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Kopet Dag
The Köpet Dag, Kopet Dagh, or Koppeh Dagh ( tk, Köpetdag; fa, کپهداغ), also known as the Turkmen-Khorasan Mountain Range, is a mountain range on the border between Turkmenistan and Iran that extends about along the border southeast of the Caspian Sea, stretching northwest-southeast from near the Caspian Sea in the northwest to the Harirud River in the southeast. In the southwest it borders on the parallel eastern endings of the Alborz mountains being together part of the much larger Alpide belt. The highest peak of the range in Turkmenistan is the Mount Rizeh (Kuh-e Rizeh), located at the southwest of the capital Ashgabat and stands at . The highest Iranian summit is Mount Quchan (Kuh-e Quchan) with . Etymology Vambery conjectured that ''köpet'' originates from the Turkmen language where "köp" means "a lot" or "many" and the word "dag" means "mountain" or "peak". He thus translated Köpetdag as "Many mountains (peaks)". He and others noted that in Persian ''koppe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bereket
Bereket, formerly Gazanjyk or ''Kazandzhik'' (russian: Казанджик or tk, Газанҗык gɑˈzɑnd͡ʒik), is a city in Balkan Province in western Turkmenistan. Bereket is the administrative centre of Bereket District. Bereket is located in an oasis in the foothills of the Kopetdag Mountains and on the edge of the Karakum Desert. Bereket is a strategic junction of the Trans-Caspian Railway (Caspian Sea-Turkmenistan-Uzbekistan-Kazakhstan) and North-South Transnational Railway (Russia-Kazakhstan-Turkmenistan-Iran-Persian Gulf. The city has a large locomotive repair depot and a modern railway station. The city is located approximately west of the Turkmen capital of Ashgabat and east of the Caspian Sea port of Türkmenbaşy, Turkmenistan, Turkmenbashy. The largest cities nearby are Balkanabat to the west, and Serdar (city), Serdar to the east. The estimated population of the city is 24,500 as of March 2015. Etymology ''Gazanjyk'' is probably derived from th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first epoch (geology), geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Parthia
Parthia ( peo, 𐎱𐎼𐎰𐎺 ''Parθava''; xpr, 𐭐𐭓𐭕𐭅 ''Parθaw''; pal, 𐭯𐭫𐭮𐭥𐭡𐭥 ''Pahlaw'') is a historical region located in northeastern Greater Iran. It was conquered and subjugated by the empire of the Medes during the 7th century BC, was incorporated into the subsequent Achaemenid Empire under Cyrus the Great in the 6th century BC, and formed part of the Hellenistic Seleucid Empire following the 4th-century-BC conquests of Alexander the Great. The region later served as the political and cultural base of the Eastern Iranian Parni people and Arsacid dynasty, rulers of the Parthian Empire (247 BC – 224 AD). The Sasanian Empire, the last state of pre-Islamic Iran, also held the region and maintained the seven Parthian clans as part of their feudal aristocracy. Name The name "Parthia" is a continuation from Latin ', from Old Persian ', which was the Parthian language self-designator signifying "of the Parthians" who were an Iranian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bactria–Margiana Archaeological Complex
The Bactria–Margiana Archaeological Complex (short BMAC) or Oxus Civilization, recently dated to c. 2250–1700 BC,Lyonnet, Bertille, and Nadezhda A. Dubova, (2020b)"Questioning the Oxus Civilization or Bactria- Margiana Archaeological Culture (BMAC): an overview" in Bertille Lyonnet and Nadezhda A. Dubova (eds.), ''The World of the Oxus Civilization'', Routledge, London and New York, p. 32.: "...Salvatori has often dated its beginning very early (ca. 2400 BC), to make it match with Shahdad where a large amount of material similar to that of the BMAC has been discovered. With the start of international cooperation and the multiplication of analyses, the dates now admitted by all place the Oxus Civilization between 2250 and 1700 BC, while its final phase extends until ca. 1500 BC..." is the modern archaeological designation for a Bronze Age civilization of Central Asia, previously dated to c. 2400–1900 BC, by Sandro Salvatori, in its urban phase or Integration Era. Though i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jeitun
Jeitun (Djeitun) is an archaeological site of the Neolithic period in southern Turkmenistan, about 30 kilometers north of Ashgabat in the Kopet-Dag mountain range. The settlement was occupied from about 7200 to 4500 BC possibly with short interruptions. Jeitun has given its name to the whole Neolithic period in the foothills of the Kopet Dag. Excavations Jeitun was discovered by Alexander Marushchenko and has been excavated since the 1950s by Boris Kuftin and Mikhail Masson. The site covers an area of about 5,000 square meters. It consists of free-standing houses of a uniform ground plan. The houses were rectangular and had a large fireplace on one side and a niche facing it as well as adjacent yard areas. The floors were covered with lime plaster. The buildings were made of sun-dried cylindrical clay blocks about 70 cm long and 20 cm thick. The clay was mixed with finely chopped straw. There were about 30 houses that could have accommodated about 150–200 persons.Harris, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gorgan Plain
The Gorgan Plain, or Dasht-e Gorgan ( fa, دشت گرگان), is situated in northeastern Iran in Golestan Province. It extends from the lower slopes of the Alborz and Kopet Dag mountain ranges to the steppes of Turkmenistan. The River Gorgan flows through the plain from east to west, emptying into the Caspian Sea. The provincial capital Gorgan lies to the south of the plain, which covers an area of about and is situated between 37°00' and 37°30' north latitude, and between 54°00' and 54°30' east longitude. The annual precipitation in the south of the plain is about which is much higher than the just to the north. The southern part is very fertile, being watered by the many streams that flow from the Alborz Mountains. History More than fifty Neolithic sites have been identified on the Gorgan Plain. Most are raised on mounds and many have seen more than one period of occupation. The sites are thought to relate to the Jeitun culture of southern Turkmenistan and may date t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karakum , a medieval city in Mongolia
{{Disambiguation ...
