Beichuan Qiang Autonomous County ( simplified Chinese : 北川羌族自治县 ; traditional Chinese : 北川羌族自治縣 ; pinyin : Běichuān Qiāngzú Zìzhì Xiàn ; Qiang : Juda Rrmea nyujugvexueaji xae) is a county under the jurisdiction of Mianyang City in northern Sichuan province, China. It is located in an ethnically diverse mountainous region of Sichuan. Its Chinese name literally means "North" (bei) "River" (chuan). Its new county seat is located at Yongchang after the 2008 Sichuan earthquake .
61-580: Beichuan County has an area of 3,084 square kilometres (1,191 sq mi). The county varies in elevation from 540 to 4,769 meters in height. The county's major rivers, which include the Tongkou River [ zh ] , the Anchang River [ zh ] , and the Pingtong River ( 平通河 ; Píngtōng Hé ) belong to the larger Fu River watershed. The first administrative county of Beichuan
122-580: A Sino-Tibetan language as their main native language. Other languages of the family are spoken in the Himalayas , the Southeast Asian Massif , and the eastern edge of the Tibetan Plateau . Most of these have small speech communities in remote mountain areas, and as such are poorly documented. Several low-level subgroups have been securely reconstructed , but reconstruction of a proto-language for
183-476: A detailed classification, with six top-level divisions: Shafer was sceptical of the inclusion of Daic, but after meeting Maspero in Paris decided to retain it pending a definitive resolution of the question. James Matisoff abandoned Benedict's Tibeto-Karen hypothesis: Some more-recent Western scholars, such as Bradley (1997) and La Polla (2003), have retained Matisoff's two primary branches, though differing in
244-562: A family whose diversity has been compared with the Romance languages . Diversity is greater in the rugged terrain of southeast China than in the North China Plain . Burmese is the national language of Myanmar , and the first language of some 33 million people. Burmese speakers first entered the northern Irrawaddy basin from what is now western Yunnan in the early ninth century, in conjunction with an invasion by Nanzhao that shattered
305-482: A geographic grouping, as Matisoff does, van Driem leaves them unclassified. He has proposed several hypotheses, including the reclassification of Chinese to a Sino-Bodic subgroup: Van Driem points to two main pieces of evidence establishing a special relationship between Sinitic and Bodic and thus placing Chinese within the Tibeto-Burman family. First, there are some parallels between the morphology of Old Chinese and
366-402: A group with two branches, Chinese-Siamese and Tibeto-Burman. August Conrady called this group Indo-Chinese in his influential 1896 classification, though he had doubts about Karen. Conrady's terminology was widely used, but there was uncertainty regarding his exclusion of Vietnamese. Franz Nikolaus Finck in 1909 placed Karen as a third branch of Chinese-Siamese. Jean Przyluski introduced
427-555: A huge body of literature from the first millennium BC. However, the Chinese script is logographic and does not represent sounds systematically; it is therefore difficult to reconstruct the phonology of the language from the written records. Scholars have sought to reconstruct the phonology of Old Chinese by comparing the obscure descriptions of the sounds of Middle Chinese in medieval dictionaries with phonetic elements in Chinese characters and
488-517: A hypothesis called Sino-Kiranti . The proposal takes two forms: that Sinitic and Kiranti are themselves a valid node or that the two are not demonstrably close so that Sino-Tibetan has three primary branches: George van Driem , like Shafer, rejects a primary split between Chinese and the rest, suggesting that Chinese owes its traditional privileged place in Sino-Tibetan to historical, typological, and cultural, rather than linguistic, criteria. He calls
549-402: A population of 235,304 in 2017, of which 61.5% are Han Chinese , 36.6% of which are Qiang people (a Sino-Tibetan people related to Tibetans ), 1.5% are Tibetans, 0.2% are Hui , and the remaining 0.2% belong to various other ethnic groups. The county is home to 34 standard schools, of which, 24 are primary schools , 9 junior high schools , and 1 compulsory school . Beichuan also houses
610-425: A prototypical example of the isolating morphological type, southern Chinese languages express this trait far more strongly than northern Chinese languages do. Initial consonant alternations related to transitivity are pervasive in Sino-Tibetan; while devoicing (or aspiration) of the initial is associated with a transitive/ causative verb, voicing is linked to its intransitive/ anticausative counterpart. This
