|
Shabran District
Shabran District ( az, Şabran rayonu) is one of the 66 districts of Azerbaijan. It is located in the north-east of the country and belongs to the Guba-Khachmaz Economic Region. The district borders the districts of Khachmaz, Quba, Khizi and Siyazan. Its capital and largest city is Shabran. As of 2020, the district had a population of 59,900. History The district was formed as Davachi District on August 8, 1930. It was abolished and included into Absheron District in 1963, however, two years later, the district was re-established. In 1992, the new Siazan District was formed south of modern Shabran District by the order of the National Assembly of Azerbaijan, which included part of Davachi District's territory. In 2010, the district was renamed ''Shabran District''. Geography The greater part of the district is mountainous. The Caspian Sea is located 12 km from Shabran city. The district borders upon Quba, Khachmaz, Shamakhi and Siazan Districts. Forests occupy 27000 h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Administrative Divisions Of Azerbaijan
Azerbaijan is administratively divided into 66 districts () and 11 cities () that are subordinate to the Republic. Out of these, 7 districts and 1 city is located within the Nakhchivan Autonomous Republic. The districts are further divided into municipalities (). Additionally, the districts of Azerbaijan are grouped into 14 Economic Regions (). On July 7, 2021, the President of Azerbaijan Ilham Aliyev signed Decree "On the new division of economic regions in the Republic of Azerbaijan". Administrative divisions Contiguous Azerbaijan The territory of former Nagorno-Karabakh Autonomous Oblast presently consists of the districts of Khojavend, Shusha, Khojaly, the eastern portion of Kalbajar and the western portion of Tartar. The Autonomous Oblast was abolished on 26 November 1991, by the Supreme Soviet of the Azerbaijan SSR. Since then, the territory of the autonomous oblast has been administratively split between the aforementioned districts. As a result of the First Nag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Assembly Of Azerbaijan
The National Assembly ( az, Milli Məclis), also transliterated as Milli Mejlis, is the legislative branch of government in Azerbaijan. The unicameral National Assembly has 125 deputies: previously 100 members were elected for five-year terms in single-seat constituency, constituencies and 25 were members elected by proportional representation; as of the latest election, however, all 125 deputies are returned from single-member constituencies. Power in Azerbaijan is heavily concentrated in Ilham Aliyev, the President of Azerbaijan. Parliamentary elections in Azerbaijan are not free and fair. History Azerbaijan Democratic Republic (1918–1920) Following the Russian Revolution (1917), Russian Revolution in February 1917, a special committee consisting of deputies from Transcaucasian Seym#Sejm, Transcaucasian State Duma was created. In November, Transcaucasian Commissariat was created as the first government of independent Transcaucasia. The Sejm made up of representatives ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silk Road
The Silk Road () was a network of Eurasian trade routes active from the second century BCE until the mid-15th century. Spanning over 6,400 kilometers (4,000 miles), it played a central role in facilitating economic, cultural, political, and religious interactions between the East and West. The name "Silk Road", first coined in the late 19th century, has fallen into disuse among some modern historians in favor of Silk Routes, on the grounds that it more accurately describes the intricate web of land and sea routes connecting East and Southeast Asia, the Indian subcontinent, Central Asia, the Middle East, East Africa and Europe. The Silk Road derives its name from the highly lucrative trade of silk textiles that were produced almost exclusively in China. The network began with the Han dynasty's expansion into Central Asia around 114 BCE, which largely pacified the once untamed region. Imperial envoy Zhang Qian was commissioned to explore the unknown lands beyond the regio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chirag Gala
Chirag Gala ( az, Çıraqqala), also spelled Çiraq Qala or Çirax Qala, which means ''lamp castle'' in Azerbaijani is a ruined ancient fortress overlooking the Caspian coastal plains north of Baku in Azerbaijan. It is located on the top of a mountain, in the Guba Forest. It was constructed by the Sassanid Persians in the 5th century, it was used as a defense for the khanate of Quba Quba () is a city and the administrative centre of the Quba District of Azerbaijan. The city lies on the north-eastern slopes of Shahdag mountain, at an altitude of 600 metres above sea level, on the right bank of the Kudyal river. It has a po ... in the 18th century. Today the Chirag Gala is a historic site and is frequently visited by tourists. Because of the large rocks and rough road, the Chirag Gala is almost impossible to reach with any vehicle. Most tourists and people travel by foot to the top of the mountain. History Chirag gala was built in 4-5th century AD and its function is sta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tat People (Caucasus)