Karakum may refer to: *Karakum Desert, a desert in Central Asia * ''Karakum'' (film), a 1994 Turkmen film *Karakum Canal, Turkmenistan * Karakum District, Turkmenistan See also * Karakoram, a large mountain range spanning the borders of India, Pakistan and China * Karakorum Karakorum ( Khalkha Mongolian: Хархорум, ''Kharkhorum''; Mongolian Script:, ''Qaraqorum''; ) was the capital of the Mongol Empire between 1235 and 1260 and of the Northern Yuan dynasty in the 14–15th centuries. Its ruins lie in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geosyncline
A geosyncline (originally called a geosynclinal) is an obsolete geological concept to explain orogens, which was developed in the late 19th and early 20th centuries, before the theory of plate tectonics was envisaged. Şengör (1982), p. 11 A geosyncline was described as a giant downward fold in the Earth's crust, with associated upward folds called geanticlines (or geanticlinals), that preceded the climax phase of orogenic deformation. History The geosyncline concept was first conceived by the American geologists James Hall and James Dwight Dana in the mid-19th century, during the classic studies of the Appalachian Mountains. Émile Haug further developed the geosyncline concept, and introduced it to Europe in 1900. Şengör (1982), p. 26 Eduard Suess, a leading geologist of his time, disapproved the concept of geosyncline, and in 1909 he argued against its use due to its association with outdated theories. Şengör (1982), p. 43 This did not prevent further development of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eurasian Plate
The Eurasian Plate is a tectonic plate that includes most of the continent of Eurasia (a landmass consisting of the traditional continents of Europe and Asia), with the notable exceptions of the Indian subcontinent, the Arabian subcontinent and the area east of the Chersky Range in eastern Siberia. It also includes oceanic crust extending westward to the Mid-Atlantic Ridge and northward to the Gakkel Ridge. The eastern edge is a boundary with the North American Plate to the north and a boundary with the Philippine Sea Plate to the south and possibly with the Okhotsk Plate and the Amurian Plate. The southern edge is a boundary with the African Plate to the west, the Arabian Plate in the middle and the Indo-Australian Plate to the east. The western edge is a divergent boundary with the North American Plate forming the northernmost part of the Mid-Atlantic Ridge, which is straddled by Iceland. All volcanic eruptions in Iceland, such as the 1973 eruption of Eldfell, the 17 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iranian Plate
The Iranian Plate is a small tectonic plate thought to underlie the Persian plateau, covering the modern-day countries of Iran and Afghanistan, and parts of Iraq and Pakistan. It is compressed between the Arabian Plate to the southwest, the Eurasian Plate to the north, and the Indian Plate to the southeast. This compression is likely a cause for the very mountainous terrain of the area including the Alborz and Zagros Mountains The Zagros Mountains ( ar, جبال زاغروس, translit=Jibal Zaghrus; fa, کوههای زاگرس, Kuh hā-ye Zāgros; ku, چیاکانی زاگرۆس, translit=Çiyakani Zagros; Turkish: ''Zagros Dağları''; Luri: ''Kuh hā-ye Zāgr .... References * William Bayne Fisher''The Middle East: a Physical, Social, and Regional Geography'' Routledge 1978, , p. 15–16 Tectonic plates Geology of Afghanistan Geology of Iran Geology of Iraq Geology of Pakistan {{tectonics-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arabian Plate
The Arabian Plate is a minor tectonic plate in the Northern and Eastern Hemispheres. It is one of the three continental plates (along with the African and the Indian Plates) that have been moving northward in geological history and colliding with the Eurasian Plate. That is resulting in a mingling of plate pieces and mountain ranges extending in the west from the Pyrenees, crossing Southern Europe to Iran, forming the Alborz and the Zagros Mountains, to the Himalayas and ranges of Southeast Asia. Lexicology The ''Arabian Plate'' is a designation of the region, and it is also sometimes referred to as the ''Arab Plate''. Borders The Arabian Plate consists mostly of the Arabian Peninsula; it extends westward to the Sinai Peninsula and the Red Sea and northward to the Levant. The plate borders are: *East, with the Indian Plate, at the Owen Fracture Zone *South, with the African Plate to the west and the Somali Plate and the Indian Plate to the east *West, a left lateral ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