671-544: A provisional classification of the remaining languages: Following that, because they propose that the three best-known branches may be much closer related to each other than they are to "minor" Sino-Tibetan languages, Blench and Post argue that "Sino-Tibetan" or "Tibeto-Burman" are inappropriate names for a family whose earliest divergences led to different languages altogether. They support the proposed name "Trans-Himalayan". A team of researchers led by Pan Wuyun and Jin Li proposed
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#1733085313271732-481: A separate Tibeto-Burman subgroup, Hill (2014) finds that Burmese has distinct correspondences for Old Chinese rhymes -ay : *-aj and -i : *-əj, and hence argues that the development *ə > *a occurred independently in Tibetan and Burmese. The descriptions of non-literary languages used by Shafer and Benedict were often produced by missionaries and colonial administrators of varying linguistic skills. Most of
793-412: A six-vowel system originally suggested by Nicholas Bodman . Similarly, Karlgren's *l has been recast as *r, with a different initial interpreted as *l, matching Tibeto-Burman cognates, but also supported by Chinese transcriptions of foreign names. A growing number of scholars believe that Old Chinese did not use tones and that the tones of Middle Chinese developed from final consonants. One of these, *-s,
854-526: A special relationship between Chinese and Bodic. Van Driem has also proposed a "fallen leaves" model that lists dozens of well-established low-level groups while remaining agnostic about intermediate groupings of these. In the most recent version (van Driem 2014), 42 groups are identified (with individual languages highlighted in italics ): He also suggested (van Driem 2007) that the Sino-Tibetan language family be renamed "Trans-Himalayan", which he considers to be more neutral. Orlandi (2021) also considers
915-508: A survey in the 1937 Chinese Yearbook , Li Fang-Kuei described the family as consisting of four branches: Tai and Miao–Yao were included because they shared isolating typology, tone systems and some vocabulary with Chinese. At the time, tone was considered so fundamental to language that tonal typology could be used as the basis for classification. In the Western scholarly community, these languages are no longer included in Sino-Tibetan, with
976-461: A two-way distinction on initial consonants based on voicing, with aspiration conditioned by pre-initial consonants that had been retained in Tibetic but lost in many other languages. Thus, Benedict reconstructed the following initials: Although the initial consonants of cognates tend to have the same place and manner of articulation , voicing and aspiration are often unpredictable. This irregularity
1037-518: Is a family of more than 400 languages, second only to Indo-European in number of native speakers. Around 1.4 billion people speak a Sino-Tibetan language. The vast majority of these are the 1.3 billion native speakers of Sinitic languages . Other Sino-Tibetan languages with large numbers of speakers include Burmese (33 million) and the Tibetic languages (6 million). Four United Nations member states ( China , Singapore , Myanmar , and Bhutan ) have
1098-470: Is believed to be a suffix, with cognates in other Sino-Tibetan languages. Tibetic has extensive written records from the adoption of writing by the Tibetan Empire in the mid-7th century. The earliest records of Burmese (such as the 12th-century Myazedi inscription ) are more limited, but later an extensive literature developed. Both languages are recorded in alphabetic scripts ultimately derived from
1159-747: Is disagreement over whether to include the entire Kra–Dai family or just Kam–Tai (Zhuang–Dong excludes the Kra languages ), because the Chinese cognates that form the basis of the putative relationship are not found in all branches of the family and have not been reconstructed for the family as a whole. In addition, Kam–Tai itself no longer appears to be a valid node within Kra–Dai. Benedict overtly excluded Vietnamese (placing it in Mon–Khmer) as well as Hmong–Mien and Kra–Dai (placing them in Austro-Tai ). He otherwise retained
1220-422: Is no consensus regarding the date and location of their origin. During the 18th century, several scholars noticed parallels between Tibetan and Burmese, both languages with extensive literary traditions. Early in the following century, Brian Houghton Hodgson and others noted that many non-literary languages of the highlands of northeast India and Southeast Asia were also related to these. The name "Tibeto-Burman"
1281-481: The Beichuan High School campus, where more than 1,000 students lost their lives after two main buildings collapsed. Beichuan's Party and government building also collapsed, and Yang Zesen, Beichuan's vice mayor then was among the victims. 80% of the county's buildings are said to have collapsed. The county town, which prior to the earthquake had a population of 20,000, is to be made into a memorial park , as
