a city in Iraq. It stands on the east bank of the Tigris in the Saladin Governorate,125 kilometers north of Baghdad, in 2003 the city had an estimated population of 348,700. Samarra was once in the Sunni Triangle of violence during the violence in Iraq. In the medieval times, Samarra was the capital of the Abbasid Caliphate, in 2007, UNESCO named Samarra one of its World Heritage Sites. The remains of prehistoric Samarra were first excavated between 1911 and 1914 by the German archaeologist Ernst Herzfeld, Samarra became the type site for the Samarra culture. Since 1946, the notebooks, letters, unpublished excavation reports and photographs have been in the Freer Gallery of Art in Washington, the civilization flourished alongside the Ubaid period, as one of the first town states in the Near East. It lasted from 5,500 BCE and eventually collapsed in 3,900 BCE, a city of Sur-marrati is insecurely identified with a fortified Assyrian site of Assyrian at al-Huwaysh on the Tigris opposite modern Samarra. The State Archives of Assyria Online identifies Surimarrat as the site of Samarra. In 836 the Abbasid Caliph Al-Mutasim founded a new capital at the banks of the Tigris, here he built extensive palace complexes surrounded by garrison settlements for his guards, mostly drawn from Central Asia and Iran or North Africa. Although quite often called Mamluk slave soldiers, their status was quite elevated, for his son al-Mutazz he built the large palace Bulkuwara. Samarra remained the residence of the caliph until 892, when al-Mutadid eventually returned to Baghdad, the city declined but maintained a mint until the early 10th century. After the collapse of the Abbasid empire in about 940 Samarra was abandoned and its population returned to Baghdad and the city rapidly declined. Its field of ruins is the only metropolis of late antiquity which is available for serious archaeology. This has made it an important pilgrimage centre for the Twelvers, in addition, Hakimah and Narjis, female relatives of the Muhammad and the Imams, held in high esteem by Muslims, are buried there, making this mosque one of the most significant sites of worship. In the eighteenth century, one of the most bloody battles of the 1730–1735 Ottoman–Persian War, the Battle of Samarra, took place, the engagement decided the fate of Ottoman Iraq and kept it under Istanbuls suzerainty until the First World War. Many local people were displaced by the dam, resulting in an increase in Samarras population, Samarra is a key city in Saladin Governorate, a major part of the so-called Sunni Triangle where insurgents were active during the Iraq War. Though Samarra is famous for its Shii holy sites, including the tombs of several Shii Imams, tensions arose between Sunnis and the Shia during the Iraq War. On February 22,2006, the dome of the al-Askari Mosque was bombed, setting off a period of rioting
25.
Al-Jazira, Mesopotamia
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Upper Mesopotamia is the name used for the uplands and great outwash plain of northwestern Iraq, northeastern Syria and southeastern Turkey, in the northern Middle East. This region is approximately correspondent with what was Assyria from the 25th century BC through to the mid-7th century AD and it extends down the Tigris to Samarra and down the Euphrates to Hit. The Khabur River runs for over 400 km across the plain, from Turkey in the north, the major settlements are Mosul, Deir ez-Zor, Raqqa, Al Hasakah, Diyarbakır and Qamishli. The western, Syrian part, is contiguous with the Syrian Al-Hasakah Governorate and is described as Syrias breadbasket. The eastern, Iraqi part, includes and extends slightly beyond the Iraqi Ninewa Governorate, in the north it includes the Turkish provinces of Şanlıurfa, Mardin, and parts of Diyarbakır Province. The name al-Jazira has been used since the 7th century CE by Islamic sources to refer to the section of Mesopotamia. The name means island, and at one time referred to the land between the two rivers, which in Aramaic is Bit Nahren. Historically the name referred to as little as the Sinjar plain coming down from the Sinjar Mountains, in pre-Abbasid times the western and eastern boundaries seem to have fluctuated, sometimes including what is now northern Syria to the west and Adiabene in the east. Al-Jazira is characterised as an outwash or alluvial plain, quite distinct from the Syrian Desert and lower-lying central Mesopotamia, however the area includes eroded hills, the region has several parts to it. In the northwest is one of the largest salt flats in the world, further south, extending from Mosul to near Basra is a sandy desert not unlike the Empty Quarter. In the late 20th and early 21st centuries the region has been plagued by drought and this is the area where the earliest signs of agriculture and domestication of animals have been found, and thus the starting point leading to civilization and the modern world. Al-Jazirah includes the mountain Karaca Dağ in southern Turkey, where the closest relative to modern wheat still grows wild, domestication of goats and sheep followed within a few generations, but didnt become widespread for more than a millennium. Weaving and pottery followed about two years later. Further surprises followed in the 1990s with the finds of the megalithic structures at Göbekli Tepe in south-eastern Turkey. The earliest of these apparently ritual buildings are from before 9000 BC—over five thousand years older than Stonehenge—and thus the absolute oldest known megalithic structures anywhere, as far as we know today no well-established farming societies existed at the time. Farming seemed to be experimental and only a smallish supplement to continued hunting and gathering. After all, Göbekli Tepe lies just 32 km from Karaca Dağ, the questions raised by Göbekli Tepe have led to intense and creative discussions among archeologists of the Middle East. Excavations at Göbekli Tepe continues, only about 5 percent has been revealed so far, Upper Mesopotamia is the heartland of ancient Assyria, founded circa the 25th century BC
26.
