1.
Russian language
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Russian is an East Slavic language and an official language in Russia, Belarus, Kazakhstan, Kyrgyzstan and many minor or unrecognised territories. Russian belongs to the family of Indo-European languages and is one of the four living members of the East Slavic languages, written examples of Old East Slavonic are attested from the 10th century and beyond. It is the most geographically widespread language of Eurasia and the most widely spoken of the Slavic languages and it is also the largest native language in Europe, with 144 million native speakers in Russia, Ukraine and Belarus. Russian is the eighth most spoken language in the world by number of native speakers, the language is one of the six official languages of the United Nations. Russian is also the second most widespread language on the Internet after English, Russian distinguishes between consonant phonemes with palatal secondary articulation and those without, the so-called soft and hard sounds. This distinction is found between pairs of almost all consonants and is one of the most distinguishing features of the language, another important aspect is the reduction of unstressed vowels. Russian is a Slavic language of the Indo-European family and it is a lineal descendant of the language used in Kievan Rus. From the point of view of the language, its closest relatives are Ukrainian, Belarusian, and Rusyn. An East Slavic Old Novgorod dialect, although vanished during the 15th or 16th century, is considered to have played a significant role in the formation of modern Russian. In the 19th century, the language was often called Great Russian to distinguish it from Belarusian, then called White Russian and Ukrainian, however, the East Slavic forms have tended to be used exclusively in the various dialects that are experiencing a rapid decline. In some cases, both the East Slavic and the Church Slavonic forms are in use, with different meanings. For details, see Russian phonology and History of the Russian language and it is also regarded by the United States Intelligence Community as a hard target language, due to both its difficulty to master for English speakers and its critical role in American world policy. The standard form of Russian is generally regarded as the modern Russian literary language, mikhail Lomonosov first compiled a normalizing grammar book in 1755, in 1783 the Russian Academys first explanatory Russian dictionary appeared. By the mid-20th century, such dialects were forced out with the introduction of the education system that was established by the Soviet government. Despite the formalization of Standard Russian, some nonstandard dialectal features are observed in colloquial speech. Thus, the Russian language is the 6th largest in the world by number of speakers, after English, Mandarin, Hindi/Urdu, Spanish, Russian is one of the six official languages of the United Nations. Education in Russian is still a choice for both Russian as a second language and native speakers in Russia as well as many of the former Soviet republics. Russian is still seen as an important language for children to learn in most of the former Soviet republics, samuel P. Huntington wrote in the Clash of Civilizations, During the heyday of the Soviet Union, Russian was the lingua franca from Prague to Hanoi
2.
Crimean Tatar language
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Crimean Tatar, also called Crimean Turkish or simply Crimean, is a language spoken for centuries in Crimea. It is a Turkic language spoken in Crimea and the Crimean Tatar diasporas of Uzbekistan, Turkey, Romania and Bulgaria, as well as communities in the United States. It should not be confused with Tatar proper, spoken in Tatarstan and adjacent regions in Russia, though only distantly related, it has been extensively influenced by nearby Oghuz Turkic languages such as Turkish, Turkmen, and Azerbaijani. Today, more than 260,000 Crimean Tatars live in Crimea, approximately 150,000 reside in Central Asia, where their ancestors had been exiled in 1944 during World War II by the Soviet Union. However, of all people, mostly the older generations are the only ones still speaking Crimean Tatar. In 2013, the language was estimated to be on the brink of extinction, Turkey has provided support to Ukraine, to aid in bringing the schools teaching in Crimean Tatar to a modern state. An estimated 5 million people of Crimean origin live in Turkey, descendants of those who emigrated in the 19th, of these an estimated 2,000 still speak the language. Smaller Crimean Tatar communities are found in Romania, Bulgaria. Crimean Tatar is one of the endangered languages in Europe. Almost all Crimean Tatars are bilingual or multilingual, using as their first language the dominant languages of their home countries, such as Ukrainian, Turkish, Uzbek. Each of the three groups of the Crimean Tatars has its own dialect. The dialect of the Nogays, the inhabitants of the Crimean steppe, is of Kypchak–Nogay origin. The Yalıboylus, who lived on the southern coast of Crimea before 1944, the Tat Tatars from the Crimean Mountains use a middle dialect of Kypchak–Cuman origin. The dialect is a descendant of the Cuman language. The modern Crimean Tatar written language is based on Tat because the Tats comprise about 55% of the total Crimean Tatar population, the forming of the Crimean Tatar spoken dialects began with the first Turkic invasions of Crimea and ended during the period of the Crimean Khanate. However, the written languages of the Crimean Khanate were Chagatai. After Islamization, Crimean Tatars wrote with an Arabic script, in 1876, the different Turkic Crimean dialects were made into a uniform written language by Ismail Gasprinski. A preference was given to the Oghuz dialect of the Yalıboylus, in 1928, the language was reoriented to the middle dialect spoken by the majority of the people
3.
