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Lake Nipigon

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Lake Nipigon ( / ˈ n ɪ p ɪ ɡ ɒ n / NIP -ih-gon ; French : lac Nipigon ; Ojibwe : Animbiigoo-zaaga'igan ) is part of the Great Lakes drainage basin . It is the largest lake entirely within the boundaries of the Canadian province of Ontario .

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90-528: In the Jesuit Relations the lake is called lac Alimibeg , and was subsequently known as Alemipigon or Alepigon . In the 19th century it was frequently spelled as Lake Nepigon . This may have originated from the Ojibwe word Animbiigoong , meaning 'at continuous water' or 'at waters that extend [over the horizon].' Though some sources claim the name may also be translated as 'deep, clear water,' this description

180-494: A lingua franca or trade language in the circum-Great Lakes area , particularly in interactions with speakers of other Algonquian languages. Documentation of such usage dates from the 18th and 19th centuries, but earlier use is likely, with reports as early as 1703 suggesting that Ojibwe was used by different groups from the Gulf of Saint Lawrence to Lake Winnipeg , and from as far south as Ohio to Hudson Bay . Documentation from

270-495: A playa lake , sabkha , and mudflat environments; purple shales and siltstones interpreted as subaerial mudflat deposits; and an upper unit of cross-stratified sandstone beds, which are interpreted to be aeolian in origin. They accumulated in an intracratonic rift basin between 1450 and 1500 million years ( Ma ) ago. The Sibley Group unconformably overlies highly deformed and metamorphosed Archean turbiditic sandstones and meta volcanic and granitic rocks. The strata of

360-435: A schwa and depending on the writer, may be transcribed as "i", "e" or "a". For example, anami'egiizhigad [ na · m ' e · gii · zh gad /əˌnaməˈʔɛːˌɡiːʒəˌɡad/ ] (Sunday, literally 'prayer day') may be transcribed as anama'egiizhigad in those dialects. The general grammatical characteristics of Ojibwe are shared across its dialects. The Ojibwe language is polysynthetic , exhibiting characteristics of synthesis and

450-492: A stratum ( pl. : strata ) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either bedding surfaces or bedding planes . Prior to the publication of the International Stratigraphic Guide, older publications have defined a stratum as being either equivalent to

540-456: A central role in Ojibwe grammar. Noun inflection and particularly verb inflection indicate a wide variety of grammatical information, realized through the use of prefixes and suffixes added to word stems . Grammatical characteristics include the following: There is a distinction between two different types of third person : the proximate (the third person deemed more important or in focus) and

630-436: A few millimeters to several meters or more. A band may represent a specific mode of deposition : river silt , beach sand , coal swamp , sand dune , lava bed, etc. In the study of rock and sediment strata, geologists have recognized a number of different types of strata, including bed , flow , band , and key bed . A bed is a single stratum that is lithologically distinguishable from other layers above and below it. In

720-515: A fur trading post on Lake Nipigon named Fort la Tourette after his brother, Claude Greysolon, Sieur de la Tourette. The Alexis Hubert Jaillot map of 1685 ( Partie de la Nouvelle-France ) suggests that this fort was somewhere in Ombabika Bay at the northeast end of the lake where the Ombabika River and Little Jackfish River (Kabasakkandagaming) empty. This post, like most of the western French posts,

810-567: A geographical term of convenience rather than a genetic subgroup , and its use does not indicate that the Central languages are more closely related to each other than to the other Algonquian languages. The most general Indigenous designation for the language is Anishinaabemowin 'speaking the native language' ( Anishinaabe 'native person,' verb suffix –mo 'speak a language,' suffix –win 'nominalizer'), with varying spellings and pronunciations depending upon dialect. Some speakers use

900-577: A high morpheme -to-word ratio. Ojibwe is a head-marking language in which inflectional morphology on nouns and particularly verbs carries significant amounts of grammatical information. Word classes include nouns , verbs , grammatical particles , pronouns , preverbs , and prenouns . Preferred word orders in a simple transitive sentence are verb-initial, such as verb–object–subject and verb–subject–object . While verb-final orders are dispreferred, all logically possible orders are attested. Complex inflectional and derivational morphology play

