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82-801: Taryatu-Chulutu ( Mongolian : Тариатын чулуут , romanized :  tariatyn chuluut , "rocks of Tariat") is a volcanic field in Mongolia . It is part of a volcanic area in Central Asia in the Hangai range that may be linked to the rifting of the Lake Baikal Rift . The field itself is located within the valleys of the Chuluut and Suman rivers . Volcanic activity occurred in the Miocene , Pliocene , Pleistocene and Holocene . The Khorgo cinder cone erupted during

164-520: A cave . A lava tube is a type of lava cave formed when a low- viscosity lava flow develops a continuous and hard crust, which thickens and forms a roof above the still-flowing lava stream. Tubes form in one of two ways: either by the crusting over of lava channels , or from pāhoehoe flows where the lava is moving under the surface. Lava usually leaves the point of eruption in channels. These channels tend to stay very hot as their surroundings cool. This means they slowly develop walls around them as

246-741: A literary standard for Mongolian in whose grammar is said to be based on the Standard Mongolian of Inner Mongolia and whose pronunciation is based on the Chakhar dialect as spoken in the Plain Blue Banner . Dialectologically, however, western Mongolian dialects in Inner Mongolia are closer to Khalkha than they are to eastern Mongolian dialects in Inner Mongolia: e.g. Chakhar is closer to Khalkha than to Khorchin. Juha Janhunen (2003: 179) lists

328-432: A main lava tube. The largest of these lava tubes is 2 meters (6.6 ft) in diameter and has columnar jointing due to the large cooling surface. Other tubes have concentric and radial jointing features. The tubes are infilled due to the low slope angle of emplacement. Lunar lava tubes have been discovered and have been studied as possible human habitats, providing natural shielding from radiation. Several holes on

410-574: A much broader "Mongolian language" consisting of a Central dialect (Khalkha, Chakhar, Ordos), an Eastern dialect (Kharchin, Khorchin), a Western dialect (Oirat, Kalmyk), and a Northern dialect (consisting of two Buryat varieties). Additionally, the Language Policy in the People's Republic of China: Theory and Practice Since 1949 , states that Mongolian can be classified into four dialects: the Khalkha dialect in

492-534: A parameter called ATR ( advanced tongue root ); the groups are −ATR, +ATR, and neutral. This alignment seems to have superseded an alignment according to oral backness. However, some scholars still describe Mongolian as being characterized by a distinction between front vowels and back vowels, and the front vowel spellings 'ö' and 'ü' are still often used in the West to indicate two vowels which were historically front. The Mongolian vowel system also has rounding harmony. Length

574-530: A postalveolar or palatalized consonant will be followed by an epenthetic [i] , as in [ˈatʃĭɮ] . Stress in Mongolian is nonphonemic (does not distinguish different meanings) and thus is considered to depend entirely on syllable structure. But scholarly opinions on stress placement diverge sharply. Most native linguists, regardless of which dialect they speak, claim that stress falls on the first syllable. Between 1941 and 1975, several Western scholars proposed that

656-491: A report on sports composed in Mongolian script on stone, which is most often dated at 1224 or 1225. The Mongolian- Armenian wordlist of 55 words compiled by Kirakos of Gandzak (13th century) is the first written record of Mongolian words. From the 13th to the 15th centuries, Mongolian language texts were written in four scripts (not counting some vocabulary written in Western scripts): Uyghur Mongolian (UM) script (an adaptation of

738-578: A river, generating the Terkhiin Tsagaan Lake (although there is evidence of a former lake there, dammed by earlier eruptions). The eruption of Khorgo was probably fed from a north-northeast striking eruption fissure. Other vents in the area are Bosko, Haer, Shava, Shute, Tsagan and Zala. Augitite , potassic limburgite , pyroxene trachybasalts and trachyte - andesite are found in the Pliocene layers. Potassic basanite and limburgite are found in

820-426: A short first syllable are stressed on the second syllable. But if their first syllable is long, then the data for different acoustic parameters seems to support conflicting conclusions: intensity data often seems to indicate that the first syllable is stressed, while F0 seems to indicate that it is the second syllable that is stressed. The grammar in this article is also based primarily on Khalkha Mongolian. Unlike

