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Atlin River

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The Copper River or Ahtna River ( / ˈ ɑː t n ə / ), Ahtna Athabascan ‘Atna’tuu ( [ʔatʰnaʔtʰuː] ), "river of the Ahtnas", Tlingit Eeḵhéeni ( [ʔìːq.híː.nì] ), "river of copper", is a 290-mile (470 km) river in south-central Alaska in the United States. It drains a large region of the Wrangell Mountains and Chugach Mountains into the Gulf of Alaska . It is known for its extensive delta ecosystem , as well as for its prolific runs of wild salmon , which are among the most highly prized stocks in the world. The river is the tenth largest in the United States, as ranked by average discharge volume at its mouth.

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38-978: The Atlin River ( Lingít : Áa Tlein Héeni ) is a river located in the Atlin/Áa Tlein Téix'i Provincial Park in the Canadian province of British Columbia . It flows out from Atlin Lake . 59°37′20″N 133°51′12″W  /  59.62222°N 133.85333°W  / 59.62222; -133.85333 This article related to a river in British Columbia , Canada is a stub . You can help Misplaced Pages by expanding it . Tlingit language The Tlingit language ( English: / ˈ k l ɪ ŋ k ɪ t / KLING -kit ; Lingít Tlingit pronunciation: [ɬɪ̀nkɪ́tʰ] )

76-416: A circumflex , and long low vowels are marked with a grave accent. Short low vowels are unmarked. Coastal Tlingit <áa> and <aa> are Inland <â> and <à> respectively. Coastal <éi> and <ei> are Inland <ê> and <è>, Coastal <ée> and <ee> are Inland <î> and <ì>, and Coastal <óo> and <oo> are Inland <û> and <ù>. Word onset

114-622: A modern work postdating Naish and Story's work in the 1960s. Copper River (Alaska) The Copper River rises out of the Copper Glacier , which lies on the northeast side of Mount Wrangell , in the Wrangell Mountains , within Wrangell-Saint Elias National Park . It begins by flowing almost due north in a valley that lies on the east side of Mount Sanford , and then turns west, forming

152-468: Is murmured , essentially a rapid opening of the glottis once articulation is begun.) The tone values in two-tone dialects can be predicted in some cases from the three-tone values but not the reverse. Earlier, it was hypothesized that the three-tone dialects were older and that the two-tone dialects evolved from them. However, Jeff Leer 's discovery of the Tongass dialect in the late 1970s has shown that

190-673: Is always consonantal in Tlingit and so words never begin with a vowel. Where a vowel would theoretically have occurred, such as by prefixing or compounding, the vowel is always followed by either [ʔ] or [j] . The former is universal in single words, and both are found in word-medial position in compounds. The orthography does not reflect the [ʔ] in word-initial position, but either . or y may be seen in medial position. For example: khu- INDH . OBJ - ÿu- PERF - ÿa- ( 0 , - D , +I)- t'áa hot khu- ÿu- ÿa- t'áa INDH .OBJ- PERF- {(0, -D, +I)}- hot "the weather

228-442: Is because of the influence of English, which makes a similar distinction. For speakers who make the voiced/unvoiced distinction, the distribution is symmetrical with the unaspirated/aspirated distinction among other speakers. Maddieson , Smith, and Bessel (2001) note that all word final non-ejective stops are phonemically unaspirated. That contrasts with the orthography that typically represents them as aspirated stops: t [tʰ] for

266-434: Is common to later hear such speakers producing those forms themselves. It is uncertain whether this assimilation is autochthonous or if it arose from contact with English, but the former is more likely from a purely articulatory perspective. Young speakers and second-language learners are increasingly making a voiced/unvoiced distinction between consonants, rather than the traditional unaspirated/aspirated distinction. That

304-404: Is divided into roughly five major dialects, all of which are essentially mutually intelligible: The various dialects of Tlingit can be classified roughly into two-tone and three-tone systems. Tongass Tlingit, however, has no tone but a four-way register contrast between short, long, glottalized, and "fading" vowels. (In the last type, the onset of the vowel is articulated normally but the release