Irrigation
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Irrigation is the method in which a controlled amount of water is supplied to plants at regular intervals for agriculture. It is used to assist in the growing of crops, maintenance of landscapes. Additionally, irrigation also has a few uses in crop production. In contrast, agriculture that only on direct rainfall is referred to as rain-fed or dry land farming. Irrigation systems are used for dust suppression, disposal of sewage. Irrigation is often studied together with drainage, which is the natural or artificial removal of surface and sub-surface water from a given area, Irrigation has been a central feature of agriculture for over 5,000 years and is the product of many cultures. Historically, it was the basis for economies and societies across the globe, archaeological investigation has found evidence of irrigation where the natural rainfall was insufficient to support crops for rainfed agriculture. Ancient Egyptians practiced Basin irrigation using the flooding of the Nile to inundate land plots which had surrounded by dykes. The flood water was held until the sediment had settled before the surplus was returned to the watercourse. The Ancient Nubians developed a form of irrigation by using a device called a sakia. Irrigation began in Nubia some time between the third and second millennium BCE and it largely depended upon the flood waters that would flow through the Nile River and other rivers in what is now the Sudan. In sub-Saharan Africa irrigation reached the Niger River region cultures and civilizations by the first or second millennium BCE and was based on wet season flooding, terrace irrigation is evidenced in pre-Columbian America, early Syria, India, and China. These canals are the earliest record of irrigation in the New World, traces of a canal possibly dating from the 5th millennium BCE were found under the 4th millennium canal. Large scale agriculture was practiced and a network of canals was used for the purpose of irrigation. Ancient Persia as far back as the 6th millennium BCE, where barley was grown in areas where the rainfall was insufficient to support such a crop. The Qanats, developed in ancient Persia in about 800 BCE, are among the oldest known irrigation methods still in use today and they are now found in Asia, the Middle East and North Africa. The system comprises a network of wells and gently sloping tunnels driven into the sides of cliffs. The noria, a wheel with clay pots around the rim powered by the flow of the stream, was first brought into use at about this time
27.
Nineveh Plain
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Nineveh Plains is a region in Iraqs Nineveh Governorate to the north and east of the city Mosul, from which it is also known as the Plain of Mosul. It was formerly known as the Plain of Sanjar or Sinjar from its major medieval settlement and it was the location of al-Khwārizmīs determination of a degree during the reign of the caliph al-Mamun. Nineveh Plains lie to the east, northeast of the city of Mosul in the Iraqi Ninawa Province, the ancient city of Nineveh stood where the eastern outskirts of Mosul are today, on the bank of the Tigris river. The villages on the part of the plains are inhabited by minority religious groups that are non-Muslim. Most of these inhabitants are Assyrian Christians, peutingers map of the inhabited world known to the Roman geographers depicts Singara as located west of the Trogoditi. Persi. who inhabited the territory around Mount Sinjar, by the medieval Arabs, most of the plain was reckoned as part of the province of Diyār Rabīʿa, the abode of the Rabīʿa tribe. The plain was the site of the determination of the degree by al-Khwārizmī, Sinjar also boasted a famous Assyrian cathedral in the 8th century. Schools especially received much attention in this area and in Kurdish areas where Assyrian concentrated population lives, in addition, agriculture and medical clinics received financial help from the Assyrian diaspora. As attacks on Christians increased in Basra, Baghdad, Ramadi, more families turned northward to the extended family holdings in the Nineveh Plain. This place of refuge remains underfunded and gravely lacking in infrastructure to aid the ever-increasing internally displaced people population, in February 2010, the attacks against Assyrians in Mosul forced 4,300 Assyrians to flee to the Nineveh plains where there is an Assyrian-majority population. From 2012, it began receiving influxes of Assyrians from Syria owing to the civil war there. In August 2014 nearly all of the inhabitants of the southern regions of the Plains were driven out by the Islamic State of Iraq. There have been calls by some politicians inside and outside Iraq to create a region for Assyrian Christians in this area. The same article has used to proclaim an autonomous province for the Yezidi people. On January 21,2014, the Iraqi government had declared that Nineveh Plains would become a new province, the Nineveh Plains is the only region in Iraq where a plurality of inhabitants follow Syriac Christianity. Before ISIS invaded Nineveh, Assyrians made up around 40% of the population within the plains, other inhabitants are the Yazidis, Shabaks, Turkmens and Kurds. It is believed that this added incentive for absorption by the KRG of the region may lead to conflict with Sunni Arab tribes in the Mosul region itself. Assyrians claim that without Nineveh Plain autonomous administration, the indigenous Assyrian presence in its ancient homeland could well disappear, there are some oil reserves in Nineveh Plains
28.