902-588: A surface area of 773 square kilometres (298 sq mi) and lies at an altitude of 2,060 metres (6,760 ft). The Terkhiin Tsagaan Lake is an important food source for migratory waterfowl and has a surface area of 268 square kilometres (103 sq mi). Mongolian language Mongolian is the principal language of the Mongolic language family that originated in the Mongolian Plateau . It

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984-583: A system of vowel harmony : For historical reasons, these have been traditionally labeled as "front" vowels and "back" vowels, as /o/ and /u/ developed from /ø/ and /y/, while /ɔ/ and /ʊ/ developed from /o/ and /u/ in Middle Mongolian. Indeed, in Mongolian romanizations , the vowels /o/ and /u/ are often conventionally rendered as ⟨ö⟩ and ⟨ü⟩ , while the vowels /ɔ/ and /ʊ/ are expressed as ⟨o⟩ and ⟨u⟩ . However, for modern Mongolian phonology, it

1066-404: A variety of stalactite forms generally known as lavacicles , which can be of the splash, "shark tooth", or tubular varieties. Lavacicles are the most common of lava tube speleothems. Drip stalagmites may form under tubular lava stalactites, and the latter may grade into a form known as a tubular lava helictite . A runner is a bead of lava that is extruded from a small opening and then runs down

1148-459: A wall. Lava tubes may also contain mineral deposits that most commonly take the form of crusts or small crystals , and less commonly, as stalactites and stalagmites. Some stalagmites may contain a central conduit and are interpreted as hornitos extruded from the tube floor. Lava tubes can be up to 14–15 metres (46–49 ft) wide, though are often narrower, and run anywhere from 1–15 metres (3 ft 3 in – 49 ft 3 in) below

1230-508: Is Classical Mongolian , which is dated from the 17th to the 19th century. This is a written language with a high degree of standardization in orthography and syntax that sets it quite apart from the subsequent Modern Mongolian. The most notable documents in this language are the Mongolian Kangyur and Tengyur as well as several chronicles. In 1686, the Soyombo alphabet ( Buddhist texts )

1312-433: Is determined according to phonotactic requirements. The following table lists the consonants of Khalkha Mongolian. The consonants enclosed in parentheses occur only in loanwords. The occurrence of palatalized consonant phonemes, except /tʃ/ /tʃʰ/ /ʃ/ /j/ , is restricted to words with [−ATR] vowels. A rare feature among the world's languages, Mongolian has neither a voiced lateral approximant, such as [l] , nor

1394-409: Is ellipsis . The rules governing the morphology of Mongolian case endings are intricate, and so the rules given below are only indicative. In many situations, further (more general) rules must also be taken into account in order to produce the correct form: these include the presence of an unstable nasal or unstable velar, as well as the rules governing when a penultimate vowel should be deleted from

1476-466: Is CVVCCC, where the last C is a word-final suffix. A single short vowel rarely appears in syllable-final position . If a word was monosyllabic historically, *CV has become CVV. In native words, the following consonants do not occur word-initially: /w̜/ , /ɮ/ , /r/ , /w̜ʲ/ , /ɮʲ/ , /rʲ/ , /tʰʲ/ , and /tʲ/ . [ŋ] is restricted to codas (else it becomes [n] ), and /p/ and /pʲ/ do not occur in codas for historical reasons. For two-consonant clusters,

1558-438: Is a +ATR vowel, then every vowel of the word must be either /i/ or a +ATR vowel. In the case of suffixes, which must change their vowels to conform to different words, two patterns predominate. Some suffixes contain an archiphoneme /A/ that can be realized as /a, ɔ, e, o/ ; e.g. Other suffixes can occur in /U/ being realized as /ʊ, u/ , in which case all −ATR vowels lead to /ʊ/ and all +ATR vowels lead to /u/ ; e.g. If

1640-485: Is based primarily on the Khalkha dialect as spoken in Ulaanbaatar , Mongolia's capital. The phonologies of other varieties such as Ordos, Khorchin, and even Chakhar, differ considerably. This section discusses the phonology of Khalkha Mongolian with subsections on Vowels, Consonants, Phonotactics and Stress. The standard language has seven monophthong vowel phonemes. They are aligned into three vowel harmony groups by

1722-418: Is deep. Xenoliths are also found in the Pliocene layers and are composed of peridotite , sanidine and spinel - lherzolite . Pleistocene layers contain ultramafic xenoliths, with the youngest Holocene flows containing the largest amounts. Shavaryn-Tsaram is particularly well known as a source of xenoliths. In the 1970s and 1980s this volcano was prospected and mined for garnets . Volcanic activity in

