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Little Zab
The Little Zab or Lower Zab (, ''al-Zāb al-Asfal''; or '; , ''Zâb-e Kuchak''; , ''Zāba Taḥtāya'') is a river that originates in Iran and joins the Tigris just south of Al Zab in the Kurdistan region of Iraq. It is approximately long and drains an area of about . The river is fed by rainfall and snowmelt, resulting in a peak discharge in spring and low water in summer and early fall. Two dams have been built on the Little Zab, regulating the river flow, providing water for irrigation and generating hydroelectricity. The Zagros Mountains have been occupied since at least the Lower Palaeolithic, but the earliest archaeological site in the Little Zab basin, Barda Balka, dates to the Middle Palaeolithic. Human occupation of the Little Zab basin has been attested for every period since then. Course The Little Zab rises in the Zagros Mountains in Iran at an elevation of circa amsl. In its upper reaches, the course of the Little Zab is determined by the alignment of the major m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Medieval Greek
Medieval Greek (also known as Middle Greek, Byzantine Greek, or Romaic) is the stage of the Greek language between the end of classical antiquity in the 5th–6th centuries and the end of the Middle Ages, conventionally dated to the Ottoman conquest of Constantinople in 1453. From the 7th century onwards, Greek was the only language of administration and government in the Byzantine Empire. This stage of language is thus described as Byzantine Greek. The study of the Medieval Greek language and literature is a branch of Byzantine studies, the study of the history and culture of the Byzantine Empire. The beginning of Medieval Greek is occasionally dated back to as early as the 4th century, either to 330 AD, when the political centre of the Roman Empire was moved to Constantinople, or to 395 AD, the division of the empire. However, this approach is rather arbitrary as it is more an assumption of political, as opposed to cultural and linguistic, developments. Indeed, by this time ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Al Zab
Al Zab, Al-Zab, or Az-Zab is a town in Iraq administered as part of the Kirkuk Governorate's Hawija District. Between 2014-2017, it was under the control of the Islamic State of Iraq and the Levant (ISIL) and was recaptured by Iraqi government forces during the Hawija offensive in September, 2017. Geography Al Zab is located just northeast of the Little Zab's confluence with the Tigris River in northeastern Iraq. History Al Zab is located just north of the former site of Shenna, a major settlement during the Abbasid Caliphate which boasted a Nestorian bishopric. Due to the relatively rapid demographic growth of Iraq's Kurdish population, Saddam Hussein added the majority Arab district of Hawija, including AlZab, to the Kirkuk Governorate in 1968 to render it more easily controlled by his Baath Party.. In December 2005, during the Iraq War, a resistance bomb detonated near AlZab on its road to Hawija, killing an American soldier.. Another bomb on the same road disabled an arm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diyala River
The Diyala River (Arabic: ; ku, Sîrwan; Farsi: , ) is a river and tributary of the Tigris. It is formed by the confluence of Sirwan river and Tanjaro river in Darbandikhan Dam in the Sulaymaniyah Governorate of Northern Iraq. It covers a total distance of . Course It rises near Hamadan, in the Zagros Mountains of Iran. It then descends through the mountains, where for some 32 km it forms the border between the two countries. It finally feeds into the Tigris below Baghdad. Navigation of the upper reaches of the Diyala is not possible because of its narrow defiles, but the river's valley provides an important trade route between Iran and Iraq. The river flows southwest of the Hamrin Mountains. Name Its Aramaic origin is "Diyalas" and in Kurdish it is called "Sirwan", meaning 'roaring sea' or 'shouting river'. In early Islamic period, the lower course of the river formed part of the Nahrawan Canal. The Diyala Governorate in Iraq is named after the river. History The river ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Zab
The Great Zab or Upper Zab ( (''al-Zāb al-Kabīr''), or , , ''(zāba ʻalya)'') is an approximately long river flowing through Turkey and Iraq. It rises in Turkey near Lake Van and joins the Tigris in Iraq south of Mosul. The drainage basin of the Great Zab covers approximately , and during its course, the rivers collects the water from many tributaries. The river and its tributaries are primarily fed by rainfall and snowmelt – as a result of which discharge fluctuates highly throughout the year. At least six dams have been planned on the Great Zab and its tributaries, but construction of only one, the Bekhme Dam, has commenced but was halted after the Gulf War. The Zagros Mountains have been occupied since at least the Lower Palaeolithic, and Neanderthal occupation of the Great Zab basin has been testified at the archaeological site of Shanidar Cave. Historical records for the region are available from the end of the third millennium BCE onward. In the Neo-Assyrian period ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sulaymaniyah Governorate