The Tat people (also: ''Tat'', ''Parsi'', ''Daghli'', ''Lohijon'') are an Iranian people presently living within Azerbaijan and Russia (mainly Southern Dagestan). The Tats are part of the indigenous peoples of Iranian origin in the Caucasus. Tats use the Tat language, a southwestern Iranian language somewhat different from Standard Persian, as well as Azerbaijani and Russian. Tats are mainly Shia Muslims with a significant Sunni Muslim minority. The 1886–1892 Tsarist population figures counted 124,683 Tats in the Russian Caucasus of which 118,165 were located in the Baku Governorate and 3,609 in the Dagestan Oblast.Tsutsiev, Arthur. "Appendix 3: Ethnic Composition of the Caucasus: Historical Population Statistics". Atlas of the Ethno-Political History of the Caucasus, New Haven: Yale University Press, 2014, p. 180. The 1897 Russian Empire census recorded 95,056 Tats, of which 89,519 were in the Baku Governorate and 2,998 in the Dagestan Oblast. The 1926 Soviet census only ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gravel
Gravel is a loose aggregation of rock fragments. Gravel occurs naturally throughout the world as a result of sedimentary and erosive geologic processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb). Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Gas
Natural gas (also called fossil gas or simply gas) is a naturally occurring mixture of gaseous hydrocarbons consisting primarily of methane in addition to various smaller amounts of other higher alkanes. Low levels of trace gases like carbon dioxide, nitrogen, hydrogen sulfide, and helium are also usually present. Natural gas is colorless and odorless, so odorizers such as mercaptan (which smells like sulfur or rotten eggs) are commonly added to natural gas supplies for safety so that leaks can be readily detected. Natural gas is a fossil fuel and non-renewable resource that is formed when layers of organic matter (primarily marine microorganisms) decompose under anaerobic conditions and are subjected to intense heat and pressure underground over millions of years. The energy that the decayed organisms originally obtained from the sun via photosynthesis is stored as chemical energy within the molecules of methane and other hydrocarbons. Natural gas can be burned for h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Global Warming
In common usage, climate change describes global warming—the ongoing increase in global average temperature—and its effects on Earth's climate system. Climate change in a broader sense also includes previous long-term changes to Earth's climate. The current rise in global average temperature is more rapid than previous changes, and is primarily caused by humans burning fossil fuels. Fossil fuel use, deforestation, and some agricultural and industrial practices increase greenhouse gases, notably carbon dioxide and methane. Greenhouse gases absorb some of the heat that the Earth radiates after it warms from sunlight. Larger amounts of these gases trap more heat in Earth's lower atmosphere, causing global warming. Due to climate change, deserts are expanding, while heat waves and wildfires are becoming more common. Increased warming in the Arctic has contributed to melting permafrost, glacial retreat and sea ice loss. Higher temperatures are also causing ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene. Some geologists assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868). During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first humans ('' Homo habilis'') appeared in Africa near the end of the period. Some continental movements took place, the most significant event being the connection of North America, North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the warm ocean currents from th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene ( ; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago ( Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of the Cretaceous–Paleogene extinction event that ended the preceding ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mud Volcano
A mud volcano or mud dome is a landform created by the eruption of mud or slurries, water and gases. Several geological processes may cause the formation of mud volcanoes. Mud volcanoes are not true igneous volcanoes as they do not produce lava and are not necessarily driven by magmatic activity. Mud volcanoes may range in size from merely 1 or 2 meters high and 1 or 2 meters wide, to 700 meters high and 10 kilometers wide. Smaller mud exudations are sometimes referred to as mud-pots. The mud produced by mud volcanoes is mostly formed as hot water, which has been heated deep below the Earth's surface, begins to mix and blend with subterranean mineral deposits, thus creating the mud slurry exudate. This material is then forced upwards through a geological fault or fissure due to local subterranean pressure imbalances. Mud volcanoes are associated with subduction zones and about 1100 have been identified on or near land. The temperature of any given active mud volcano genera ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