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1804-661: Is exposed in river terraces of the Chulutu river. The 130–200 metres (430–660 ft) terraces formed during the Miocene and the 100–120 metres (330–390 ft) terraces in the Pliocene. Lava sheets in the lower two thirds of the Pliocene layers are thicker than the upper lava flows. The 60 metres (200 ft) terrace of the Chulutu river and the 40–60 metres (130–200 ft) terraces in the Taryatu river are of Pleistocene age. This sequence reaches thicknesses of 40–90 metres (130–300 ft). In

1886-423: Is found directly southwest of Khorog/Khorgo. The first volcano has a crater lip in its side, while the other two volcanoes are partly buried in lava flows. These lava flows show sag structures formed by the collapse of lava tubes . Khorog/Khorgo has a dimension of 1,200 metres (3,900 ft) base diameter and a height of 120 metres (390 ft). On top of the cone sits a 180 metres (590 ft) wide crater. Among

1968-566: Is impeded by the fact that existing data for the major varieties is not easily arrangeable according to a common set of linguistic criteria. Such data might account for the historical development of the Mongolian dialect continuum , as well as for its sociolinguistic qualities. Though phonological and lexical studies are comparatively well developed, the basis has yet to be laid for a comparative morphosyntactic study, for example between such highly diverse varieties as Khalkha and Khorchin. In Juha Janhunen's book titled Mongolian , he groups

2050-410: Is more appropriate to instead characterize the two vowel-harmony groups by the dimension of tongue root position. There is also one neutral vowel, /i/ , not belonging to either group. All the vowels in a non compound word, including all its suffixes, must belong to the same group. If the first vowel is −ATR, then every vowel of the word must be either /i/ or a −ATR vowel. Likewise, if the first vowel

2132-403: Is not clear if the lava flow and the pyroclastic deposit were formed by the same volcanic eruption. In the western part of the depression, six Holocene cinder cones are found which have generated lava flows. These lava flows have thicknesses of 3–5 metres (9.8–16.4 ft). These cones include Khorog and Dzan Tologai. An arcuate chain of volcanoes named Odnobokii, Listvennichnyi, and Sosnovyi

2214-427: Is not in line with the current international standard. Mongolian is a language with vowel harmony and a complex syllabic structure compared to other Mongolic languages, allowing clusters of up to three consonants syllable-finally. It is a typical agglutinative language that relies on suffix chains in the verbal and nominal domains. While there is a basic word order, subject–object–verb , ordering among noun phrases

2296-1261: Is phonemic for vowels, and except short [e], which has merged into short [i], at least in Ulaanbaatar dialect, each of the other six phonemes occurs both short and long. Phonetically, short /o/ has become centralised to the central vowel [ɵ] . In the following table, the seven vowel phonemes, with their length variants, are arranged and described phonetically. The vowels in the Mongolian Cyrillic alphabet are: Khalkha also has four diphthongs : historically /ui, ʊi, ɔi, ai/ but are pronounced more like [ʉe̯, ʊe̯, ɞe̯, æe̯] ; e.g. ой in нохой ( nohoi ) [nɔ̙ˈχɞe̯] 'dog', ай in далай ( dalai ) [taˈɮæe̯] sea', уй in уйлах ( uilah ) [ˈʊe̯ɮɐχ] 'to cry', үй in үйлдвэр ( üildver ) [ˈʉe̯ɮtw̜ɘr] 'factory', эй in хэрэгтэй ( heregtei ) [çiɾɪxˈtʰe] 'necessary'. There are three additional rising diphthongs /ia/ (иа), /ʊa/ (уа) /ei/ (эй); e.g. иа in амиараа ( amiaraa ) [aˈmʲæɾa] 'individually', уа in хуаран ( huaran ) [ˈχʷaɾɐɴ] 'barracks'. This table below lists vowel allophones (short vowels allophones in non-initial positions are used interchangeably with schwa): Mongolian divides vowels into three groups in

2378-458: Is relatively free, as grammatical roles are indicated by a system of about eight grammatical cases . There are five voices . Verbs are marked for voice, aspect , tense and epistemic modality / evidentiality . In sentence linking, a special role is played by converbs . Modern Mongolian evolved from Middle Mongol , the language spoken in the Mongol Empire of the 13th and 14th centuries. In