342-405: Is hot" Unknown glossing abbreviation(s) ( help ); But when the perfective prefix ÿu- is word-initial, the glottal stop appears to ensure that the word begins with a consonant. ∅- 3 . NEU . OBJ - ÿu- PERF - ÿa- ( 0 , - D , +I)- t'áa hot ∅- ÿu- ÿa- t'áa 3. NEU .OBJ- PERF- {(0, -D, +I)}- hot "it is hot" Unknown glossing abbreviation(s) ( help ); Until

380-555: Is now a ghost town tourist attraction and historic district maintained by the National Park Service . Copper River Highway (Alaska Route 10) runs from Cordova to the lower Copper River near Childs Glacier, following the old railroad route and ending at the reconstructed Million Dollar Bridge across the river. The Tok Cut-Off (Alaska Route 1) follows the Copper River Valley on the north side of

418-734: Is open all year-long, but peak season on the Copper River lasts from August to September, when the coho salmon runs. The fisheries are co-managed by the Alaska Department of Fish and Game (ADF&G) and the Department of the Interior Federal Subsistence Board. Management data is obtained primarily by ADF&G at the Miles Lake sonar station and via the native village of Eyak at

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456-410: Is possible but has not been verified that aspirated and unaspirated stops are collapsed into a single phoneme word-finally. Maddieson and colleagues also confirm that the ejective fricatives in Tlingit are in fact true ejectives, despite the widely-held assumption that ejective fricatives are not actually phonetically ejective but are as a sequence of fricative and glottal stop. In Tlingit, at least,

494-735: Is spoken by the Tlingit people of Southeast Alaska and Western Canada and is a branch of the Na-Dene language family . Extensive effort is being put into revitalization programs in Southeast Alaska to revive and preserve the Tlingit language and culture. Missionaries of the Russian Orthodox Church were the first to develop a written version of Tlingit by using the Cyrillic script to record and translate it when

532-621: Is symmetric with an aspirated consonant Cʰ , and a glottalized vowel Vʔ is symmetric with an ejective (glottalized) consonant Cʼ . That implies that the two systems have no familial relationship. Leer (1978) speculated that the maintenance of the pretonal system in Tongass Tlingit was caused by the proximity of its speakers around the Cape Fox area near the mouth of the Portland Canal to speakers of Coastal Tsimshian, just to

570-546: The Chugach Mountains . The river's famous salmon runs arise from the use of the river watershed by over 2 million salmon each year for spawning. The extensive runs result in many unique varieties, prized for their fat content. The river's commercial salmon season is very brief, beginning in May for chinook salmon , and sockeye salmon for periods lasting mere hours or several days at a time. Sport fishing by contrast

608-542: The Coast Tsimshian dialect . However, Krauss and Leer (1981, p. 165) point out that the fading vowels in Coastal Tsimshian are the surface realization of underlying sequences of vowel and glottalized sonorant, VʔC . That is in contradistinction to the glottal modifications in Tongass Tlingit, which Leer argues are symmetric with the modifications of the consonantal system. Thus, a fading vowel V̤

646-663: The Russian Empire had contact with Alaska and the coast of North America down to Sonoma County, California . After the Alaska Purchase , English-speaking missionaries from the United States developed a written version of the language with the Latin alphabet . The history of Tlingit is poorly known, mostly because there is no written record until the first contact with Europeans around the 1790s. Documentation

684-748: The Taku River and into northern British Columbia and the Yukon around Atlin Lake ( Áa Tleen "Big Lake") and Teslin Lake ( Desleen < Tas Tleen "Big Thread") lake districts, as well as a concentration around Bennett Lake at the end of the Chilkoot Trail ( Jilkhoot ). Otherwise, Tlingit is not found in Canada . Tlingit legend tells that groups of Tlingit once inhabited the Stikine , Nass , and Skeena river valleys during their migrations from