Duhok
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The city is encircled by mountains along the Tigris river. Dohuk has a growing tourist industry and its population has increased rapidly since the 1990s, as the rural population moved to the cities. The University of Dohuk, founded in 1992, is a center for teaching. Another theory is that the name comes from Taok due to the fact that the region is well known for vine trees. The Syriac name Bēṯ Nūhadrā translates to House/Land of the military leader and it refers to a small village nearby which is a district in the city due to the growth of the city during the last century. The name Nūhadrā continues to be used in reference to the city and is also a name among Assyrian women. Throughout history to the present time, Duhok has acquired a position historically and geographically. During the Christian era became an eparchy within the Assyrian Church of the East metropolitanate of Ḥadyab, the city became prominent again in 1236, when Hasan Beg Saifadin joined the Kurdish Badinan principality. In 1842, the principality was dissolved by the Ottomans and connected to the city of Mosul, in 1898 there were according to a report eleven small and private schools in the city, two Assyrian Christian and two Jewish schools. In 1920 there were in all of Iraq only five schools that were accessible for girls. From 22 to 24 September 2005 Dohuk held a festival that was for the first time in Dohuk to which Kurdish writers from all countries were invited. The citys population is made up of around 340,000 inhabitants, the Assyrians of Dohuk boast one of the largest churches in the region named the Mar Marsi Cathedral, and is the center of an Eparchy. Another football team from the city is Zeravani SC which plays in the Kurdish Premier League, Dohuk also has a range of other sport clubs, notably the Duhok Basketball Club. Duhok SC basketball competes in the Iraqi Division I Basketball League, Duhok SC football club won the Iraqi premier league championship In the 2009/2010 season beating Talaba SC 1–0 to become the champions for the first time. Köppen-Geiger climate classification system classifies this climate as a semi-arid climate, the temperatures are typical to the northern parts of Mesopotamia region, with extremely hot summers and relatively cool, wet winters. Precipitation falls in the cooler months
29.
Zakho
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Zakho is a city, at the centre of the eponymous Zakho District of the Dohuk Governorate of Iraq, located a few kilometers from the Iraqi-Turkish border. The city has a population of 350,000 and it may have originally begun on a small island surrounded on all sides by the Little Khabur river, which flows through the modern city. The Khabur flows west from Zakho to form the border between Iraq and Turkey, continuing into the Tigris, the most important rivers in the area are the Zeriza, Seerkotik and the aforementioned Little Khabur. In July 2010, Zakho became the seat of the University of Zakho, there are several theories concerning the derivation of the name Zakho. Some Aramaic sources maintain that the name comes from the Aramaic zāḵū, another version maintains that the name comes from the Kurdish words zey- khowin, possibly referring to the same battle. A third opinion attributes the name to the Kurdish for river bend, from zey, the town of Zakho was known to the ancient Greeks. In 1844, the traveller William Francis Ainsworth commented, The appearance of Zakho in the present day coincides in a manner with what it was described to be in the time of Xenophon. Gertrude Bell was convinced that Zakho was same place as the ancient town of Hasaniyeh and she also reported that the first Christian missionary to the region, the Dominican monk Poldo Soldini, was buried there in 1779. His grave was still a destination in the 1950s. Zakho was formerly known for its synagogues and large, ancient Jewish community and was known as The Jerusalem of Assyria, the Jews spoke the Aramaic of their ancestors. The banks of the nearby Khabur River are mentioned in the Bible as one of the places to which the Israelites were exiled, there were serious attacks on the Jews in 1891, when one of the synagogues was burnt down. The troubles intensified in 1892, with heavy taxes being imposed, outbreaks of looting, Jews from Zakho were among the first to emigrate to Palestine after 1920. Most of the relocated to Israel in the 1950s. Assyrians have lived in Zakho since at least the 5th century, with some Assyrian bishops being mentioned from the fifth to the seventh century, which indicates its long history. Additionally, The city was the center of a large Chaldean Catholic diocese up until the middle of the nineteenth century, however, the diocese was recently merged back into the Chaldean Catholic Eparchy of Amadiya in 2013 due to becoming vacant after the death of its Bishop in 2010. Prior to merging with Amadiya, The diocese comprised 3500 Assyrian Catholics, ten resident priests, fifteen parishes or stations, twenty churches and chapels, in regards to the city of Zakho itself, there is a large Assyrian population. The Armenians of Zakho established their community after the Armenian Genocide from 1915-1923, some of the Armenians of Zakho left in 1932 to found the village of Avzrog Miri in the plains west of the city of Simele. Zakho has served as a checkpoint for many decades and it is a major marketplace with its goods and merchandise serving the Kurdish controlled area and most of north and middle Iraq
30.