2460-423: Is spoken by ethnic Mongols and other closely related Mongolic peoples who are native to modern Mongolia and surrounding parts of East and North Asia . Mongolian is the official language of Mongolia and Inner Mongolia and a recognized language of Xinjiang and Qinghai . The number of speakers across all its dialects may be 5–6 million, including the vast majority of the residents of Mongolia and many of

2542-400: Is usually another lava tube leading back to the eruption point. Called pāhoehoe flows, these areas of surface-moving lava cool, forming either a smooth or rough, ropy surface. The lava continues to flow this way until it begins to block its source. At this point, the subsurface lava is still hot enough to break out at a point, and from this point the lava begins as a new "source". Lava flows from

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2624-402: Is word-final, it gets stressed anyway. In cases where there is only one phonemic short word-initial syllable, even this syllable can get the stress: More recently, the most extensive collection of phonetic data so far in Mongolian studies has been applied to a partial account of stress placement in the closely related Chakhar dialect. The conclusion is drawn that di- and trisyllabic words with

2706-516: The Altaic language family and contrasted with the Mainland Southeast Asia linguistic area . However, instead of a common genetic origin, Clauson, Doerfer, and Shcherbak proposed that Turkic, Mongolic and Tungusic languages form a language Sprachbund , rather than common origin. Mongolian literature is well attested in written form from the 13th century but has earlier Mongolic precursors in

2788-501: The Kalmyk variety ) and Buryat, both of which are spoken in Russia, Mongolia, and China; and Ordos , spoken around Inner Mongolia's Ordos City . The influential classification of Sanžeev (1953) proposed a "Mongolian language" consisting of just the three dialects Khalkha, Chakhar, and Ordos, with Buryat and Oirat judged to be independent languages. On the other hand, Luvsanvandan (1959) proposed

2870-642: The Shuluun Huh/Zhènglán Banner , and is written in the traditional Mongolian script . The number of Mongolian speakers in China is still larger than in the state of Mongolia, where the majority of Mongolians in China speak one of the Khorchin dialects , or rather more than two million of them speak the Khorchin dialect itself as their mother tongue, so that the Khorchin dialect group has about as many speakers as

2952-627: The Uyghur alphabet), 'Phags-pa script (Ph) (used in decrees), Chinese (SM) ( The Secret History of the Mongols ), and Arabic (AM) (used in dictionaries). While they are the earliest texts available, these texts have come to be called " Middle Mongol " in scholarly practice. The documents in UM script show some distinct linguistic characteristics and are therefore often distinguished by terming their language "Preclassical Mongolian". The Yuan dynasty referred to

3034-501: The ethnic Mongol residents of the Inner Mongolia of China . In Mongolia , Khalkha Mongolian is predominant, and is currently written in both Cyrillic and the traditional Mongolian script . In Inner Mongolia, it is dialectally more diverse and written in the traditional Mongolian script. However, Mongols in both countries often use the Latin script for convenience on the Internet. In

3116-553: The syllable 's position in the word. In word-initial syllables, there is a phonemic contrast in vowel length . A long vowel has about 208% the length of a short vowel. In word-medial and word-final syllables, formerly long vowels are now only 127% as long as short vowels in initial syllables, but they are still distinct from initial-syllable short vowels. Short vowels in noninitial syllables differ from short vowels in initial syllables by being only 71% as long and by being centralized in articulation. As they are nonphonemic, their position

3198-726: The Holocene and lava flows from it formed a lava dam generating Terkhiin Tsagaan Nuur lake. The volcanic field lies in the Taryatu depression, on the northern slope of the Hangai range. There, the field spans the river valleys of the Chuluut River, its tributary Gichigin and the Suman River rivers. The field is sometimes named Tariat volcanic field after the town of Tariat . Rivers frequently run in canyons bordered by lava plains. Tectonically,

3280-538: The Inner Mongolia since September, which caused widespread protests among ethnic Mongol communities. These protests were quickly suppressed by the Chinese government. Mandarin has been deemed the only language of instruction for all subjects as of September 2023. Mongolian belongs to the Mongolic languages . The delimitation of the Mongolian language within Mongolic is a much disputed theoretical problem, one whose resolution