990-633: A o/ and three corresponding long vowels /iː aː oː/ in addition to a fourth long vowel /eː/ , which lacks a corresponding short vowel. The short vowel /i/ typically has phonetic values centring on [ɪ] ; /a/ typically has values centring on [ə]~[ʌ] ; and /o/ typically has values centring on [o]~[ʊ] . Long /oː/ is pronounced [uː] for many speakers, and /eː/ is often [ɛː] . Ojibwe has nasal vowels . Some arising predictably by rule in all analyses, and other long nasal vowels are of uncertain phonological status. The latter have been analysed as underlying phonemes and/or as predictable and derived by

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1080-621: A single bed or composed of a number of beds; as a layer greater than 1 cm in thickness and constituting a part of a bed; or a general term that includes both bed and lamina . Related terms are substrate and substratum (pl. substrata ), a stratum underlying another stratum. Typically, a stratum is generally one of a number of parallel layers that lie one upon another to form enormous thicknesses of strata. The bedding surfaces (bedding planes) that separate strata represent episodic breaks in deposition associated either with periodic erosion , cessation of deposition, or some combination of

1170-427: A third subgroup which is further divided into (i) a subgrouping of Northwestern Ojibwe and Saulteaux , and a subgrouping consisting of Eastern Ojibwe and a further subgrouping comprising Southwestern Ojibwe and Central Ojibwe. Valentine has proposed that Ojibwe dialects are divided into three groups: a northern tier consisting of Severn Ojibwe and Algonquin; a southern tier consisting of "Odawa, Chippewa, Eastern Ojibwe,

1260-1042: Is 165 metres (541 ft). Its original watershed area is 24,560 km (9,484 sq mi). This was increased by about 60% to 38,920 square kilometres (15,030 sq mi) after 14,360 square kilometres (5,545 sq mi) of the Ogoki River basin were diverted in 1943 to the headwaters of the Little Jackfish River, a tributary of Lake Nipigon. Lake Nipigon occupies a basin created by repeated and preferential erosion of relatively flat-lying and faulted, Proterozoic sedimentary strata and igneous sills by repeated Pleistocene glaciations . The Sibley Group consists of about 950 metres (3,120 ft) of unmetamorphosed Mesoproterozoic red beds that are typically flat-lying. These red beds consist of basal fluvial - lacustrine conglomerates , sandstones , and shales overlain by cyclic dolomite - siltstone layers, stromatolites and red mudstones , which represent

1350-490: Is a significant Ojibwe influence. In locations such as Turtle Mountain, North Dakota individuals of Ojibwe ancestry now speak Michif and Ojibwe. Bungi Creole is an English-based Creole language spoken in Manitoba by the descendants of "English, Scottish, and Orkney fur traders and their Cree or Saulteaux wives ...". Bungee incorporates elements of Cree; the name may be from the Ojibwe word bangii 'a little bit' or

1440-585: Is adduced. The Central languages share a significant number of common features. These features can generally be attributed to diffusion of features through borrowing: "Extensive lexical, phonological, and perhaps grammatical borrowing—the diffusion of elements and features across language boundaries—appears to have been the major factor in giving the languages in the area of the Upper Great Lakes their generally similar cast, and it has not been possible to find any shared innovations substantial enough to require

1530-494: Is also in place at Lowell Elementary School in Duluth, Minnesota . The Algonquian language family of which Ojibwemowin is itself a member of the Algic language family, other Algic languages being Wiyot and Yurok . Ojibwe is sometimes described as a Central Algonquian language, along with Fox , Cree , Menominee , Miami-Illinois , Potawatomi , and Shawnee . Central Algonquian is

1620-613: Is an open-source app available for iOS devices. The Ojibwe People's Dictionary is an online language resource created in collaboration with the University of Minnesota. It is an accessible system that allows users to search in English or Ojibwe and includes voice recordings for many of the 17 000 entries in the collection. Despite what they have faced in the American and Canadian Governments' attempt to force Ojibwe into language death through

1710-846: Is called makade-mashkikiwaaboo ('black liquid-medicine') by many speakers, rather than gaapii . These new words vary from region to region, and occasionally from community to community. For example, in Northwest Ontario Ojibwemowin , 'airplane' is ombaasijigan , literally 'device that gets uplifted by the wind' (from ombaasin , 'to be uplifted by the wind') as opposed to the Minnesota bemisemagak . Like any language dialects spanning vast regions, some words that may have had identical meaning at one time have evolved to have different meanings today. For example, zhooniyaans (literally 'small[-amount of] money' and used to refer to coins) specifically means 'dime' (10-cent piece) in

