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Alasht
Alasht ( fa, آلاشت, ', meaning ''Eagle Sanctuary'', also Romanized as Ālāsht) is a city in the Central District of Savadkuh County, Mazandaran Province, Iran. At the 2016 census, its population was 1,193. Alasht is isolated by surrounding mountains, which gives it a cooler climate than most regions of the province. It is most known for being the birthplace of Reza Shah Pahlavi, the founder of the Pahlavi dynasty. Natural resources Alasht has a natural spring and is also noted for being one of the few cryotherapy spots of the province. In addition, caves in and around Alasht are rich with minerals, mostly anthracite coal reserves. Climate Due to its location, Alasht is fairly cool throughout the year. Winter in the village is particularly harsh, causing most of the inhabitants to move to warmer areas for the season. However, the rainfall in the village is similar to the rest of the province, with approximately 593 millimeters of precipitation per year. Gallery File:A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reza Shah
Reza Shah Pahlavi ( fa, رضا شاه پهلوی; ; originally Reza Khan (); 15 March 1878 – 26 July 1944) was an Iranian Officer (armed forces), military officer, politician (who served as Ministry of Defence and Armed Forces Logistics (Iran), minister of war and Prime Minister of Iran, prime minister), and first shah of the Pahlavi dynasty, House of Pahlavi of the Pahlavi Iran, Imperial State of Iran and father of the Mohammad Reza Pahlavi, last shah of Iran. He reigned from 15 December 1925 until he was forced to abdication, abdicate by the Anglo-Soviet invasion of Iran on 16 September 1941. Reza Shah introduced many social, economic, and political reforms during his reign, ultimately laying the foundation of the modern Iranian state. Therefore, he is regarded as the founder of modern Iran. At the age of 14 he joined the Persian Cossack Brigade, Iranian Cossack Brigade, and also served in the army. In 1911, he was promoted to first lieutenant, by 1912 he was elevated to the r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Savadkuh County
Savadkuh County ( fa, شهرستان سوادكوه, ''Ŝahrestāne Sawādkuh''; also Savadkooh and Savadkouh) is located in Mazandaran province, Iran. The capital of the county is Pol Sefid. At the 2006 census, the county's population (including those portions of the county later split off to form North Savadkuh County) was 66,430, in 17,918 households. Retrieved 4 November 2022 At the 2016 census, the county's population was 43,913, in 14,956 households. The county of North Savadkuh was formed in 2013 from the former Shirgah and Narenjestan Districts of Savadkuh County, including the city of Shirgah and the village of Leford. Covering an area of , Savadkuh is at the centre of Mazandaran Province. It is limited northwestward by North Savadkuh County, westward by Babol County, eastward by Sari County, southward by the Alborz mountain range and Tehran province, and southeast by Semnan province. The main part of this county is located in a valley, in the central Alborz regio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reza Shah Pahlavi
, , spouse = Maryam Savadkoohi Tadj ol-Molouk Ayromlu (queen consort) Turan Amirsoleimani Esmat Dowlatshahi , issue = Princess Hamdamsaltaneh Princess ShamsMohammad Reza ShahPrincess Ashraf Prince Ali Reza Prince Gholam Reza Prince Abdul Reza Prince Ahmad Reza Prince Mahmoud Reza Princess Fatemeh Prince Hamid Reza , house = Pahlavi , father = Abbas-Ali Khan , mother = Noush-Afarin , religion = , birth_date = , birth_place = Alasht, Savadkuh, Mazandaran, Sublime State of Persia , death_date = , death_place = Johannesburg, Union of South Africa , burial_place = 7 May 1950 Mausoleum of Reza Shah, Shah Abdol-Azim Shrine, Rey , signature = , module = Reza Shah Pahlavi ( fa, رضا شاه پهلوی; ; originally Reza Khan (); 15 March 1878 – 26 July 1944) was an Iranian military officer, politician (who served as minister of war and prime minister), and first shah of the House of Pahlavi of the Imperial St ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pahlavi Dynasty
The Pahlavi dynasty ( fa, دودمان پهلوی) was the last Iranian royal dynasty, ruling for almost 54 years between 1925 and 1979. The dynasty was founded by Reza Shah Pahlavi, a non-aristocratic Mazanderani soldier in modern times, who took on the name of the Pahlavi language spoken in the pre-Islamic Sasanian Empire in order to strengthen his nationalist credentials. The dynasty replaced the Qajar dynasty in 1925 after the 1921 coup d'état, beginning on 14 January 1921 when 42-year-old soldier Reza Khan was promoted by British General Edmund Ironside to lead the British-run Persian Cossack Brigade. About a month later, under British direction, Reza Khan's 3,000-4,000 strong detachment of the Cossack Brigade reached Tehran in what became known as the 1921 Persian coup d'état. The rest of the country was taken by 1923, and by October 1925 the Majlis agreed to depose and formally exile Ahmad Shah Qajar. The Majlis declared Reza Pahlavi as the new Shah of Iran o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central District (Savadkuh County)