3362-512: The Khalkha dialect group in the State of Mongolia. Nevertheless, the Chakhar dialect, which today has only about 100,000 native speakers and belongs to the Khalkha dialect group, is the basis of standard Mongolian in China. The characteristic differences in the pronunciation of the two standard varieties include the umlauts in Inner Mongolia and the palatalized consonants in Mongolia (see below) as well as

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3444-601: The Miocene-Pliocene a major lava plateau was formed on the eastern end of the Taryat depression, with a surface area of 24 by 15 kilometres (14.9 mi × 9.3 mi). The depression itself however does not appear to contain lavas from this plateau. Between 0.75 and 0.36 mya the Taryat–Chulutyn lava river was erupted from several Pleistocene-Holocene centres and grew to a length of c. 100 kilometres (62 mi). Within

3526-812: The Mongolian language in Chinese as "Guoyu" ( Chinese : 國語 ), which means "National language", a term also used by other non-Han dynasties to refer to their languages such as the Manchu language during the Qing dynasty , the Jurchen language during the Jin dynasty (1115–1234) , the Khitan language during the Liao dynasty , and the Xianbei language during the Northern Wei period. The next distinct period

3608-497: The Mongolic language family into four distinct linguistic branches: The Common Mongolic branch is grouped in the following way: There is no disagreement that the Khalkha dialect of the Mongolian state is Mongolian. However, the status of certain varieties in the Common Mongolic group—whether they are languages distinct from Mongolian or just dialects of it—is disputed. There are at least three such varieties: Oirat (including

3690-473: The Pleistocene layers. Holocene layers contain augitite, leucite basanite, potassic hawaiite and leucite tephrite . Horgo/Khorgo is constructed from phonolitic tephrite and its lavas range alkali basalt -basanite. There is a clear trend in increasing K 2 O and alkali content during the Pleistocene and the Holocene, indicating together with the xenolith content that the origin of these recent basalts

3772-426: The accusative, while it must take the nominative if it is indefinite . In addition to case, a number of postpositions exist that usually govern the genitive, dative-locative, comitative and privative cases, including a marked form of the nominative (which can itself then take further case forms). There is also a possible attributive case (when a noun is used attributively ), which is unmarked in most nouns but takes

3854-529: The activity of all three centres. Tsagan may be younger than Khorgo. Khorgo volcano is 530 kilometres (330 mi) west of Ulaanbataar . It is part of the Khorgo-Terkhiin Tsagaan Nuur National Park , which was established in 1965 and is a major tourism destination. Most precipitation in the area falls during summer. The national park ( 48°8′N 99°38′E  /  48.133°N 99.633°E  / 48.133; 99.633 ) has

3936-514: The central problem remains the question of how to classify Chakhar, Khalkha, and Khorchin in relation to each other and in relation to Buryat and Oirat. The split of [tʃ] into [tʃ] before *i and [ts] before all other reconstructed vowels, which is found in Mongolia but not in Inner Mongolia, is often cited as a fundamental distinction, for example Proto-Mongolic *tʃil , Khalkha /tʃiɮ/ , Chakhar /tʃil/ 'year' versus Proto-Mongolic *tʃøhelen , Khalkha /tsoːɮəŋ/ , Chakhar /tʃoːləŋ/ 'few'. On

4018-485: The components of the cone are scoria and large blocks of basalt. The cone is breached at the location of a lava tube. Its eruption also generated an eastward pointing ash deposit with thicknesses of 3–5 metres (9.8–16.4 ft). It also contains lapilli and lava bombs with dimensions of 0.5–1 metre (1 ft 8 in – 3 ft 3 in). Very little soil is developed on the Khorgo lavas. Lavas from this cone dammed

4100-480: The depression it has a width of 6 kilometres (3.7 mi), a thickness of 90 metres (300 ft) and a length of c. 50 kilometres (31 mi). Shavaryn-Tsaram forms a breccia and pyroclastic deposit accompanied by a lava flow following the valley bottom, 10 kilometres (6.2 mi) south of the Suman river. The pyroclastic deposit covers a surface area of 600 by 800 metres (2,000 ft × 2,600 ft). It

4182-425: The discussion of grammar to follow, the variety of Mongolian treated is the standard written Khalkha formalized in the writing conventions and in grammar as taught in schools, but much of it is also valid for vernacular (spoken) Khalkha and other Mongolian dialects, especially Chakhar Mongolian . Some classify several other Mongolic languages like Buryat and Oirat as varieties of Mongolian, but this classification