722-573: The Baird Canyon and Canyon Creek research stations. The Copper River Delta, which extends for 700,000 acres (2,800 km ), is the largest contiguous wetlands along the Pacific coast of North America . It is used annually by 16 million shorebirds, including the world's entire population of western sandpipers and the pacific flyway population of dunlins . It is also home to the world's largest population of nesting trumpeter swans and

760-458: The Copper River. Both Miles Glacier and Childs Glacier calve directly into the river. The Copper enters the Gulf of Alaska southeast of Cordova where it creates a delta nearly 50 miles (80 km) wide. The name of the river comes from the abundant copper deposits along the upper river that were used by Alaska Native population and then later by settlers from the Russian Empire and

798-516: The Haida linguist John Enrico presented new arguments and reopened the debate. Victor Golla writes in his 2011 California Native Languages , "John Enrico, the contemporary linguist with the deepest knowledge of Haida, continues to believe that a real, if distant, genetic relationship connects Haida to Na-Dene[.]" The Tlingit language is distributed from near the mouth of the Copper River down

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836-601: The Northern dialect, the dominant spoken dialect of Tlingit and the standard for written Tlingit, every vowel may take either high or low tone ; in the orthography high tone is indicated by an acute accent ( áa ) and low tone is unmarked ( aa ). The Southern and Transitional dialects have a mid tone which is unmarked and additional low tone which is marked by a grave accent ( àa ). The Inland Tlingit orthography does not use vowel digraphs. Instead, short high vowels are marked with an acute accent, long high vowels are marked with

874-468: The Tongass vowel system is adequate to predict the tonal features of both the two-tone and three-tone dialects, but none of the tonal dialects could be used to predict vocalic feature distribution in Tongass Tlingit. Thus, Tongass Tlingit is the most conservative of the various dialects of Tlingit, preserving contrasts which have been lost in the other dialects. The fading and glottalized vowels in Tongass Tlingit have also been compared with similar systems in

912-531: The United States. Extraction of the copper resources was problematic due to navigation difficulties at the river's mouth. The construction of the Copper River and Northwestern Railway from Cordova through the upper river valley from 1908 to 1911 allowed widespread extraction of the mineral resources, in particular from the Kennecott Mine , discovered in 1898. The mine was abandoned in 1938 and

950-481: The articulation of ejective fricatives includes complete closure of the glottis before frication begins, and the larynx is raised in the same manner as with ejective stops. Characteristically, the ejective fricatives in Tlingit feature a much smaller aperture for frication than is found in ordinary fricatives. That articulation provides increased resistance to counter the continual loss of dynamic airstream pressure. Also, ejective fricatives appear to include tightening of

988-464: The distances that separate them, both geographic and linguistic. Tlingit is currently classified as a distinct and separate branch of Na-Dene, an indigenous language family of North America . Edward Sapir (1915) argued for its inclusion in the Na-Dené family, a claim that was subsequently debated by Franz Boas (1917), P.E. Goddard (1920), and many other prominent linguists of the time. Studies in

1026-718: The interior. There is a small group of speakers (some 85) in Washington as well. Golla (2007) reported a decreasing population of 500 speakers in Alaska. The First Peoples' Cultural Council (2014) reported 2 speakers in Canada out of an ethnic population of 400. As of 2013, Tlingit courses are available at the University of Alaska Southeast . In April 2014, Alaska HB 216 recognized Tlingit as an official language of Alaska, lending support to language revitalization . Tlingit

1064-676: The late 1960s, Tlingit was written exclusively in phonetic transcription in the works of linguists and anthropologists except for a little-known Cyrillic alphabet used for publications by the Russian Orthodox Church . A number of amateur anthropologists doing extensive work on the Tlingit had no training in linguistics and so left numerous samples in vague and inconsistent transcriptions, the most famous being George T. Emmons . However, such noted anthropologists as Franz Boas , John R. Swanton , and Frederica de Laguna have transcribed Tlingit in various related systems that feature accuracy and consistency but sacrifice readability. Two problems ensue from