Mesopotamian Marshes
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The Mesopotamian Marshes or Iraqi Marshes are a wetland area located in southern Iraq and partially in southwestern Iran and Kuwait. Historically the marshlands, mainly composed of the separate but adjacent Central, Hawizeh and Hammar Marshes and it is a rare aquatic landscape in the desert, providing habitat for the Marsh Arabs and important populations of wildlife. Draining of portions of the began in the 1950s and continued through the 1970s to reclaim land for agriculture. However, in the late 1980s and 1990s, during the presidency of Saddam Hussein, before 2003, the marshes were drained to 10% of their original size. After the fall of Husseins regime in 2003, the marshes have partially recovered but drought along with upstream dam construction and operation in Turkey, Syria, since 2016 the mesopotamian marshes are listed as an Unesco Heritage Site. The crucial trigger was the availability of wild plant species. Farming arose early in the Fertile Crescent because the area had a quantity of wild wheat and pulse species that were nutritious. In the 10th and 11th centuries, the marshes were the site of the state of Batihah founded by Imran ibn Shahin, the Marsh Arabs are the primary inhabitants of the Mesopotamian Marshes and are the descendants of ancient Sumerians, as their civilization dates back 5000 years. They live in secluded villages of elaborate reed houses throughout the marshes, fish, rice cultivation, water buffalo and other resources are also used in their daily lives. In the 1950s, there were an estimated 500,000 Marsh Arabs and this population shrank to about 20,000 following the draining and Saddams violent reprisals, and between 80,000 and 120,000 fled to neighboring Iran. Following the 2003 Iraq invasion, Marsh Arabs have begun to return to the marshes, as their name suggests, the Mesopotamian Marshes are located in the larger region which used to be called Mesopotamia. Mesopotamia, meaning in between rivers, is now occupied by modern Iraq, eastern Syria, south-eastern Turkey, the marshes lie mostly within southern Iraq and a portion of southwestern Iran. Before the 2003 Invasion of Iraq, about 90% of the marshes had been drained, the marshes lie on a flat alluvial plain, as the Euphrates decreases only 12 m in elevation during its last 300 km while the Tigris falls 24 m. This delta provides an environment that allows the Tigris and Euphrates to meander, the Euphrates has often terminated near Nasiriyah into the Hammar Marshes as its flow slows. The Tigris can distribute some of its flow into the Central, downstream of Amarah though, several of its tributaries originating in Iran allow the Tigris flow to increase and maintain a steady course thereafter. The three marshes combined once provided an environment, particularly during periods of flooding as the rivers overflowed. The Central Marshes receive water from influxes of the Tigriss distributaries, namely the Shatt al-Muminah, the Tigris serves as the marshes eastern boundary while the Euphrates serves as its southern boundary. Covering an area of 3,000 km2, the marshes consist of reed beds, the Al-Zikri and Hawr Umm Al-Binni lakes are two of the notable lakes and are 3 m deep
31.
Shatt al-Arab
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The southern end of the river constitutes the border between Iraq and Iran down to the mouth of the river as it discharges into the Persian Gulf. The river is significant because it forms a natural border between Iran and the Arab world. It varies in width from about 232 metres at Basra to 800 metres at its mouth and it is thought that the waterway formed relatively recently in geologic time, with the Tigris and Euphrates originally emptying into the Persian Gulf via a channel further to the west. The Karun river, a tributary joins the waterway from the Iranian side, deposits large amounts of silt into the river. The area is judged to hold the largest date palm forest in the world, in the mid-1970s, the region included 17 to 18 million date palms, an estimated one-fifth of the worlds 90 million palm trees. But by 2002, war, salt, and pests had wiped out more than 14 million of the palms, many of the remaining 3 to 4 million trees are in poor condition. In Middle Persian literature and the Shahnama, the name اروند Arvand is used for the Tigris, Iranians also used this name specifically to designate the Shatt al-Arab during the later Pahlavi period, and continue to do so after the Iranian Revolution of 1979. The Iranian cities of Abadan and Khorramshahr and the Iraqi city, the tribes on both sides of the lower waterway, however, are Marsh Arabs, and the Ottoman Empire claimed to represent them. Tensions between the empires that extended across a wide range of religious, cultural and political conflicts. The Second Treaty of Erzurum was signed by the two parties in 1847 after protracted negotiations, which included British and Russian delegates. A protocol between the Ottomans and the Persians was signed in Istanbul in 1913, which declared that the Ottoman-Persian frontier run along the thalweg, in 1937, Iran and Iraq signed a treaty that settled the dispute over control of the Shatt al-Arab. By the late 1960s, the build-up of Iranian power under Shah Mohammad Reza Pahlavi, in April 1969, Iran abrogated the 1937 treaty over the Shatt al-Arab, and as such, Iran ceased paying tolls to Iraq when its ships used the Shatt al-Arab. Iraq threatened war over the Iranian move, but when on 24 April 1969 an Iranian tanker escorted by Iranian warships sailed down the Shatt al-Arab, Iraq being the militarily weaker state did nothing. The Iranian abrogation of the 1937 treaty marked the beginning of a period of acute Iraqi-Iranian tension that was to last until the Algiers Accords of 1975, all United Nations attempts to intervene as mediators were rebuffed. Under Saddam Hussein, Baathist Iraq claimed the entire waterway up to the Iranian shore as its territory, in response, Iran in the early 1970s became the main patron of Iraqi Kurdish groups fighting for independence from Iraq. In 1980, Hussein released a statement claiming to abrogate the treaty that he signed, international law, however, holds that in all cases no bilateral or multilateral treaty can be abrogated by one party only. The main thrust of the movement on the ground was across the waterway which was the stage for most of the military battles between the two armies. The waterway was Iraqs only outlet to the Persian Gulf, and thus, its shipping lanes were greatly affected by continuous Iranian attacks
32.