1800-492: Is for Lake Temagami . Today, the Ojibwa bands call Lake Nipigon Animbiigoo-zaaga'igan . The 1778 Il Paese de' Selvaggi Outauacesi, e Kilistinesi Intorno al Lago Superiore map by John Mitchell identifies the lake as Lago Nepigon and its outlet as F. Nempissaki . In the 1807 map A New Map of Upper & Lower Canada by John Cary, the lake was called Lake St. Ann or Winnimpig , while the outflowing river as Red Stone R. Today,

1890-533: Is impossible because of the existence of three dams that effectively hinders navigation. Ontario Parks has designated the area as the Lake Nipigon Basin Signature Site, because of its remarkable range of natural and recreational values. The site includes many provincial parks, conservation reserves, and enhanced management areas around the lake and within its watershed. Protected areas on or at Lake Nipigon include: Other protected areas within

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1980-447: Is known that some speakers of Menominee also speak Ojibwe and that the pattern persisted into the 20th century. Similarly, bilingualism in Ojibwe is still common among Potawatomis who speak Potawatomi. Reports from traders and travellers as early as 1744 indicate that speakers of Menominee , another Algonquian language, used Ojibwe as a lingua franca. Other reports from the 18th century and the early 19th century indicate that speakers of

2070-543: Is more commonly employed in the United States and in southwestern Ontario among descendants of Ojibwe migrants from the United States. Ojibwe and Potawatomi are frequently viewed as being more closely related to each other than to other Algonquian languages. Ojibwe and Potawatomi have been proposed as likely candidates for forming a genetic subgroup within Proto-Algonquian , although the required research to ascertain

2160-669: Is no single dialect that is considered the most prestigious or most prominent, and no standard writing system that covers all dialects. Dialects of Ojibwemowin are spoken in Canada, from southwestern Quebec , through Ontario , Manitoba and parts of Saskatchewan , with outlying communities in Alberta ; and in the United States, from Michigan to Wisconsin and Minnesota , with a number of communities in North Dakota and Montana , as well as groups that were removed to Kansas and Oklahoma during

2250-798: Is not in dispute. The relatively low degrees of mutual intelligibility between some nonadjacent Ojibwe dialects led Rhodes and Todd to suggest that Ojibwe should be analyzed as a linguistic subgroup consisting of several languages. While there is some variation in the classification of Ojibwe dialects, at a minimum the following are recognized, proceeding west to east: Western Ojibwe (Saulteaux) , Southwestern Ojibwe (Chippewa) , Northwestern Ojibwe , Severn Ojibwe (Oji-Cree) , Ottawa (Odawa) , Eastern Ojibwe , and Algonquin . Based upon contemporary field research, Valentine also recognizes several other dialects: Berens Ojibwe in northwestern Ontario, which he distinguishes from Northwestern Ojibwe; North of (Lake) Superior; and Nipissing. The latter two cover approximately

2340-476: Is phonologically contrastive and so is phonemic . Although long and short vowels are phonetically distinguished by vowel quality, vowel length is phonologically relevant since the distinction between long and short vowels correlates with the occurrence of vowel syncope , which characterizes the Ottawa and Eastern Ojibwe dialects, as well as word stress patterns in the language. There are three short vowels /i

2430-497: Is present in phonological representations . The Ottawa and Southwestern Ojibwe (Chippewa) have /h/ in a small number of affective vocabulary items in addition to regular /ʔ/ . Some dialects may have otherwise non-occurring sounds such as /f, l, r/ in loanwords . Obstruent consonants are divided into lenis and fortis sets, with these features having varying phonological analyses and phonetic realizations cross-dialectally. In some dialects, such as Severn Ojibwe, members of

2520-403: Is the most plausible explanation for the distinctive linguistic features found in these three dialects. Many communities adjacent to these relatively sharply differentiated dialects show a mix of transitional features, reflecting overlap with other nearby dialects. While each of these dialects has undergone innovations that make them distinctive, their status as part of the Ojibwe language complex

2610-413: The 2000 United States Census and the 2006 Canadian census . The Ojibwe language is reported as spoken by a total of 8,791 people in the United States of which 7,355 are Native Americans and by as many as 47,740 in Canada, making it one of the largest Algic languages by numbers of speakers. The Red Lake , White Earth , and Leech Lake reservations are known for their tradition of singing hymns in