The Central District of Savadkuh County ( fa, بخش مرکزی شهرستان سوادکوه) is a district ( bakhsh) in Savadkuh County, Mazandaran Province, Iran. At the 2006 census, its population was 42,679, in 11,396 families. The District has three cities: Pol Sefid, Zirab, and Alasht. The District has four rural districts (''dehestan''): Kaseliyan Rural District, Rastupey Rural District, Sorkhkola Rural District, and Valupey Rural District Valupey Rural District ( fa, دهستان ولوپي) (Velopi use in local pronunciation) is a rural district (''dehestan'') in the Central District of Savadkuh County, Mazandaran Province, Iran Iran, officially the Islamic Republi .... References Savadkuh County Districts of Mazandaran Province {{Savadkuh-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Sovereign States
The following is a list providing an overview of sovereign states around the world with information on their status and recognition of their sovereignty. The 206 listed states can be divided into three categories based on membership within the United Nations System: 193 member states of the United Nations, UN member states, 2 United Nations General Assembly observers#Present non-member observers, UN General Assembly non-member observer states, and 11 other states. The ''sovereignty dispute'' column indicates states having undisputed sovereignty (188 states, of which there are 187 UN member states and 1 UN General Assembly non-member observer state), states having disputed sovereignty (16 states, of which there are 6 UN member states, 1 UN General Assembly non-member observer state, and 9 de facto states), and states having a political status of the Cook Islands and Niue, special political status (2 states, both in associated state, free association with New Zealand). Compi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, Rain and snow mixed, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called shower (precipitation), showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anthracite Coal
Anthracite, also known as hard coal, and black coal, is a hard, compact variety of coal that has a submetallic luster. It has the highest carbon content, the fewest impurities, and the highest energy density of all types of coal and is the highest ranking of coals. Anthracite is the most metamorphosed type of coal (but still represents low-grade metamorphism), in which the carbon content is between 86% and 97%. The term is applied to those varieties of coal which do not give off tarry or other hydrocarbon vapours when heated below their point of ignition. Anthracite ignites with difficulty and burns with a short, blue, and smokeless flame. Anthracite is categorized into standard grade, which is used mainly in power generation, high grade (HG) and ultra high grade (UHG), the principal uses of which are in the metallurgy sector. Anthracite accounts for about 1% of global coal reserves, and is mined in only a few countries around the world. The Coal Region of northeastern P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mineral
In geology and mineralogy, a mineral or mineral species is, broadly speaking, a solid chemical compound with a fairly well-defined chemical composition and a specific crystal structure that occurs naturally in pure form.John P. Rafferty, ed. (2011): Minerals'; p. 1. In the series ''Geology: Landforms, Minerals, and Rocks''. Rosen Publishing Group. The geological definition of mineral normally excludes compounds that occur only in living organisms. However, some minerals are often biogenic (such as calcite) or are organic compounds in the sense of chemistry (such as mellite). Moreover, living organisms often synthesize inorganic minerals (such as hydroxylapatite) that also occur in rocks. The concept of mineral is distinct from rock, which is any bulk solid geologic material that is relatively homogeneous at a large enough scale. A rock may consist of one type of mineral, or may be an aggregate of two or more different types of minerals, spacially segregated into disti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as '' speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cryotherapy
Cryotherapy, sometimes known as cold therapy, is the local or general use of low temperatures in medical therapy. Cryotherapy may be used to treat a variety of tissue lesions. The most prominent use of the term refers to the surgical treatment, specifically known as cryosurgery or cryoablation. Cryosurgery is the application of extremely low temperatures to destroy abnormal or diseased tissue and is used most commonly to treat skin conditions. Cryotherapy is used in an effort to relieve muscle pain, sprains and swelling after soft tissue damage or surgery. For decades, it has been commonly used to accelerate recovery in athletes after exercise. Cryotherapy decreases the temperature of tissue surface to minimize hypoxic cell death, edema accumulation, and muscle spasms, all of which ultimately alleviate discomfort and inflammation. It can be a range of treatments from the application of ice packs or immersion in ice baths (generally known as cold therapy), to the use of cold chamb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (water)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