Alluvial plain
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An alluvial plain is a largely flat landform created by the deposition of sediment over a long period of time by one or more rivers coming from highland regions, from which alluvial soil forms. As the highlands due to weathering and water flow, the sediment from the hills is transported to the lower plain. Various creeks will carry the water further to a river, lake, bay, as the sediments are deposited during flood conditions in the floodplain of a creek, the elevation of the floodplain will be raised. As this reduces the channel capacity, the creek will, over time, seek new, lower paths. These processes, over time, will form the plain. The NCSS glossary instead suggests flood plain
33.
Baghdad
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Baghdad is the capital of the Republic of Iraq. The population of Baghdad, as of 2016, is approximately 8,765,000 making it the largest city in Iraq, the second largest city in the Arab world, and the second largest city in Western Asia. Located along the Tigris River, the city was founded in the 8th century, within a short time of its inception, Baghdad evolved into a significant cultural, commercial, and intellectual center for the Islamic world. This, in addition to housing several key institutions, garnered the city a worldwide reputation as the Centre of Learning. Throughout the High Middle Ages, Baghdad was considered to be the largest city in the world with a population of 1,200,000 -3,000,000 people. The city was destroyed at the hands of the Mongol Empire in 1258, resulting in a decline that would linger through many centuries due to frequent plagues. With the recognition of Iraq as an independent state in 1938, in contemporary times, the city has often faced severe infrastructural damage, most recently due to the 2003 invasion of Iraq, and the subsequent Iraq War that lasted until December 2011. In recent years, the city has been subjected to insurgency attacks. As of 2012, Baghdad was listed as one of the least hospitable places in the world to live, the site where the city of Baghdad developed has been populated for millennia. By the 8th century AD, several villages had developed there, including a Persian hamlet called Baghdad, the name is of Indo-European origin and a Middle Persian compound of Bagh god and dād given by, translating to Bestowed by God or Gods gift. In Old Persian the first element can be traced to boghu and is related to Slavic bog god, a similar term in Middle Persian is the name Mithradāt, known in English by its Hellenistic form Mithridates, meaning gift of Mithra. There are a number of locations in the wider region whose names are compounds of the word bagh, including Baghlan. The name of the town Baghdati in Georgia shares the same etymological origins, when the Abbasid caliph, al-Mansur, founded a completely new city for his capital, he chose the name Madinat al-Salaam or City of Peace. This was the name on coins, weights, and other official usage. By the 11th century, Baghdad became almost the exclusive name for the world-renowned metropolis, after the fall of the Umayyads, the first Muslim dynasty, the victorious Abbasid rulers wanted their own capital whence they could rule. They chose a site north of the Sassanid capital of Ctesiphon, on 30 July 762, the caliph Al-Mansur commissioned the construction of the city, mansur believed that Baghdad was the perfect city to be the capital of the Islamic empire under the Abbasids. Mansur loved the site so much he is quoted saying, This is indeed the city that I am to found, where I am to live, and where my descendants will reign afterward. The citys growth was helped by its excellent location, based on at least two factors, it had control over strategic and trading routes along the Tigris, the abundance of water in a dry climate
34.
River delta
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A river delta is a landform that forms from deposition of sediment carried by a river as the flow leaves its mouth and enters slower-moving or standing water. This occurs where a river enters an ocean, sea, estuary, lake, reservoir, River deltas are ecologically important as they provide coastline defense, are home to many species, and can impact drinking water supply. The tidal currents also cannot be too strong, as sediment would wash out into the body faster than the river deposits it. Of course, the river must carry enough sediment to layer into deltas over time, the rivers velocity decreases rapidly, causing it to deposit the majority, if not all, of its load. This alluvium builds up to form the river delta, when the flow enters the standing water, it is no longer confined to its channel and expands in width. This flow expansion results in a decrease in the flow velocity, as a result, sediment drops out of the flow and deposits. Over time, this single channel builds a deltaic lobe, pushing its mouth into the standing water, as the deltaic lobe advances, the gradient of the river channel becomes lower because the river channel is longer but has the same change in elevation. As the slope of the channel decreases, it becomes unstable for two reasons. First, gravity makes the flow in the most direct course down slope. If the river breaches its natural levees, it out onto a new course with a shorter route to the ocean. Second, as its slope gets lower, the amount of stress on the bed decreases, which results in deposition of sediment within the channel. This makes it easier for the river to breach its levees, often when the channel does this, some of its flow remains in the abandoned channel. When these channel-switching events occur, a mature delta develops a distributary network, another way these distributary networks form is from deposition of mouth bars. When this mid-channel bar is deposited at the mouth of a river and this results in additional deposition on the upstream end of the mouth-bar, which splits the river into two distributary channels. A good example of the result of this process is the Wax Lake Delta, in both of these cases, depositional processes force redistribution of deposition from areas of high deposition to areas of low deposition. This results in the smoothing of the shape of the delta as the channels move across its surface. Because the sediment is laid down in fashion, the shape of these deltas approximates a fan. The more often the flow changes course, the shape develops as closer to an ideal fan, the Mississippi and Ural River deltas, with their birds-feet, are examples of rivers that do not avulse often enough to form a symmetrical fan shape
35.