2700-597: The Gull Bay First Nation . Formerly, the Whitesand First Nation was also located along the northwestern shores of Lake Nipigon until they were relocated in 1942. The membership of these six First Nations total about 5,000. Additionally along Lake Nipigon, there are three Indian reserves  : McIntyre Bay IR 54 (Rocky Bay First Nation), Jackfish Island IR 57 and Red Rock (Parmachene) IR 53 (Red Rock First Nation). The first nations CBC TV series Spirit Bay

2790-641: The Indian Removal period . While there is some variation in the classification of its dialects, at least the following are recognized, from east to west: Algonquin , Eastern Ojibwe , Ottawa (Odawa) , Western Ojibwe (Saulteaux) , Oji-Cree (Severn Ojibwe) , Northwestern Ojibwe , and Southwestern Ojibwe (Chippewa) . Based upon contemporary field research, J. R. Valentine also recognizes several other dialects: Berens Ojibwe in northwestern Ontario, which he distinguishes from Northwestern Ojibwe; North of (Lake) Superior; and Nipissing. The latter two cover approximately

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2880-589: The Indian Reorganization Act of 1934 mandated the phasing-out of the Native American boarding school program, the practice of sending youth to these institutions continued into the 1960s and 1970s. Because children were forced to live away from their home communities, many never had the opportunity to hear and use their native language. This government assimilation effort caused widespread loss of language and culture among indigenous communities, including

2970-611: The Midcontinent Rift System event, estimated at 1,109 Ma ago. Thick sills up to 150 to 200 metres (490–660 ft) thick are also related with the rifting event, forming cliffs that are up to 150 to 200 metres (490–660 ft) high. The mafic and ultramafic intrusions in and around the Nipigon Embayment have widely been interpreted to represent a failed arm of the Midcontinent Rift System, although

3060-693: The Province of Canada in the Robinson Treaty of 1850, also known as the Robinson Superior Treaty . A four square mile reservation was set aside on Gull River near Lake Nipigon on both sides of the river for the Chief Mishe-muckqua (from Mishi-makwa , "Great Bear"). That same year, the HBC moved its trading post there from Wabinosh Bay. The post, known as Nipigon or Fort Nipigon, was headquarters of

3150-627: The Red Rock First Nation located along the Nipigon River still bears the "Red Stone" name. In the 1827 map Partie de la Nouvelle Bretagne. by Philippe Vandermaelen, the lake was called L. St. Anne , while the outflowing river as R. Nipigeon . In the 1832 map North America sheet IV. Lake Superior. by the Society for the Diffusion of Useful Knowledge, the lake was called S Ann or Red L. , while

3240-656: The Treaty of Paris (1763) , the area passed into the hands of the British, and the Hudson's Bay Company (HBC) expanded its trading area to include the Lake, to compete with the North West Company , who were already operating there. In 1784 and 1790, the HBC sent representatives to survey the lake, and set up their first trading post in 1792 on the north-east side. Around 1821, the HBC replaced

3330-540: The obviative (the third person deemed less important or out of focus). Nouns can be singular or plural in number and either animate or inanimate in gender. Separate personal pronouns exist but are used mainly for emphasis; they distinguish inclusive and exclusive first-person plurals. Verbs, the most complex word class, are inflected for one of three orders ( indicative , the default; conjunct , used for participles and in subordinate clauses ; and imperative , used with commands), as negative or affirmative, and for

3420-664: The 17th century indicates that the Wyandot language (also called Huron), one of the Iroquoian languages , was also used as a trade language east of the Great Lakes by speakers of the Nipissing and Algonquin dialects of Ojibwe, and also by other groups south of the Great Lakes, including the Winnebago and by a group of unknown affiliation identified only as "Assistaeronon." The political decline of

3510-674: The Cree equivalent, but whether there is any other Ojibwe component in Bungee is not documented. Ojibwe borrowings have been noted in Menominee , a related Algonquian language . All dialects of Ojibwe generally have an inventory of 17 consonants . Most dialects have the segment glottal stop /ʔ/ in their inventory of consonant phonemes; Severn Ojibwe and the Algonquin dialect have /h/ in its place. Some dialects have both segments phonetically, but only one

3600-564: The Hurons in the 18th century and the ascendancy of Ojibwe-speaking groups including the Ottawa led to the replacement of Huron as a lingua franca. In the area east of Georgian Bay , the Nipissing dialect was a trade language. In the Lower Peninsula of Michigan , the eastern end of the Upper Peninsula , the area between Lake Erie and Lake Huron , and along the north shore of Georgian Bay,