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4264-412: The examples given above, the words are phonetically [ˈxɔjɔ̆r] , [ˈatʃĭɮ] , and [ˈsaːrmăɢ] . The phonetic form of the epenthetic vowel follows from vowel harmony triggered by the vowel in the preceding syllable. Usually it is a centralized version of the same sound, with the following exceptions: preceding /u/ produces [e] ; /i/ will be ignored if there is a nonneutral vowel earlier in the word; and

4346-593: The field is located within the Tarvagatay terrane which formed 3,000-200 mya ago and between 1,000 and 250 mya was accreted into the Central Asian Orogenic Belt. This terrane is formed by amphibolite , gneiss , migmatite and schist . An anorthosite pluton has yielded ages of 3,050 mya and is the oldest age from this terrane. Following stabilization of the whole Hangai region in the Paleozoic , only in

4428-411: The field ranges from Pliocene to Holocene, commencing about 8 mya ago. The Shavaryn-Tsaram volcano has an age of 1.2 mya. The Tariat valley flows were emplaced between 240,000 and 60,000 years ago. Seismic tomography has identified traces of a former magmatic intrusion under the volcanic field. The total volume of lava is less than 300 cubic kilometres (72 cu mi). The Khorgo/Horgo cinder cones

4510-612: The following Mongol dialects, most of which are spoken in Inner Mongolia . There are two standard varieties of Mongolian. Standard Mongolian in the state of Mongolia is based on the northern Khalkha Mongolian dialects, which include the dialect of Ulaanbaatar , and is written in the Mongolian Cyrillic script . Standard Mongolian in Inner Mongolia is based on the Chakhar Mongolian of the Khalkha dialect group, spoken in

4592-444: The following restrictions obtain: Clusters that do not conform to these restrictions will be broken up by an epenthetic nonphonemic vowel in a syllabification that takes place from right to left. For instance, hoyor 'two', azhil 'work', and saarmag 'neutral' are, phonemically, /xɔjr/ , /atʃɮ/ , and /saːrmɡ/ respectively. In such cases, an epenthetic vowel is inserted to prevent disallowed consonant clusters. Thus, in

4674-583: The independent words derived using verbal suffixes can roughly be divided into three classes: final verbs , which can only be used sentence-finally, i.e. ‑ na (mainly future or generic statements) or ‑ ö (second person imperative); participles (often called "verbal nouns"), which can be used clause-finally or attributively, i.e. ‑ san ( perfect - past ) or ‑ maar 'want to'; and converbs , which can link clauses or function adverbially , i.e. ‑ zh (qualifies for any adverbial function or neutrally connects two sentences ) or ‑ tal (the action of

4756-413: The language is spoken by roughly half of the country's 5.8 million ethnic Mongols (2005 estimate) However, the exact number of Mongolian speakers in China is unknown, as there is no data available on the language proficiency of that country's citizens. The use of Mongolian in Inner Mongolia has witnessed periods of decline and revival over the last few hundred years. The language experienced a decline during

4838-511: The late Cenozoic did tectonic activity recommence. Volcanism in this field appears to be related to volcanism which is widespread in this part of Asia . Localized asthenosphere upwellings may be responsible for these volcanic events at Hangai and other volcanic centres around Lake Baikal . Other theories for the Hangai postulate a mantle plume or the removal of part of the lithosphere by asthenospheric currents. Magnetotelluric analysis has found evidence of mantle upwelling. The volcanism

4920-405: The late Qing period, a revival between 1947 and 1965, a second decline between 1966 and 1976, a second revival between 1977 and 1992, and a third decline between 1995 and 2012. However, in spite of the decline of the Mongolian language in some of Inner Mongolia's urban areas and educational spheres, the ethnic identity of the urbanized Chinese-speaking Mongols is most likely going to survive due to

5002-418: The leftmost heavy syllable gets the stress. Yet other positions were taken in works published between 1835 and 1915. Walker (1997) proposes that stress falls on the rightmost heavy syllable unless this syllable is word-final: A "heavy syllable" is defined as one that is at least the length of a full vowel; short word-initial syllables are thereby excluded. If a word is bisyllabic and the only heavy syllable