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#17330853132711342-936: The Brahmi script of Ancient India. Most comparative work has used the conservative written forms of these languages, following the dictionaries of Jäschke (Tibetan) and Judson (Burmese), though both contain entries from a wide range of periods. There are also extensive records in Tangut , the language of the Western Xia (1038–1227). Tangut is recorded in a Chinese-inspired logographic script, whose interpretation presents many difficulties, even though multilingual dictionaries have been found. Gong Hwang-cherng has compared Old Chinese, Tibetic, Burmese, and Tangut to establish sound correspondences between those languages. He found that Tibetic and Burmese /a/ correspond to two Old Chinese vowels, *a and *ə. While this has been considered evidence for
1403-576: The Karen languages , spoken by 4 million people in the hill country along the Myanmar–Thailand border, with the greatest diversity in the Karen Hills , which are believed to be the homeland of the group. The highlands stretching from northeast India to northern Myanmar contain over 100 highly diverse Sino-Tibetan languages. Other Sino-Tibetan languages are found along the southern slopes of the Himalayas and
1464-605: The Lolo-Burmese group. While Benedict contended that Proto-Tibeto-Burman would have a two-tone system, Matisoff refrained from reconstructing it since tones in individual languages may have developed independently through the process of tonogenesis . Sino-Tibetan is structurally one of the most diverse language families in the world, including all of the gradation of morphological complexity from isolating ( Lolo-Burmese , Tujia ) to polysynthetic ( Gyalrongic , Kiranti ) languages. While Sinitic languages are normally taken to be
1525-687: The Pyu city-states . Other Burmish languages are still spoken in Dehong Prefecture in the far west of Yunnan. By the 11th century, their Pagan Kingdom had expanded over the whole basin. The oldest texts, such as the Myazedi inscription , date from the early 12th century. The closely related Loloish languages are spoken by 9 million people in the mountains of western Sichuan, Yunnan, and nearby areas in northern Myanmar, Thailand, Laos, and Vietnam. The Tibetic languages are spoken by some 6 million people on
1586-536: The Tibetan Plateau and neighbouring areas in the Himalayas and western Sichuan . They are descended from Old Tibetan , which was originally spoken in the Yarlung Valley before it was spread by the expansion of the Tibetan Empire in the seventh century. Although the empire collapsed in the ninth century, Classical Tibetan remained influential as the liturgical language of Tibetan Buddhism . The remaining languages are spoken in upland areas. Southernmost are
1647-739: The Beichuan Red Army Elementary School. Fu River (Sichuan) Fu River , or Fu Jiang ( Chinese : 涪江 ; pinyin : Fú Jiāng ) is a river of in China 's Sichuan Province and Chongqing Municipality. It is a right tributary of the Jialing River , which in its turn is a left tributary of the Yangtze ; it is thus part of the East China Sea basin. The Fu River flows in the general southern and south-eastern direction across
1708-523: The French term sino-tibétain as the title of his chapter on the group in Meillet and Cohen 's Les langues du monde in 1924. He divided them into three groups: Tibeto-Burman, Chinese and Tai, and was uncertain about the affinity of Karen and Hmong–Mien . The English translation "Sino-Tibetan" first appeared in a short note by Przyluski and Luce in 1931. In 1935, the anthropologist Alfred Kroeber started
1769-648: The Sino-Tibetan Philology Project, funded by the Works Project Administration and based at the University of California, Berkeley . The project was supervised by Robert Shafer until late 1938, and then by Paul K. Benedict . Under their direction, the staff of 30 non-linguists collated all the available documentation of Sino-Tibetan languages. The result was eight copies of a 15-volume typescript entitled Sino-Tibetan Linguistics . This work
1830-458: The Yangshao and/or Majiayao cultures. Sagart et al. (2019) performed another phylogenetic analysis based on different data and methods to arrive at the same conclusions to the homeland and divergence model but proposed an earlier root age of approximately 7,200 years ago, associating its origin with millet farmers of the late Cishan culture and early Yangshao culture. Several low-level branches of