3690-498: The Nipigon District from 1881 to 1892. In 1900, the post was renamed to Nipigon House, and renamed again in 1954 to Gull Bay. In 1871 Lake Nipigon was included in the new Thunder Bay District . The Township of Nipigon was incorporated in 1908. The Municipality of Greenstone (pop 5662) was incorporated in 2001 and includes Orient Bay, MacDiarmid, Beardmore, Nakina, Longlac, Caramat, Jellicoe and Geraldton. In 1943 Canada and

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3780-556: The Ojibwe language is kept alive through indigenous methods of teaching, which emphasizes hands-on experiences, such as the sugar bush harvest. The language is then passed on in a similar manner in which it has been throughout history in that older members of the community—including elders/instructors and older students at the schools—relay their knowledge and experiences to the younger generation. Ojibwe communities are found in Canada from southwestern Quebec , through Ontario , southern Manitoba and parts of southern Saskatchewan ; and in

3870-510: The Ojibwe language is notable for its relative lack of borrowing from other languages. Instead, speakers far prefer to create words for new concepts from existing vocabulary. For example in Minnesota Ojibwemowin , 'airplane' is bemisemagak , literally 'thing that flies' (from bimisemagad , 'to fly'), and 'battery' is ishkode-makakoons , literally 'little fire-box' (from ishkode , 'fire', and makak , 'box'). Even 'coffee'

3960-421: The Ojibwe language may be more culturally meaningful to communities than simply educating about the culture through English. The goal, as with many other language immersion schools across the country, is to meet state-mandated standards for curriculum in the native language. This can be a challenge as public education standards are rigorous with curriculum on complex mathematic and scientific concepts occurring at

4050-583: The Ojibwe language, is a language of action." Therefore, students are encouraged to learn the language by observing and by doing. For example, each spring the students at Waadookodaading participate in a maple sugar harvest. Older students and elders instruct the younger students on the harvest process, narrating what they are doing in Ojibwemowin as the younger students observe. The younger students are then encouraged to participate as they learn, gathering wood, helping to drill trees, and hauling buckets of sap. Thus,

4140-452: The Ojibwe language. These courses mainly target adults and young adults; however, there are many resources for all age groups, including online games which provide domains for online language use. In the 1980s, The Northern Native-Languages Project was introduced in Ontario to get Indigenous languages such as Ojibwe, to be taught in schools. Years later, the first curriculum was established for

4230-420: The Ojibwe language. As of 2011, Ojibwe is the official language of Red Lake. Because the dialects of Ojibwe are at least partly mutually intelligible, Ojibwe is usually considered to be a single language with a number of dialects, i.e. Ojibwe is "... conventionally regarded as a single language consisting of a continuum of dialectal varieties since ... every dialect is at least partly intelligible to

4320-527: The Ojibwe of the Border Lakes region between Minnesota and Ontario, and Saulteaux; and third, a transitional zone between these two polar groups, in which there is a mixture of northern and southern features." Michif is a mixed language that primarily is based upon French and Plains Cree , with some vocabulary from Ojibwe, in addition to phonological influence in Michif-speaking communities where there

4410-584: The Ojibwe people. With the remaining population of native speakers declining as older generations pass away, many historians consider now an important point in the language's history that will determine if it will proliferate or become extinct. Ojibwe historian Anton Treuer estimates that there are about 1,000 speakers of Ojibwe left in the United States, most residing in Minnesota on the Red Lake Indian Reservation or in Mille Lacs region. Teacher of

4500-402: The Ottawa dialect served as a trade language. In the area south of Lake Superior and west of Lake Michigan Southwestern Ojibwe was the trade language. A widespread pattern of asymmetrical bilingualism is found in the area south of the Great Lakes in which speakers of Potawatomi or Menominee, both Algonquian languages, also spoke Ojibwe, but Ojibwe speakers did not speak the other languages. It

4590-553: The Sibley Group fill and are limited to a rift basin known as the Nipigon Embayment that underlies Lake Nipigon. Outside of the rift basin and east and west of Lake Nipigon, the Sibley Group is absent and erosion resistant Archean rocks are either exposed at the surface or blanketed by Pleistocene glacial sediments. The Archean and Proterozoic strata are intruded by a number of mafic and ultramafic intrusions , which define