Roman-Kosh
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Roman-Kosh is the highest peak of Crimean Mountains. List of European ultra prominent peaks Енциклопедія українознавства, — Париж, Нью-Йорк, Молоде життя, 1954—1989
4.
Summit
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A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
5.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
6.
Crimea
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The peninsula is located south of the Ukrainian region of Kherson and west of the Russian region of Kuban. It is connected to Kherson Oblast by the Isthmus of Perekop and is separated from Kuban by the Strait of Kerch, the Arabat Spit is located to the northeast, a narrow strip of land that separates a system of lagoons named Sivash from the Sea of Azov. Crimea has historically been at the boundary between the world and the Pontic–Caspian steppe. Crimea and adjacent territories were united in the Crimean Khanate during the 15th to 18th century, in 1783, Crimea was annexed by the Russian Empire. It became the Autonomous Republic of Crimea within newly independent Ukraine in 1991, with Sevastopol having its own administration, within Ukraine, the ex-Soviet Black Sea Fleet and its facilities were divided between Russias Black Sea Fleet and the Ukrainian Naval Forces. The two navies shared some of the harbours and piers, while others were demilitarised or used by either country. Sevastopol remained the location of the Russian Black Sea Fleet headquarters with the Ukrainian Naval Forces Headquarters also based in the city, most of the international community does not recognize the annexation and considers Crimea to be Ukrainian territory. Russia currently administers the peninsula as two federal subjects, the Republic of Crimea and the city of Sevastopol. Ukraine continues to assert its right over the peninsula, the classical name Tauris or Taurica is from the Greek Ταυρική, after the peninsulas Scytho-Cimmerian inhabitants, the Tauri. In English usage since the modern period the Crimean Khanate is referred to as Crim Tartary. The Italian form Crimea also becomes current during the 18th century, the omission of the definite article in English became common during the later 20th century. The name Crimea follows the Italian form from the Crimean Tatar name for the city Qırım which served as a capital of the Crimean province of the Golden Horde, the name of the capital was extended to the entire peninsula at some point during Ottoman suzerainty. The origin of the word Qırım is uncertain, suggestions argued in various sources include, a corruption of Cimmerium. A derivation from the Turkic term qirum, from qori-, other suggestions that have not been supported by sources but are apparently based on similarity in sound include, a derivation from the Greek Cremnoi. However, he identifies the port, not in Crimea, no evidence has been identified that this name was ever in use for the peninsula. The classical name was revived in 1802 in the name of the Russian Taurida Governorate, in the 8th century BCE the Cimmerians migrated to the region and subsequently the Scythians as well it being the site of Greek colonies. The most important city was Chersonesos at the edge of todays Sevastopol, the Persian Achaemenid Empire expanded to Crimea. Later occupiers included the Romans, Goths, Huns, Bulgars, the Byzantine Empire, Khazars, the Kipchaks, the Golden Horde, consideration of the succeeding residents of the peninsula by their linguistic grouping is also of relevance
7.