1891-423: The absence of any sort of systematic comparison – whether the data are thought reliable or not – such "subgroupings" are essentially vacuous. The use of pseudo-genetic labels such as "Himalayish" and "Kamarupan" inevitably gives an impression of coherence which is at best misleading. In their view, many such languages would for now be best considered unclassified, or "internal isolates" within the family. They propose
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1952-610: The central Sichuan ( Mianyang and Suining Prefectures), and then enters the Chongqing Municipality, where it merges with the Jialing River. 29°59′17″N 106°16′05″E / 29.9881°N 106.268°E / 29.9881; 106.268 This article related to a river in China is a stub . You can help Misplaced Pages by expanding it . Sino-Tibetan Sino-Tibetan (sometimes referred to as Trans-Himalayan )
2013-415: The current spread of Sino-Tibetan languages is the result of historical expansions of the three groups with the most speakers – Chinese, Burmese and Tibetic – replacing an unknown number of earlier languages. These groups also have the longest literary traditions of the family. The remaining languages are spoken in mountainous areas, along the southern slopes of the Himalayas , the Southeast Asian Massif and
2074-547: The details of Tibeto-Burman. However, Jacques (2006) notes, "comparative work has never been able to put forth evidence for common innovations to all the Tibeto-Burman languages (the Sino-Tibetan languages to the exclusion of Chinese)" and that "it no longer seems justified to treat Chinese as the first branching of the Sino-Tibetan family," because the morphological divide between Chinese and Tibeto-Burman has been bridged by recent reconstructions of Old Chinese . The internal structure of Sino-Tibetan has been tentatively revised as
2135-527: The eastern edge of the Tibetan Plateau . The branch with the largest number of speakers by far is the Sinitic languages , with 1.3 billion speakers, most of whom live in the eastern half of China. The first records of Chinese are oracle bone inscriptions from c. 1250 BC , when Old Chinese was spoken around the middle reaches of the Yellow River . Chinese has since expanded throughout China, forming
2196-523: The eastern edge of the Tibetan plateau. The 22 official languages listed in the Eighth Schedule to the Constitution of India include only two Sino-Tibetan languages, namely Meitei (officially called Manipuri) and Bodo . There has been a range of proposals for the Sino-Tibetan urheimat , reflecting the uncertainty about the classification of the family and its time depth. Three major hypotheses for
2257-453: The entire family "Tibeto-Burman", a name he says has historical primacy, but other linguists who reject a privileged position for Chinese nevertheless continue to call the resulting family "Sino-Tibetan". Like Matisoff, van Driem acknowledges that the relationships of the "Kuki–Naga" languages ( Kuki , Mizo , Meitei , etc.), both amongst each other and to the other languages of the family, remain unclear. However, rather than placing them in
2318-451: The evacuated town. No casualties were caused. Beichuan was at the center of one of two zones where seismic intensity were the highest at XI liedu during this earthquake and its aftershocks. Since the earthquake, the central government has increased fortification intensity for seismic design for the old county town from VI to VIII. Beichuan County has 9 towns , 9 townships , and 1 ethnic township . ^ Beichuan County had
2379-445: The family as a whole is still at an early stage, so the higher-level structure of Sino-Tibetan remains unclear. Although the family is traditionally presented as divided into Sinitic (i.e. Chinese languages) and Tibeto-Burman branches, a common origin of the non-Sinitic languages has never been demonstrated. The Kra–Dai and Hmong–Mien languages are generally included within Sino-Tibetan by Chinese linguists but have been excluded by
2440-451: The family, particularly Lolo-Burmese , have been securely reconstructed, but in the absence of a secure reconstruction of a Sino-Tibetan proto-language , the higher-level structure of the family remains unclear. Thus, a conservative classification of Sino-Tibetan/Tibeto-Burman would posit several dozen small coordinate families and isolates ; attempts at subgrouping are either geographic conveniences or hypotheses for further research. In
2501-413: The few scholars still arguing that Chinese is not related to Tibeto-Burman. Benedict also reconstructed, at least for Tibeto-Burman, prefixes such as the causative s- , the intransitive m- , and r- , b- g- and d- of uncertain function, as well as suffixes -s , -t and -n . Old Chinese is by far the oldest recorded Sino-Tibetan language, with inscriptions dating from around 1250 BC and