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4680-657: The Sibley Group, are host to unconformity -related uranium and redbed -type copper ore deposits. As the last ice age was ending, Lake Nipigon was, at times, part of the drainage path for Lake Agassiz . The French Jesuit Claude Allouez celebrated the first Mass beside the Nipigon River May 29, 1667. He visited the village of the Nipissing Indians who had fled there during the Iroquois onslaught of 1649-50. In 1683, Daniel Greysolon, Sieur du Lhut , established

4770-641: The United States agreed to the Ogoki diversion which diverts water into Lake Superior that would normally flow into James Bay and thence into Hudson Bay . The diversion connects the upper portion of the Ogoki River to Lake Nipigon. This water was diverted to boost the Sir Adam Beck Hydroelectric Generating Stations at Niagara Falls . The diversion is governed by the International Lake Superior Board of Control which

4860-675: The United States from northern Michigan through northern Wisconsin and northern Minnesota , with a number of communities in northern North Dakota and northern Montana . Groups of speakers of the Ottawa dialect migrated to Kansas and Oklahoma during the historical period, with a small amount of linguistic documentation of the language in Oklahoma. The presence of Ojibwe in British Columbia has been noted. Current census data indicate that all varieties of Ojibwe are spoken by approximately 56,531 people. This figure reflects census data from

4950-456: The United States, but a 'quarter' (25-cent piece) in Canada, or desabiwin (literally 'thing to sit upon') means 'couch' or 'chair' in Canada, but is used to specifically mean 'saddle' in the United States. Cases like 'battery' and 'coffee' also demonstrate the often great difference between the literal meanings of the individual morphemes in a word, and the overall meaning of the entire word. Strata In geology and related fields,

5040-628: The Waadookodaading Ojibwe Language Immersion School located on the Lac Courte Oreilles Reservation in northern Wisconsin. Most students come from English-speaking homes and are learning Ojibwemowin as their second language. At this school, instructors and elders teach the preschoolers to third graders entirely in the Ojibwe language, so that by the time that students complete kindergarten, they know both English and Ojibwe alphabets and writing systems. In

5130-525: The beginning of a word are frequently lost. In the Ottawa and Eastern Ojibwe dialects, all metrically weak vowels are deleted. For example, bemisemagak(in) (airplane(s), in the Southwestern Ojibwe dialect) is stressed as [ be · m se · m gak /ˈbɛːmɪˌseːmʌˌɡak/ ] in the singular but as [ be · m se · m ga · kin /ˌbeːmɪˈsɛːmʌˌɡaˌkin/ ] in the plural. In some other dialects, metrically weak (unstressed) vowels, especially "a" and "i", are reduced to

5220-473: The classification hierarchy of sedimentary lithostratigraphic units, a bed is the smallest formal unit. However, only beds that are distinctive enough to be useful for stratigraphic correlation and geologic mapping are customarily given formal names and considered formal lithostratigraphic units. The volcanic equivalent of a bed, a flow, is a discrete extrusive volcanic stratum or body distinguishable by texture, composition, or other objective criteria. As in case of

5310-507: The classroom, students generally first become familiar with the language by hearing and speaking it and then advance to reading and writing it as well. They are taught mathematics, reading, social studies, music, and other typical school subjects through the medium of the Ojibwe language so as to increase student's exposure to Ojibwemowin while providing a well-rounded education. In her research study on Ojibwe immersion schools, Ojibwe scholar and educator Mary Hermes suggests that educating through

5400-560: The current outline of the Nipigon Embayment. They consist of relatively flat-lying and undeformed diabase sills known as the Nipigon diabase sills. These sills range in thickness from a few meters to 150 metres (490 ft) thick in cliff sections to more than 250 metres (820 ft) thick in drill core. They are estimated to cover an area in excess of 20,000 square kilometres (7,700 sq mi). The Nipigon diabase sills give evidence of rift -related continental basaltic magmatism during

5490-537: The educational system, many indigenous communities across the Great Lakes region are making efforts towards the Ojibwe language revival by similarly using the school system. Largely inspired by the success of Polynesian languages immersion schools in Hawaii and New Zealand , similar school programs have been starting throughout Minnesota and Wisconsin in recent years. One of the most notable programs—developed by Ojibwe educators Lisa LaRonge and Keller Paap —is that of

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5580-540: The fortis set are realized as a sequence of /h/ followed by a single segment drawn from the set of lenis consonants: /p t k tʃ s ʃ/ . Algonquin Ojibwe is reported as distinguishing fortis and lenis consonants on the basis of voicing , with fortis being voiceless and lenis being voiced. In other dialects fortis consonants are realized as having greater duration than the corresponding lenis consonant, invariably voiceless, "vigorously articulated," and aspirated in certain environments. In some practical orthographies such as