Geologic time scale
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The table of geologic time spans, presented here, agrees with the nomenclature, dates and standard color codes set forth by the International Commission on Stratigraphy. Evidence from radiometric dating indicates that Earth is about 4.54 billion years old, the geology or deep time of Earth’s past has been organized into various units according to events which took place in each period. Older time spans, which predate the reliable record, are defined by their absolute age. Some other planets and moons within the Solar System have sufficiently rigid structures to have preserved records of their own histories, for example, Venus, Mars, dominantly fluid planets, such as the gas giants, do not preserve their history in a comparable manner. Apart from the Late Heavy Bombardment, events on other planets probably had little influence on the Earth. Construction of a scale that links the planets is, therefore, of only limited relevance to the Earths time scale. The existence, timing, and terrestrial effects of the Late Heavy Bombardment is still debated, the largest defined unit of time is the supereon, composed of eons. Eons are divided into eras, which are in turn divided into periods, epochs, the terms eonothem, erathem, system, series, and stage are used to refer to the layers of rock that correspond to these periods of geologic time in Earths history. Geologists qualify these units as early, mid, and late when referring to time, and lower, middle, for example, the lower Jurassic Series in chronostratigraphy corresponds to the early Jurassic Epoch in geochronology. The adjectives are capitalized when the subdivision is formally recognized, and lower case when not, thus early Miocene but Early Jurassic. Geologic units from the time but different parts of the world often look different and contain different fossils. For example, in North America the Lower Cambrian is called the Waucoban series that is subdivided into zones based on succession of trilobites. In East Asia and Siberia, the unit is split into Alexian, Atdabanian. A key aspect of the work of the International Commission on Stratigraphy is to reconcile this conflicting terminology, the term Anthropocene is used informally by popular culture and a growing number of scientists to describe the current epoch in which we are living. The term was coined by Paul Crutzen and Eugene Stoermer in 2000 to describe the current time, others say that humans have not even started to leave their biggest impact on Earth, and therefore the Anthropocene hasnt even started yet. Whatever the case, the ICS has not officially approved the term, leonardo da Vinci concurred with Aristotles interpretation that fossils represented the remains of ancient life. The 11th-century Persian geologist Avicenna and the 13th-century Dominican bishop Albertus Magnus extended Aristotles explanation into a theory of a petrifying fluid. Avicenna also first proposed one of the principles underlying geologic time scales, the Chinese naturalist Shen Kuo also recognized the concept of deep time
8.
Cretaceous
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The Cretaceous is a geologic period and system that spans 79 million years from the end of the Jurassic Period 145 million years ago to the beginning of the Paleogene Period 66 Mya. It is the last period of the Mesozoic Era, the Cretaceous Period is usually abbreviated K, for its German translation Kreide. The Cretaceous was a period with a 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, during this time, new groups of mammals and birds, as well as flowering plants, appeared. The Cretaceous ended with a mass extinction, the Cretaceous–Paleogene extinction event, in which many groups, including non-avian dinosaurs, pterosaurs. The end of the Cretaceous is defined by the abrupt Cretaceous–Paleogene boundary, the name Cretaceous was derived from Latin creta, meaning chalk. The Cretaceous is divided into Early and Late Cretaceous epochs, or Lower and Upper Cretaceous series, in older literature the Cretaceous is sometimes divided into three series, Neocomian, Gallic and Senonian. A subdivision in eleven stages, all originating from European stratigraphy, is now used worldwide, in many parts of the world, alternative local subdivisions are still in use. As with other geologic periods, the rock beds of the Cretaceous are well identified. No great extinction or burst of diversity separates the Cretaceous from the Jurassic and this layer has been dated at 66.043 Ma. A140 Ma age for the Jurassic-Cretaceous boundary instead of the usually accepted 145 Ma was proposed in 2014 based on a study of Vaca Muerta Formation in Neuquén Basin. Víctor Ramos, one of the authors of the study proposing the 140 Ma boundary age sees the study as a first step toward formally changing the age in the International Union of Geological Sciences, due to the high sea level there was extensive space for such sedimentation. Because of the young age and great thickness of the system. Chalk is a type characteristic for the Cretaceous. It consists of coccoliths, microscopically small calcite skeletons of coccolithophores, the group is found in England, northern France, the low countries, northern Germany, Denmark and in the subsurface of the southern part of the North Sea. Chalk is not easily consolidated and the Chalk Group still consists of sediments in many places. The group also has other limestones and arenites, among the fossils it contains are sea urchins, belemnites, ammonites and sea reptiles such as Mosasaurus. In southern Europe, the Cretaceous is usually a marine system consisting of competent limestone beds or incompetent marls
9.