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2562-592: The following Stammbaum by Matisoff in the final print release of the Sino-Tibetan Etymological Dictionary and Thesaurus (STEDT) in 2015. Matisoff acknowledges that the position of Chinese within the family remains an open question. Sergei Starostin proposed that both the Kiranti languages and Chinese are divergent from a "core" Tibeto-Burman of at least Bodish, Lolo-Burmese, Tamangic, Jinghpaw, Kukish, and Karen (other families were not analysed) in
2623-472: The following phylogenetic tree in 2019, based on lexical items: Except for the Chinese, Bai , Karenic , and Mruic languages, the usual word order in Sino-Tibetan languages is object–verb . However, Chinese and Bai differ from almost all other subject–verb–object languages in the world in placing relative clauses before the nouns they modify. Most scholars believe SOV to be the original order, with Chinese, Karen, and Bai having acquired SVO order due to
2684-474: The influence of neighbouring languages in the Mainland Southeast Asia linguistic area . This has been criticized as being insufficiently corroborated by Djamouri et al. 2007, who instead reconstruct a VO order for Proto-Sino-Tibetan. Contrastive tones are a feature found across the family although absent in some languages like Purik . Phonation contrasts are also present among many, notably in
2745-500: The international community since the 1940s. Several links to other language families have been proposed, but none have broad acceptance. A genetic relationship between Chinese, Tibetan, Burmese, and other languages was first proposed in the early 19th century and is now broadly accepted. The initial focus on languages of civilizations with long literary traditions has been broadened to include less widely spoken languages, some of which have only recently, or never, been written. However,
2806-596: The modern Bodic languages. Second, there is a body of lexical cognates between the Chinese and Bodic languages, represented by the Kirantic language Limbu . In response, Matisoff notes that the existence of shared lexical material only serves to establish an absolute relationship between two language families, not their relative relationship to one another. Although some cognate sets presented by van Driem are confined to Chinese and Bodic, many others are found in Sino-Tibetan languages generally and thus do not serve as evidence for
2867-499: The other three locations in Sichuan, namely Wenchuan , Dujiangyan , and Shifang , that raised similar claims. Many places in other parts of China have made similar claims. Also like the other three counties and towns in Sichuan holding claims to be the birthplace of Yu the Great, Beichuan is among the most severely hit of all disaster regions following the 2008 Sichuan earthquake , including
2928-460: The outlines of Conrady's Indo-Chinese classification, though putting Karen in an intermediate position: Shafer criticized the division of the family into Tibeto-Burman and Sino-Daic branches, which he attributed to the different groups of languages studied by Konow and other scholars in British India on the one hand and by Henri Maspero and other French linguists on the other. He proposed
2989-555: The place and time of Sino-Tibetan unity have been presented: Zhang et al. (2019) performed a computational phylogenetic analysis of 109 Sino-Tibetan languages to suggest a Sino-Tibetan homeland in northern China near the Yellow River basin. The study further suggests that there was an initial major split between the Sinitic and Tibeto-Burman languages approximately 4,200 to 7,800 years ago (with an average of 5,900 years ago), associated with
3050-412: The reconstruction of the family is much less developed than for families such as Indo-European or Austroasiatic . Difficulties have included the great diversity of the languages, the lack of inflection in many of them, and the effects of language contact. In addition, many of the smaller languages are spoken in mountainous areas that are difficult to reach and are often also sensitive border zones. There
3111-634: The rhyming patterns of early poetry. The first complete reconstruction, the Grammata Serica Recensa of Bernard Karlgren , was used by Benedict and Shafer. Karlgren's reconstruction was somewhat unwieldy, with many sounds having a highly non-uniform distribution. Later scholars have revised it by drawing on a range of other sources. Some proposals were based on cognates in other Sino-Tibetan languages, though workers have also found solely Chinese evidence for them. For example, recent reconstructions of Old Chinese have reduced Karlgren's 15 vowels to