5670-530: The important role language revitalization has in treating health concerns. The use of language connects a community through shared views and supports the well-being of said community. Researchers found that language and the notion of culture were intertwined together instead of being separate concepts, and the people who regularly practiced their language and culture were often associated with more positive health outcomes, particularly for psychological health and mental well-being. An "Ojibway Language and People" app

5760-589: The lack of dike intrusions , compared to the relative abundance of flat, saucer-shaped sills in the embayment, has led some researchers to question the dominant failed rift arm model. The Proterozoic rocks that underlie the Lake Nipigon region contain a variety of mineral resources. Although economic deposits have yet to be found, 1.53 billion-year-old anorogenic granites within the Lake Nipigon area potentially contain yttrium , zirconium , rare earth elements and tin mineralization. The clastic sedimentary rocks of

5850-514: The lake's basin: Ojibwe language Ojibwe ( / oʊ ˈ dʒ ɪ b w eɪ / oh- JIB -way ), also known as Ojibwa ( / oʊ ˈ dʒ ɪ b w ə / oh- JIB -wə ), Ojibway , Otchipwe , Ojibwemowin , or Anishinaabemowin , is an indigenous language of North America of the Algonquian language family . The language is characterized by a series of dialects that have local names and frequently local writing systems . There

5940-665: The language Keller Paap approximates that most fluent speakers in the United States are over 70 years old, making exposure to spoken Ojibwemowin limited in many communities. Ojibwe educators and scholars across the region are working with the remaining elders who speak Ojibwemowin, known as the First Speakers, so as to document and learn the language in hopes to preserve it and pass it on to the next generation of speakers. In recent years, historian and Ojibwe professor Anton Treuer has been recording stories told by about 50 different Ojibwe elders in their native language so as to preserve both

6030-449: The language and language structure; however, it does not help grow the use of the language outside of a school setting. The most effective way of promoting language is being surrounded by the language, especially in a familial setting. This is difficult to replicate in schools, which is why speaking Ojibwe with family and in one's home life is important in growing language revitalization. Research has been done in Ojibwe communities to prove

6120-431: The language and pieces of knowledge and history. Alongside his current mentor, a Ponemah elder named Eugene Stillday, he writes the recorded stories in both Ojibwe and translated English. Recently, there has been more of a push toward bringing the Ojibwe language back into more common use, through language classes and programs sponsored by universities, sometimes available to non-students, which are essential to passing on

6210-662: The largest tributaries of Lake Superior. It lies about 120 kilometres (75 mi) northeast of the city of Thunder Bay , Ontario . Lake Nipigon has a total area (including islands within the lake) of 4,848 square kilometres (1,872 sq mi), compared to 3,150 square kilometres (1,220 sq mi) for Lake of the Woods . It is the 32nd largest lake in the world by area . The largest islands are Caribou Island, Geikie Island, Katatota Island, Kelvin Island , Logan Island, Murchison Island, Murray Island, and Shakespeare Island. Maximum depth

6300-542: The late 19th century, the American federal Native American boarding school initiative which forced Native American children to attend government-run boarding schools in an attempt to "acculturate" them into American society. Often far from their home communities, these schools attempted to remove any ties children had to their native culture and to limit their ability to visit home. Students were forced to speak English, cut their hair, dress in uniform, practise Christianity, and learn about European culture and history. Although

6390-399: The linguistic history and status of a hypothetical "Ojibwe–Potawatomi" subgroup has not yet been undertaken. A discussion of Algonquian family subgroups indicates that "Ojibwe–Potawatomi is another possibility that awaits investigation." In a proposed consensus classification of Algonquian languages, Goddard (1996) classifies Ojibwa and Potawatomi as "Ojibwayan," although no supporting evidence

6480-415: The metrical foot defines the domain for relative prominence , in which a strong syllable is assigned stress because it is more prominent than the weak member of the foot. Typically, the strong syllable in the antepenultimate foot is assigned the primary stress. Strong syllables that do not receive main stress are assigned at least secondary stress. In some dialects, metrically weak (unstressed) vowels at