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5084-565: The literature of the Khitan and other Xianbei peoples. The Bugut inscription dated to 584 CE and the Inscription of Hüis Tolgoi dated to 604–620 CE appear to be the oldest substantial Mongolic or Para-Mongolic texts discovered. Writers such as Owen Lattimore referred to Mongolian as "the Mongol language". The earliest surviving Mongolian text may be the Stele of Yisüngge  [ ru ] ,

5166-622: The lunar surface, including one in the Marius Hills region, have been observed with angled satellite imagery to lead into voids wider than the holes themselves. These are considered as possible collapses into lunar lava tubes. Martian lava tubes are associated with innumerable lava flows and lava channels on the flanks of Olympus Mons . Partially collapsed lava tubes are visible as chains of pit craters, and broad lava fans formed by lava emerging from intact, subsurface tubes are also common. Evidence of Martian lava tubes has also been observed on

5248-421: The main clause takes place until the action expressed by the suffixed verb begins). Roughly speaking, Mongolian has between seven and nine cases : nominative ( unmarked ), genitive , dative - locative , accusative , ablative , instrumental , comitative , privative and directive , though the final two are not always considered part of the case paradigm. If a direct object is definite , it must take

5330-635: The middle, the Horcin-Haracin dialect in the East, Oriat-Hilimag in the west, and Bargu–Buriyad in the north. Some Western scholars propose that the relatively well researched Ordos variety is an independent language due to its conservative syllable structure and phoneme inventory. While the placement of a variety like Alasha , which is under the cultural influence of Inner Mongolia but historically tied to Oirat, and of other border varieties like Darkhad would very likely remain problematic in any classification,

5412-491: The only vowel in the word stem is /i/ , the suffixes will use the +ATR suffix forms. Mongolian also has rounding harmony, which does not apply to close vowels. If a stem contains /o/ (or /ɔ/ ), a suffix that is specified for an open vowel will have [o] (or [ɔ] , respectively) as well. However, this process is blocked by the presence of /u/ (or /ʊ/ ) and /ei/ ; e.g. /ɔr-ɮɔ/ 'came in', but /ɔr-ʊɮ-ɮa/ 'inserted'. The pronunciation of long and short vowels depends on

5494-608: The other hand, the split between the past tense verbal suffixes - /sŋ/ in the Central varieties v. - /dʒɛː/ in the Eastern varieties is usually seen as a merely stochastic difference. In Inner Mongolia, official language policy divides the Mongolian language into three dialects: Standard Mongolian of Inner Mongolia , Oirat, and Barghu-Buryat. The Standard Mongolian of Inner Mongolia is said to consist of Chakhar, Ordos, Baarin , Khorchin, Kharchin, and Alasha. The authorities have synthesized

5576-448: The phonology, most of what is said about morphology and syntax also holds true for Chakhar, while Khorchin is somewhat more diverse. Modern Mongolian is an agglutinative —almost exclusively suffixing—language, with the only exception being reduplication. Mongolian also does not have gendered nouns, or definite articles like "the". Most of the suffixes consist of a single morpheme . There are many derivational morphemes. For example,

5658-542: The preferential policies for minorities in education, healthcare, family planning, school admissions, the hiring and promotion, the financing and taxation of businesses, and regional infrastructural support given to ethnic minorities in China. In 2020, the Chinese government required three subjects—language and literature, politics, and history—to be taught in Mandarin in Mongolian-language primary and secondary schools in

5740-597: The presence of urban ethnic communities. The multilingual situation in Inner Mongolia does not appear to obstruct efforts by ethnic Mongols to preserve their language. Although an unknown number of Mongols in China, such as the Tumets, may have completely or partially lost the ability to speak their language, they are still registered as ethnic Mongols and continue to identify themselves as ethnic Mongols. The children of inter-ethnic Mongol-Chinese marriages also claim to be and are registered as ethnic Mongols so they can benefit from

5822-404: The previous source to this breakout point as the surrounding lava of the pāhoehoe flow cools. This forms an underground channel that becomes a lava tube. A broad lava-flow field often consists of a main lava tube and a series of smaller tubes that supply lava to the front of one or more separate flows. When the supply of lava stops at the end of an eruption or lava is diverted elsewhere, lava in