1102-512: The late 20th century by (Heinz-)Jürgen Pinnow (1962, 1968, 1970, int. al.) and Michael E. Krauss (1964, 1965, 1969, int. al.) showed a strong connection to Eyak and hence to the Athabaskan languages . Sapir initially proposed a connection between Tlingit and Haida , but the debate over Na-Dene gradually excluded Haida from the discussion. Haida is now considered an isolate , with some borrowing from its long proximity with Tlingit. In 2004,

1140-421: The more accurate d [t] . There is a wide variation in ordinary speech, ranging from unreleased [t̚] to a very delayed aspiration [tːʰ] . However, the underlying phoneme is certainly unaspirated /t/ since it is consistently produced when the word is suffixed. The orthography usually but not always reflects that: hít "house" is written (du) hídi "(his) house" when marked with the possessive suffix -ÿí . It

1178-489: The multiplicity of transcription systems used for Tlingit. One is that there are many of them, thus requiring any reader to learn each individual system depending on what sources are used. The other is that most transcriptions made before Boas's study of Tlingit have numerous mistakes in them, particularly because of misinterpretations of the short vowels and ejective consonants. Accuracy of transcription can be increased by checking against similar words in other systems, or against

Atlin River - Misplaced Pages Continue

1216-748: The northwest edge of the Wrangell Mountains and separating them from the Mentasta Mountains to the northeast. It continues to turn southeast, through a wide marshy plain to Chitina , where it is joined from the southeast by the Chitina River ( Ahtna Athabascan Tsedi Na' [tʃɛ.diː.näʔ] < tsedi " copper " + na’ " river "). The Copper River is approximately 290 miles (470 km) long. It drops an average of about 12 feet per mile (2.3 m/km), and drains more than 24,000 square miles (62,000 km )—an area

1254-551: The open coast of the Gulf of Alaska and throughout almost all of the islands of the Alexander Archipelago in Southeast Alaska . It is characterized by four or five distinct dialects, but they are mostly mutually intelligible. Almost all of the area where the Tlingit language is endemic is contained within the modern borders of Alaska . The exception is an area known as "Inland Tlingit" that extends up

1292-481: The pharyngeal muscles, which reduces the diameter of the air column and so further increases pressure. That pharyngeal constriction is not true pharyngealization, however, since the diameter is still greater than what is found in pharyngealized consonants in other languages. Tlingit has eight vowels , four vowels further distinguished formally by length . However, the length distinction is often in terms of tenseness rather than length, particularly in rapid speech. For

1330-539: The size of West Virginia. The river runs at an average of 7 miles per hour (11 km/h). Downstream from its confluence with the Chitina it flows southwest, passing through a narrow glacier-lined gap in the Chugach Mountains within the Chugach National Forest east of Cordova Peak . There is an extensive area of linear sand dunes up to 250 feet (76 m) in height radiating from the mouth of

1368-514: The south. Tlingit has a complex phonological system compared to Indo-European languages such as English or Spanish . It has an almost complete series of ejective consonants accompanying its stop, fricative, and affricate consonants. The only missing consonant in the Tlingit ejective series is [ʃʼ] . The language is also notable for having several laterals but no voiced [l] and for having no labials in most dialects, except for [m] and [p] in recent English loanwords . The consonants in

1406-584: The table are given in the IPA, with the popular orthography equivalents in brackets. Marginal or historical phonemes are given in parentheses. Nasal consonants assimilating with /n/ and the velar and uvular plosives is common among Tlingit-speakers of all dialects. For example, the sequence ng ( /nk/ ) is often heard as [ŋk] and ngh ( /nq/ ) as [ɴq] . Native speakers in a teaching position may admonish learners when they produce these assimilated forms, deriding them as "not Tlingit" or "too English", but it

1444-571: Was sparse and irregular until the early 20th century. The language appears to have spread northward from the Ketchikan – Saxman area towards the Chilkat region since certain conservative features are reduced gradually from south to north. The shared features between the Eyak language , found around the Copper River delta, and Tongass Tlingit , near the Portland Canal , are all the more striking for

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