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#17330853132713172-495: The similarities attributed to diffusion across the Mainland Southeast Asia linguistic area , especially since Benedict (1942) . The exclusions of Vietnamese by Kuhn and of Tai and Miao–Yao by Benedict were vindicated in 1954 when André-Georges Haudricourt demonstrated that the tones of Vietnamese were reflexes of final consonants from Proto-Mon–Khmer . Many Chinese linguists continue to follow Li's classification. However, this arrangement remains problematic. For example, there
3233-650: The site has been deemed too vulnerable. The survivors of the quake have been relocated. The earthquake also caused a landslide on Mount Tangjia which dammed the Jian River and created the Tangjiashan Quake Lake . The lake was once in danger of causing the Tangjiashan Dam to collapse and catastrophically flood downstream communities, totalling over a million persons. On June 10, 2008, the lake spilled through an artificially constructed sluice channel and flooded
3294-575: The smaller Sino-Tibetan languages are spoken in inaccessible mountainous areas, many of which are politically or militarily sensitive and thus closed to investigators. Until the 1980s, the best-studied areas were Nepal and northern Thailand . In the 1980s and 1990s, new surveys were published from the Himalayas and southwestern China. Of particular interest was the increasing literature on the Qiangic languages of western Sichuan and adjacent areas. Most of
3355-545: The status of Qiang autonomy. The Beichuan Qiang Autonomous County was formally created on July 6, 2003. Beichuan was the first county in Sichuan to make the claim as the birthplace of Yu the Great , founder of the Xia dynasty and traditionally regarded as the first hereditary sovereign in Chinese history. Although this claim is probably more commercial than historical, Beichuan was part of West Qiang ( Chinese : 西羌 ) that some ancient records accredited as Yu's birthplace, just like
3416-413: The subclassification or even ST affiliation in all of several minor languages of northeastern India, in particular, is either poor or absent altogether. While relatively little has been known about the languages of this region up to and including the present time, this has not stopped scholars from proposing that these languages either constitute or fall within some other Tibeto-Burman subgroup. However, in
3477-415: The van Driem's Trans-Himalayan fallen leaves model to be more plausible than the bifurcate classification of Sino-Tibetan being split into Sinitic and Tibeto-Burman. Roger Blench and Mark W. Post have criticized the applicability of conventional Sino-Tibetan classification schemes to minor languages lacking an extensive written history (unlike Chinese, Tibetic, and Burmese). They find that the evidence for
3538-401: Was attacked by Roy Andrew Miller , though Benedict's supporters attribute it to the effects of prefixes that have been lost and are often unrecoverable. The issue remains unsolved today. It was cited together with the lack of reconstructable shared morphology, and evidence that much shared lexical material has been borrowed from Chinese into Tibeto-Burman , by Christopher Beckwith , one of
3599-704: Was first applied to this group in 1856 by James Richardson Logan , who added Karen in 1858. The third volume of the Linguistic Survey of India , edited by Sten Konow , was devoted to the Tibeto-Burman languages of British India . Studies of the "Indo-Chinese" languages of Southeast Asia from the mid-19th century by Logan and others revealed that they comprised four families: Tibeto-Burman, Tai , Mon–Khmer and Malayo-Polynesian . Julius Klaproth had noted in 1823 that Burmese, Tibetan, and Chinese all shared common basic vocabulary but that Thai , Mon , and Vietnamese were quite different. Ernst Kuhn envisaged
3660-488: Was never published, but furnished the data for a series of papers by Shafer, as well as Shafer's five-volume Introduction to Sino-Tibetan and Benedict's Sino-Tibetan, a Conspectus . Benedict completed the manuscript of his work in 1941, but it was not published until 1972. Instead of building the entire family tree, he set out to reconstruct a Proto-Tibeto-Burman language by comparing five major languages, with occasional comparisons with other languages. He reconstructed
3721-571: Was set up in 564 A.D. during the Northern Zhou dynasty. The Tang dynasty first created another county, Shiquan ( Chinese : 石泉 ; pinyin : Shíquán ) inside the original Beichuan county in 634 A.D., then in 651 A.D. merged Beichuan county into Shiquan. The Republic of China changed the county name back to Beichuan in 1914 because there had been a Shiquan county in Shaanxi province before 564 A.D. In 1988, China granted Beichuan county
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