5904-596: The splitting of the Middle Mongol affricates * ʧ ( ᠴ č ) and * ʤ ( ᠵ ǰ ) into ʦ ( ц c ) and ʣ ( з z ) versus ʧ ( ч č ) and ʤ ( ж ž ) in Mongolia: Aside from these differences in pronunciation, there are also differences in vocabulary and language use: in the state of Mongolia more loanwords from Russian are being used, while in Inner Mongolia more loanwords from Chinese have been adopted. The following description

5986-406: The stem with certain case endings (e.g. цэрэг  ( tsereg ) → цэргийн  ( tsergiin )). The additional morphological rules specific to loanwords are not covered. Lava tube A lava tube , or pyroduct , is a natural conduit formed by flowing lava from a volcanic vent that moves beneath the hardened surface of a lava flow. If lava in the tube empties, it will leave

6068-430: The suffix ‑ н  (‑ n ) when the stem has an unstable nasal. Nouns can also take a reflexive-possessive suffix , indicating that the marked noun is possessed by the subject of the sentence: bi najz-aa avar-san I friend- reflexive-possessive save- perfect "I saved my friend". However, there are also somewhat noun-like adjectives to which case suffixes seemingly cannot be attached directly unless there

6150-600: The surface. Lava tubes can also be extremely long; one tube from the Mauna Loa 1859 flow enters the ocean about 50 kilometers (31 mi) from its eruption point, and the Cueva del Viento–Sobrado system on Teide , Tenerife island, is over 18 kilometers (11 mi) long, due to extensive braided maze areas at the upper zones of the system. A lava tube system in Kiama , Australia , consists of over 20 tubes, many of which are breakouts of

6232-414: The surrounding lava cools and/or as the channel melts its way deeper. These channels can get deep enough to crust over, forming an insulating tube that keeps the lava molten and serves as a conduit for the flowing lava. These types of lava tubes tend to be closer to the lava eruption point. Farther away from the eruption point, lava can flow in an unchanneled, fan-like manner as it leaves its source, which

6314-456: The transition, a major shift in the vowel-harmony paradigm occurred, long vowels developed, the case system changed slightly, and the verbal system was restructured. Mongolian is related to the extinct Khitan language . It was believed that Mongolian was related to Turkic , Tungusic , Korean and Japonic languages but this view is now seen as obsolete by a majority of (but not all) comparative linguists. These languages have been grouped under

6396-458: The tube system drains downslope and leaves partially empty caves . Such drained tubes commonly exhibit step marks on their walls that mark the various depths at which the lava flowed, known as flow ledges or flow lines depending on how prominently they protrude from the walls. Lava tubes generally have pāhoehoe floors, although this may often be covered in breakdown from the ceiling. A variety of speleothems may be found in lava tubes including

6478-424: The voiceless velar plosive [k] ; instead, it has a voiced alveolar lateral fricative , /ɮ/ , which is often realized as voiceless [ɬ] . In word-final position, /n/ (if not followed by a vowel in historical forms) is realized as [ŋ] . Aspirated consonants are preaspirated in medial and word-final contexts, devoicing preceding consonants and vowels. Devoiced short vowels are often deleted. The maximal syllable

6560-547: The word baiguullagiinh consists of the root bai 'to be', an epenthetic ‑ g ‑, the causative ‑ uul ‑ (hence 'to found'), the derivative suffix ‑ laga that forms nouns created by the action (like - ation in organisation ) and the complex suffix ‑ iinh denoting something that belongs to the modified word (‑ iin would be genitive ). Nominal compounds are quite frequent. Some derivational verbal suffixes are rather productive , e.g. yarih 'to speak', yarilc 'to speak with each other'. Formally,

6642-492: Was considered to be about 4 ka old, C dating on organic material in its sediments has indicated ages of 8 ka. The Global Volcanism Program indicates a date of 2980 BCE ± 150 years. The most recent research indicates a date of 7,200 years ago. Some geologists have correlated the activity of Paektusan , Udokan Plateau and Wudalianchi volcanoes elsewhere in Asia and have presumed that common geologic events did influence

6724-417: Was created, giving distinctive evidence on early classical Mongolian phonological peculiarities. Mongolian is the official national language of Mongolia, where it is spoken (but not always written) by nearly 3.6 million people (2014 estimate), and the official provincial language (both spoken and written forms) of Inner Mongolia, where there are at least 4.1 million ethnic Mongols. Across the whole of China,

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