Lake
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A lake is an area of variable size filled with water, localized in a basin, that is surrounded by land, apart from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, and therefore are distinct from lagoons, Lakes can be contrasted with rivers or streams, which are usually flowing. Most lakes are fed and drained by rivers and streams, natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, in some parts of the world there are many lakes because of chaotic drainage patterns left over from the last Ice Age. All lakes are temporary over geologic time scales, as they will fill in with sediments or spill out of the basin containing them. The word lake comes from Middle English lake, from Old English lacu, from Proto-Germanic *lakō, cognates include Dutch laak, Middle Low German lāke as in, de, Moorlake, de, Wolfslake, de, Butterlake, German Lache, and Icelandic lækur. Also related are the English words leak and leach, none of these definitions completely excludes ponds and all are difficult to measure. For this reason, simple size-based definitions are used to separate ponds. One definition of lake is a body of water of 2 hectares or more in area, however, others have defined lakes as waterbodies of 5 hectares and above, or 8 hectares and above. Charles Elton, one of the founders of ecology, regarded lakes as waterbodies of 40 hectares or more. The term lake is used to describe a feature such as Lake Eyre. In common usage, many bear names ending with the word pond. One textbook illustrates this point with the following, In Newfoundland, for example, almost every lake is called a pond, whereas in Wisconsin, the majority of lakes on Earth are fresh water, and most lie in the Northern Hemisphere at higher latitudes. Canada, with a drainage system has an estimated 31,752 lakes larger than 3 square kilometres and an unknown total number of lakes. Finland has 187,888 lakes 500 square metres or larger, most lakes have at least one natural outflow in the form of a river or stream, which maintain a lakes average level by allowing the drainage of excess water. Some lakes do not have an outflow and lose water solely by evaporation or underground seepage or both. Many lakes are artificial and are constructed for power generation, aesthetic purposes, recreational purposes, industrial use. Globally, lakes are greatly outnumbered by ponds, of an estimated 304 million standing water bodies worldwide, 91% are 1 hectare or less in area
36.
Al Qurnah
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Al-Qurnah is a small town in southern Iraq about 74 km northwest of Basra, within the town of Nahairat. Qurna is located at the point of the Tigris and Euphrates rivers join to form the Shatt al-Arab. Local folklore holds Qurna to have been the site of the Garden of Eden, an ancient jujube tree is locally celebrated and shown to the tourists as the actual Tree of Knowledge of the Bible. The town experienced the Battle of Qurna during the Mesopotamian Campaign of World War I, the small Qurna Tourist Hotel was built during the Baathist period to encourage tourism for the region. However it is most likely not in use now, as of the start of the 2003 Iraq War, conditions at the site were reportedly woeful. Cracked pavement and bullet holes along with the condition of the tree itself made future tourism seem out of the question. However, the natural beauty and Western presence make it viable for development for tourism
37.
Silt
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Silt is granular material of a size between sand and clay, whose mineral origin is quartz and feldspar. Silt may occur as a soil or as sediment mixed in suspension with water in a body of such as a river. It may also exist as soil deposited at the bottom of a water body, Silt has a moderate specific area with a typically non-sticky, plastic feel. Silt usually has a floury feel when dry, and a slippery feel when wet, Silt can be visually observed with a hand lens. Silt is created by a variety of physical processes capable of splitting the generally sand-sized quartz crystals of primary rocks by exploiting deficiencies in their lattice and these involve chemical weathering of rock and regolith, and a number of physical weathering processes such as frost shattering and haloclasty. The main process is abrasion through transport, including fluvial comminution, aeolian attrition and it is in semi-arid environments that substantial quantities of silt are produced. Silt is sometimes known as rock flour or stone dust, especially produced by glacial action. Mineralogically, silt is composed mainly of quartz and feldspar, sedimentary rock composed mainly of silt is known as siltstone. Liquefaction created by an earthquake is silt suspended in water that is hydrodynamically forced up from below ground level. In the Udden–Wentworth scale, silt particles range between 0.0039 and 0.0625 mm, larger than clay but smaller than sand particles, ISO14688 grades silts between 0.002 mm and 0.063 mm. In actuality, silt is chemically distinct from clay, and unlike clay, grains of silt are approximately the size in all dimensions, furthermore. Clays are formed from thin plate-shaped particles held together by electrostatic forces, according to the U. S. Department of Agriculture Soil Texture Classification system, the sand-silt distinction is made at the 0.05 mm particle size. The USDA system has been adopted by the Food and Agriculture Organization, in the Unified Soil Classification System and the AASHTO Soil Classification system, the sand-silt distinction is made at the 0.075 mm particle size. Silts and clays are distinguished mechanically by their plasticity, Silt is easily transported in water or other liquid and is fine enough to be carried long distances by air in the form of dust. Thick deposits of silty material resulting from deposition by aeolian processes are called loess. Silt and clay contribute to turbidity in water, Silt is transported by streams or by water currents in the ocean. When silt appears as a pollutant in water the phenomenon is known as siltation, Silt, deposited by annual floods along the Nile River, created the rich, fertile soil that sustained the Ancient Egyptian civilization. In south east Bangladesh, in the Noakhali district, cross dams were built in the 1960s whereby silt gradually started forming new land called chars, the district of Noakhali has gained more than 28 square miles of land in the past 50 years
38.