Romanization of Ukrainian
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The romanization or Latinization of Ukrainian is the representation of the Ukrainian language using Latin letters. Ukrainian is natively written in its own Ukrainian alphabet, which is based on the Cyrillic script, methods of romanization include transliteration, representing written text, and transcription, representing the spoken word. In contrast to romanization, there have been several proposals for a native Ukrainian Latin alphabet, usually based on those used by West Slavic languages. Transliteration is the representation of text using another writing system. Also called scientific transliteration, this system is most often seen in publications on Slavic languages. It is purely phonemic, meaning each character represents one unit of sound. It was codified in the 1898 Prussian Instructions for libraries, or Preußische Instruktionen and it was later adopted by the International Organization for Standardization, with minor differences, as ISO/R9. Representing all of the diacritics on computers requires Unicode, Latin-2, Latin-4. Other Slavic based romanizations occasionally seen are those based on the Slovak alphabet or the Polish alphabet, the ALA-LC Romanization Tables, published by the American Library Association and Library of Congress. Used to represent bibliographic information by US and Canadian libraries, by the British Library since 1975, the latest 1997 revision is very similar to the 1905 version. Requires Unicode for connecting diacritics—these are used in bibliographies and catalogues, British Standard 2979,1958, from BSI, is used by the Oxford University Press. A variation is used by the British Museum and British Library, a modified version is also mentioned in the Oxford Style Manual. Requires only ASCII characters if optional separators are not used, the Soviet Unions GOST, COMECONs SEV, and Ukraines Derzhstandart are government standards bodies of the former Eurasian communist countries. They published a series of systems for Ukrainian, which were replaced by ISO9,1995. ISO9 is a standard from the International Organization for Standardization and it supports most national Cyrillic alphabets in a single transliteration table. Each Cyrillic character is represented by one unique Latin character. This was originally derived from the Scholarly system in 1954, and is meant to be usable by readers of most European languages, the 1995 revision considers only graphemes and disregards phonemic differences. So, for example, г is always represented by the g, ґ is represented by g̀
10.
Romanization of Russian
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Romanization of the Russian alphabet is the process of transliterating the Russian language from the Cyrillic script into the Latin alphabet. Scientific transliteration, also known as the International Scholarly System, is a system that has used in linguistics since the 19th century. It is based on the Czech alphabet and formed the basis of the GOST, OST8483 was the first Soviet standard on romanization of Russian, introduced in 16 October 1935. This standard is an equivalent of GOST 16876-71 and was adopted as a standard of the COMECON. GOST7. 79-2000 System of Standards on Information, Librarianship and it is the official standard of both Russia and the Commonwealth of Independent States. Machine readable passports is an adoption of an ICAO stadards for travel documents and it was used in Russian passports for a short period during 2010–2013. The standard was substituted in 2013 by GOST R ISO/IEC 7501-1-2013, which does not contain romanization, ISO/R9, established in 1954 and updated in 1968, was the adoption of the scientific transliteration by the International Organization for Standardization. It covers Russian and seven other Slavic languages, ISO9,1995 is the current transliteration standard from ISO. It is based on its predecessor ISO/R9,1968, which it deprecates, for Russian, the UNGEGN, a Working Group of the United Nations, in 1987 recommended a romanization system for geographical names, which was based on the 1983 version of GOST 16876-71. It may be found in some international cartographic products, American Library Association and Library of Congress romanization tables for Slavic alphabets are used in North American libraries and in the British Library since 1975. The formal, unambiguous version of the system requires some diacritics and two-letter tie characters, British Standard 2979,1958 is the main system of the Oxford University Press, and a variation was used by the British Library to catalogue publications acquired up to 1975. The BGN/PCGN system is relatively intuitive for Anglophones to read and pronounce, the portion of the system pertaining to the Russian language was adopted by BGN in 1944 and by PCGN in 1947. In Soviet international passports, transliteration was based on French rules, in 1997, with the introduction of new Russian passports, a diacritic-free English-oriented system was established by the Ministry of Internal Affairs, but this system was also abandoned in 2010. In 2006, GOST52535. 1-2006 was adopted, which defines technical requirements and standards for Russian international passports, in 2010, the Federal Migratory Service of Russia approved Order No. 26, stating that all names in the passports issued after 2010 must be transliterated using GOST52535. 1-2006. The standard was abandoned in 2013, finally in 2013, Order No.320 of the Federal Migratory Service of Russia came into force. It states that all names in the passports must be transliterated using the ICAO system. This system differs from the GOST52535. 1-2006 system in two things, ц is transliterated into ts, ъ is transliterated into ie, Scholarly ¹ Some archaic letters are transcribed in different ways
