|
Kopet-Dag
The Köpet Dag, Kopet Dagh, or Koppeh Dagh (; ), 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) at . Etymology Ármin Vámbéry, 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 ''koppeh'' means "pile" or " ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashgabat
Ashgabat (Turkmen language, Turkmen: ''Aşgabat'') is the capital city, capital and largest city of Turkmenistan. It lies between the Karakum Desert and the Kopet Dag, Kopetdag mountain range in Central Asia, approximately 50 km (30 mi) away from the Iran-Turkmenistan border. The city has a population of 1,030,063 (2022 census). The city was founded in 1881 on the basis of an Ahal Teke (Turkmen tribe), Teke tribal village, and made the capital of the Turkmen Soviet Socialist Republic in 1924 when it was known as Poltoratsk. Much of the city was destroyed by the 1948 Ashgabat earthquake, but has since been extensively rebuilt under the rule of Saparmurat Niyazov's "White City" urban renewal project, resulting in monumental projects sheathed in costly white marble. The Soviet-era Karakum Canal runs through the city, carrying waters from the Amu Darya from east to west. Today, as the capital of an independent Turkmenistan, Ashgabat retains a multiethnic population, wi ... [...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 Vadim 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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashgabat - Panoramio - Flydime
Ashgabat (Turkmen language, Turkmen: ''Aşgabat'') is the capital city, capital and largest city of Turkmenistan. It lies between the Karakum Desert and the Kopet Dag, Kopetdag mountain range in Central Asia, approximately 50 km (30 mi) away from the Iran-Turkmenistan border. The city has a population of 1,030,063 (2022 census). The city was founded in 1881 on the basis of an Ahal Teke (Turkmen tribe), Teke tribal village, and made the capital of the Turkmen Soviet Socialist Republic in 1924 when it was known as Poltoratsk. Much of the city was destroyed by the 1948 Ashgabat earthquake, but has since been extensively rebuilt under the rule of Saparmurat Niyazov's "White City" urban renewal project, resulting in monumental projects sheathed in costly white marble. The Soviet-era Karakum Canal runs through the city, carrying waters from the Amu Darya from east to west. Today, as the capital of an independent Turkmenistan, Ashgabat retains a multiethnic population, wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bereket
Bereket, formerly Gazanjyk or ''Kazandzhik'' ( or gɑˈzɑnd͡ʒik), is a List of cities in Turkmenistan, 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 Kopet Dag, Kopetdag Mountains and on the edge of the Karakum Desert. Bereket is a strategic Bereket railway station (Turkmenistan), junction of the Trans-Caspian Railway (Caspian Sea-Turkmenistan-Uzbekistan-Kazakhstan) and North–South Transport Corridor, 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tethys Sea
The Tethys Ocean ( ; ), also called the Tethys Sea or the Neo-Tethys, was a prehistoric ocean during much of the Mesozoic Era and early-mid Cenozoic Era. It was the predecessor to the modern Indian Ocean, the Mediterranean Sea, and the Eurasian inland marine basins (primarily represented today by the Black Sea and Caspian Sea). During the early Mesozoic, as Pangaea broke up, the Tethys Ocean was defined as the ocean located between the ancient continents of Gondwana and Laurasia. After the opening of the Indian and Atlantic oceans during the Cretaceous Period and the breakup of these continents over the same period, it came to be defined as the ocean bordered by the continents of Africa, Eurasia, India, and Australasia. During the early-mid Cenozoic, the Indian, African, Australian and Arabian plates moved north and collided with the Eurasian plate, which created new borders to the ocean, a land barrier to the flow of currents between the Indian and Mediterranean basins, and t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iranian Plate
The Iranian plateau or Persian plateau is a geological feature spanning parts of the Caucasus, Central Asia, South Asia, and West Asia. It makes up part of the Eurasian plate, and is wedged between the Arabian plate and the Indian plate. The plateau is situated between the Zagros Mountains to the west, the Caspian Sea and the Köpet Dag to the north, the Armenian Highlands and the Caucasus Mountains to the northwest, the Strait of Hormuz and the Persian Gulf to the south, and the Indian subcontinent to the southeast. As a historical region, it includes Parthia, Media, Persis, and some of the previous territories of Greater Iran."Old Iranian Online" , University of Texas College of Liberal Arts (retrieved 10 February 2007) The Zagros form the plateau's western boundary, and its eastern slopes may also be in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geosyncline
A geosyncline (originally called a geosynclinal) is an obsolete geology, geological concept to explain orogeny, orogens, which was developed in the late 19th and early 20th centuries, before the theory of plate tectonics was envisaged.#Sengor1982, Şengör (1982), p. 11 A geosyncline was described as a giant downward fold in the crust (geology), Earth's crust, with associated upward folds called geanticlines (or geanticlinals), that preceded the climax phase of orogeny, orogenic deformation. History The geosyncline concept was first conceived by the American geologists James Hall (paleontologist), 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.#Sengor1982, 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 w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pliocene
The Pliocene ( ; also Pleiocene) is the epoch (geology), epoch in the geologic time scale that extends from 5.33 to 2.58See the 2014 version of the ICS geologic time scale million years ago (Ma). It is the second and most recent epoch of the Neogene Period in the Cenozoic, Cenozoic Era. The Pliocene follows the Miocene Epoch and is followed by the Pleistocene Epoch. Prior to the 2009 revision of the geologic time scale, which placed the four most recent major glaciations entirely within the Pleistocene, the Pliocene also included the Gelasian Stage, which lasted from 2.59 to 1.81 Ma, and is now included in the Pleistocene. As with other older geologic periods, the Stratum, geological strata that define the start and end are well-identified but the exact dates of the start a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