Sulaymaniyah Governorate ( ku, پارێزگای سلێمانی, Parêzgeha Silêmaniyê, ar, محافظة السليمانية) or Sulaymaniyah Province is a mountainous Governorates of Iraq, governorate in the Kurdistan Region of Iraq. Its largest city is Sulaymaniyah. Halabja Governorate was formerly the Halabja District, Sulaymaniyah Governorate, Halabja District of Sulaymaniyah, until it became a separate governorate in 2014. Provincial Government * Governor: Dr. Haval Abubakir * Deputy Governor: Ahmed Ali Ahmed * Provincial Council Chairman (PCC): Azad Mohammad Amin Districts See also * Hazar Merd Cave References External links * Iraq Inter-Agency Information & Analysis Unit Reports, Maps and Assessments of Iraq's Governorates from the UN Inter-Agency Information & Analysis Unit Sulaymaniyah Governorate, Governorates of Iraq Geography of Iraqi Kurdistan {{Iraq-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ranya
Ranya ( ckb, ڕانیە, Ranye, ar, رانية) is a town in the Kurdistan Region of Iraq, and is part of the Sulaymaniyah Governorate. Geography and climate Ranya City is located in the north east of the Kurdistan Region of Iraq. Ranya is located on longitude (36, 28-36, 5) N and latitude (44, 60-44, 33) E. The Ranya District is surrounded by mountains, rivers, and Lake Dukan. The area of Ranya is 884 km2 and it includes five sub-districts: Ranya City, Chwarqurna, Hajiawa, Betwata, and Sarkapkan. In Ranya, there is 900 to 1,050 ml of rainfall each year. There are four seasons in Ranya, which are affected by the Mediterranean Sea. Summer is hot and dry, while winter is considered the rain/snow Notable places * University of Raparin * Darwaza Park * Darband Bridge * Lake Dukan * Bitwen Hotel and Restaurant * Historical Painting in Darband * Grda Dema * Shimshara Hill *xabat forest * Dole resort *Raparin Monoment *Kewarash Mountain Sister cities * Duluth, Minnesota, United Sta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Above Mean Sea Level
Height above mean sea level is a measure of the vertical distance (height, elevation or altitude) of a location in reference to a historic mean sea level taken as a vertical datum. In geodesy, it is formalized as ''orthometric heights''. The combination of unit of measurement and the physical quantity (height) is called "metres above mean sea level" in the metric system, while in United States customary and imperial units it would be called "feet above mean sea level". Mean sea levels are affected by climate change and other factors and change over time. For this and other reasons, recorded measurements of elevation above sea level at a reference time in history might differ from the actual elevation of a given location over sea level at a given moment. Uses Metres above sea level is the standard measurement of the elevation or altitude of: * Geographic locations such as towns, mountains and other landmarks. * The top of buildings and other structures. * Flying objects such ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Paleolithic
The Middle Paleolithic (or Middle Palaeolithic) is the second subdivision of the Paleolithic or Old Stone Age as it is understood in Europe, Africa and Asia. The term Middle Stone Age is used as an equivalent or a synonym for the Middle Paleolithic in African archeology. The Middle Paleolithic broadly spanned from 300,000 to 30,000 years ago. There are considerable dating differences between regions. The Middle Paleolithic was succeeded by the Upper Paleolithic subdivision which first began between 50,000 and 40,000 years ago. Pettit and White date the Early Middle Paleolithic in Great Britain to about 325,000 to 180,000 years ago (late Marine Isotope Stage 9 to late Marine Isotope Stage 7), and the Late Middle Paleolithic as about 60,000 to 35,000 years ago. According to the theory of the recent African origin of modern humans, anatomically modern humans began migrating out of Africa during the Middle Stone Age/Middle Paleolithic around 125,000 years ago and began to replace e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Paleolithic
The Lower Paleolithic (or Lower Palaeolithic) is the earliest subdivision of the Paleolithic or Old Stone Age. It spans the time from around 3 million years ago when the first evidence for stone tool production and use by hominins appears in the current archaeological record, until around 300,000 years ago, spanning the Oldowan ("mode 1") and Acheulean ("mode 2") lithics industries. In African archaeology, the time period roughly corresponds to the Early Stone Age, the earliest finds dating back to 3.3 million years ago, with Lomekwian stone tool technology, spanning Mode 1 stone tool technology, which begins roughly 2.6 million years ago and ends between 400,000 and 250,000 years ago, with Mode 2 technology. The Middle Paleolithic followed the Lower Paleolithic and recorded the appearance of the more advanced prepared-core tool-making technologies such as the Mousterian. Whether the earliest control of fire by hominins dates to the Lower or to the Middle Paleolithic remai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