Salt
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Salt is present in vast quantities in seawater, where it is the main mineral constituent. The open ocean has about 35 grams of solids per litre, Salt is essential for life in general, and saltiness is one of the basic human tastes. The tissues of animals contain larger quantities of salt than do plant tissues, Salt is one of the oldest and most ubiquitous food seasonings, and salting is an important method of food preservation. Salt was also prized by the ancient Hebrews, the Greeks, the Romans, the Byzantines, the Hittites, Egyptians, and the Indians. Salt became an important article of trade and was transported by boat across the Mediterranean Sea, along specially built salt roads, the scarcity and universal need for salt has led nations to go to war over it and use it to raise tax revenues. Salt is used in ceremonies and has other cultural significance. Salt is processed from salt mines, or by the evaporation of seawater or mineral-rich spring water in shallow pools. Its major industrial products are caustic soda and chlorine, and is used in industrial processes including the manufacture of polyvinyl chloride, plastics, paper pulp. Of the annual production of around two hundred million tonnes of salt, only about 6% is used for human consumption. Other uses include water conditioning processes, de-icing highways, and agricultural use, edible salt is sold in forms such as sea salt and table salt which usually contains an anti-caking agent and may be iodised to prevent iodine deficiency. As well as its use in cooking and at the table, sodium is an essential nutrient for human health via its role as an electrolyte and osmotic solute. Excessive salt consumption can increase the risk of diseases, such as hypertension, in children. Such health effects of salt have long been studied, accordingly, numerous world health associations and experts in developed countries recommend reducing consumption of popular salty foods. The World Health Organization recommends that adults should consume less than 2,000 mg of sodium, humans have always tended to build communities either around sources of salt, or where they can trade for it. All through history the availability of salt has been pivotal to civilization, the word salary comes from the Latin word for salt because the Roman Legions were sometimes paid in salt. The Natron Valley was a key region that supported the Egyptian Empire to its north, because it supplied it with a kind of salt that came to be called by its name, natron. Even before this, what is now thought to have been the first city in Europe is Solnitsata, in Bulgaria, even the name Solnisata means salt works. A very ancient salt-works operation has been discovered at the Poiana Slatinei archaeological site next to a spring in Lunca, Neamț County
39.
Water table
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The water table is the upper surface of the zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with water, the water table is the surface where the water pressure head is equal to the atmospheric pressure. It may be visualized as the surface of the materials that are saturated with groundwater in a given vicinity. The groundwater may be from precipitation or from groundwater flowing into the aquifer, in areas with sufficient precipitation, water infiltrates through pore spaces in the soil, passing through the unsaturated zone. At increasing depths water fills in more of the spaces in the soils. Below the water table, in the zone, layers of permeable rock that yield groundwater are called aquifers. In less permeable soils, such as tight bedrock formations and historic lakebed deposits, the water table should not be confused with the water level in a deeper well. The elevation of the water in this well is dependent upon the pressure in the deeper aquifer and is referred to as the potentiometric surface. The water table may vary due to changes such as precipitation and evapotranspiration. Springs, rivers, lakes and oases occur when the table reaches the surface. Springs commonly form on hillsides, where the Earths slanting surface may intersect with the water table, Groundwater entering rivers and lakes accounts for the base-flow water levels in water bodies. Within an aquifer, the table is rarely horizontal, but reflects the surface relief due to the capillary effect in soils, sediments. In the aquifer, groundwater flows from points of pressure to points of lower pressure. The slope of the table is known as the hydraulic gradient, which depends on the rate at which water is added to and removed from the aquifer. This occurs when there is a layer of rock or sediment or relatively impermeable layer above the main water table/aquifer. If a perched aquifers flow intersects the Earths dry surface, at a wall for example. On low-lying oceanic islands with porous soil, freshwater tends to collect in lenticular pools on top of the denser seawater intruding from the sides of the islands, such an islands freshwater lens, and thus the water table, rises and falls with the tides. In some regions, for example, Great Britain or California, winter precipitation is higher than summer precipitation
40.
Salinity
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Salinity is the saltiness or amount of salt dissolved in a body of water. This is usually measured in g salt k g sea water, a contour line of constant salinity is called an isohaline – or sometimes isohale. Salinity in rivers, lakes, and the ocean is conceptually simple, conceptually the salinity is the quantity of dissolved salt content of the water. Salts are compounds like sodium chloride, magnesium sulfate, potassium nitrate, the concentration of dissolved chloride ions is sometimes referred to as chlorinity. Operationally, dissolved matter is defined as that which can pass through a fine filter. Salinity can be expressed in the form of a mass fraction, Seawater typically has a mass salinity of around 35 g/kg, although lower values are typical near coasts where rivers enter the ocean. Rivers and lakes can have a range of salinities, from less than 0.01 g/kg to a few g/kg. The Dead Sea has a salinity of more than 200 g/kg, whatever pore size is used in the definition, the resulting salinity value of a given sample of natural water will not vary by more than a few percent. A bottled seawater product known as IAPSO Standard Seawater is used by oceanographers to standardize their measurements with enough precision to meet this requirement, measurement and definition difficulties arise because natural waters contain a complex mixture of many different elements from different sources in different molecular forms. The chemical properties of some of these depend on temperature and pressure. Many of these forms are difficult to measure with high accuracy, different practical definitions of salinity result from different attempts to account for these problems, to different levels of precision, while still remaining reasonably easy to use. For many purposes this sum can be limited to a set of eight major ions in natural waters, the major ions dominate the inorganic composition of most natural waters. Exceptions include some pit lakes and waters from some hydrothermal springs, the concentrations of dissolved gases like oxygen and nitrogen are not usually included in descriptions of salinity. However, carbon dioxide gas, which when dissolved is partially converted into carbonates and bicarbonates, is often included. Silicon in the form of acid, which usually appears as a neutral molecule in the pH range of most natural waters. The term salinity is, for oceanographers, usually associated with one of a set of measurement techniques. As the dominant techniques evolve, so do different descriptions of salinity, the distinctions between these different descriptions are important to physical oceanographers but are obscure and confusing to nonspecialists. Salinities were largely measured using titration-based techniques before the 1980s, titration with silver nitrate could be used to determine the concentration of halide ions to give a chlorinity
41.
Bahr al Milh
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Lake Milh, also known as Razzaza Lake, is located a few miles west of Karbala, Iraq. It is alternately called Lake Razazah, Lake Milh is a depression into which excess water from Lake Habbaniyah, which comes from the Euphrates River, is diverted through a controlled escape channel or canal. The lake is listed as a wetland of international importance, the lake is rather shallow and water levels change with the seasons. Due to the salts and the water levels, this largest freshwater lake in Iraq has lost its important stock of fish species. The lake, also termed as Kerbala Gap” has an expanse of 156,234 hectares enclosed by deserts with a few low hills on the shore line. The lake and its surrounding areas lie in a range of 28 to 56 metres. It is a closed lake in a sand/silt basin. The lakes western part of the valley has thick forest cover, in the eastern and southern parts, the terrain is of flat arid/semi-desert type. Mud flats are a feature in the lake. The geological formation in and around the lake consists of marls, siltstones, gypsum/anhydrite, and limestone bands, the lake is at a distance of 95 kilometres to the south-west of Baghdad, and 10 kilometres to the west of Karbala in the Karbala Governorate. The lake was constructed during the half of the 1970s. The lake is fed from the flood flows diverted from the Majora escape of the Habbaniya Lake. The flow from the escape is diverted through the Sin-Al-Thibban Canal and this diversion prevents flooding in the northern areas. The salinity of the lake is increasing as result of supply of water from the link canal. The local people say that the depth in the lake is reduced to about 5–10 metres since 1993 during the regime of Saddam Hussein. The reason for reduction in area is mainly due to inadequate diversion of water from Habbaniya Lake where the priority of use is irrigation. Diversion has been limited to once in 15 days only and this has also affected fishing operations in the lake which in the past used to be throughout the year. As a result, the fish species surviving in the lake is reported to be al-Shanik or Shanak, of marine origin
42.
Buhayrat ath Tharthar
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Lake Tharthar, and known in Iraq as Buhayrat ath-Tharthar, is an artificial lake opened in 1956, situated 100 kilometers northwest of Baghdad between the Tigris and the Euphrates rivers. In 1956, the part of the Tharthar depression was turned into an artificial reservoir to collect flood waters of the Tigris River. The water flows via an inlet canal, named Tharthar Canal. The canal diverts the water, by means of a regulator Samarra Barrage. It merges with the lake in its southeastern bank, the lake has an artificial outlet called Taksim Tharthar Canal, which drains to the Euphrates River directly. The canal, after 28 km from its outlet, bifurcates to another canal called Dhiraa Dijla that returns water back to the Tigris River, Lake Thartar was the site of a raid in 2005 against an insurgent training base in the region. The Tharthar depression formed During Holocene age, mainly by karstification, Tharthar covers roughly 2,050 square kilometres, flows from the central and eastern parts of Sinjar Mountains and adjacent hills, with a floor of –3 m, above the sea level. The maximum length and width of the depression are 120 and 48 km, the eastern rim of the depression is higher than the western one, the heights of both rims are 90 metres and 75 metres, respectively. Moreover, it aims in washing out the salts from the stored water, Tharthar lake and the surrounding areas are considered one of the most important grazing areas in Iraq, including the wide wheat and corn fields covering the area. The area harbors many species of animals and vegetation, Tharthar lake is considered the main wintering grounds for many threatened species of migrant birds such as saker falcon, MacQueens bustard, and sociable lapwing. 54 bird species were seen in Tharthar lake including, pallid harrier, European roller, and black-tailed godwit were recorded on passage, golden jackals have been observed regularly at the site. Striped hyenas and caracals were reported by people near the lake edge. Many species of reptiles have been observed such as Turkish gecko, Tharthar lake and the surrounding area contains about 38 species of plants. Flooded communities, periodically or occasionally flooded land dominated by Cyperus sp, rumex dentatus, Polygonum argyrocoleon, Polygonum sp. and Bacopa monnieri. Marsh vegetation, helophytic vegetation - reedbeds, characterized by Phragmites australis, terrestrial vegetation, desert shrub characterized by Tamarix sp. Alhagi maurorum, Atraplex leucoclada and Cornulaca aucheri, media related to Lake Tharthar at Wikimedia Commons
This article incorporates public domain material from the Library of Congress Country Studies website http://lcweb2.loc.gov/frd/cs/.
This article incorporates 