6570-444: The operation of phonological rules from sequences of a long vowel and /n/ and another segment, typically /j/. Placement of word stress is determined by metrical rules that define a characteristic iambic metrical foot , in which a weak syllable is followed by a strong syllable. A foot consists of a minimum of one syllable and a maximum of two syllables, with each foot containing a maximum of one strong syllable. The structure of

6660-523: The original post with a second one in the northwest, called Wabinosh House. It was nearly abandoned due to strife and murders between local indigenous groups. Once the dispute was resolved however, the post remained open. Although it was considered to be within British North America , it was not until 1850 that the watershed draining into Lake Superior was ceded formally by the Ojibwe Indians to

6750-518: The outflowing river as Neepigeon and the heights near the outlet of the Gull River as Neepigon Ho. By 1883, maps such as Statistical & General Map of Canada by Letts, Son & Co., consistently began identify the lake as Lake Nipigon . Lying 260 metres (853 ft) above sea level, the lake drains into the Nipigon River and thence into Nipigon Bay of Lake Superior . The lake and river are

6840-399: The person, number, animacy, and proximate/obviative status of both the subject and object as well as for several different modes (including the dubitative and preterit ) and tenses. Although it does contain a few loans from English (e.g. gaapii , 'coffee') and French (e.g. mooshwe , 'handkerchief' (from mouchoir ), ni-tii , 'tea' (from le thé , 'the tea'), in general,

6930-416: The postulation of a genetically distinct Central Algonquian subgroup." The possibility that the proposed genetic subgrouping of Ojibwa and Potawatomi can also be accounted for as diffusion has also been raised: "The putative Ojibwa–Potawatomi subgroup is similarly open to question, but cannot be evaluated without more information on Potawatomi dialects." Several different Ojibwe dialects have functioned as

7020-446: The program and it was known as Native Languages 1987. There has also been an increase in published children's literature. The increase in materials published in Ojibwe is essential to increasing the number of speakers. Language revitalization through Ojibwe frameworks also allows for cultural concepts to be conveyed through language. A 2014 study has indicated that learning Indigenous languages such as Ojibwe in school helps in learning

7110-408: The question as to whether or not they should include English instruction. Some research suggests that learning to write in one's first language is important prior to learning a second language. Therefore, many schools include some level of English education at certain grade levels. Along with using the native language, Waadookodaading uses native ways of teaching in its education system. "Ojibwemowin,

7200-619: The same territory as Central Ojibwa , which he does not recognize. The aggregated dialects of Ojibwemowin comprise the second most commonly spoken First Nations language in Canada (after Cree ), and the fourth most widely spoken in the United States or Canada behind Navajo , the Inuit languages and Cree. Ojibwemowin is a relatively healthy indigenous language. The Waadookodaading Ojibwe Language Immersion School in Hayward, Wisconsin teaches all classes to children in Ojibwe only. A similar program

7290-596: The same territory as Central Ojibwa , which he does not recognize. Two recent analyses of the relationships between the Ojibwe dialects are in agreement on the assignment of the strongly differentiated Ottawa dialect to a separate subgroup, and the assignment of Severn Ojibwe and Algonquin to another subgroup, and differ primarily with respect to the relationships between the less strongly differentiated dialects. Rhodes and Todd recognize several different dialectal subgroupings within Ojibwe: (a) Ottawa; (b) Severn and Algonquian; (c)

7380-483: The second and third grade levels. Ojibwe educators at these schools are constantly working with elders so as to design new ways to say lesser-used words in Ojibwe such as plastic or quotient . Because the Ojibwe language is traditionally oral, it is often difficult for educators to find adequate resources to develop the curriculum. Thus, through these school programs, the language is constantly evolving. Many of these Ojibwe language immersion schools are also considering

7470-482: The speakers of the neighboring dialects." The degree of mutual intelligibility between nonadjacent dialects varies considerably; recent research has shown that there is strong differentiation between the Ottawa dialect spoken in southern Ontario and northern Michigan; the Severn Ojibwa dialect spoken in northern Ontario and Manitoba; and the Algonquin dialect spoken in southwestern Quebec. Valentine notes that isolation

7560-662: The term Ojibwemowin . The general term in Oji-Cree (Severn Ojibwe) is Anihshininiimowin , although Anishinaabemowin is widely recognized by Severn speakers. Some speakers of Saulteaux Ojibwe refer to their language as Nakawemowin . The Ottawa dialect is sometimes referred to as Daawaamwin , although the general designation is Nishnaabemwin , with the latter term also applied to Jibwemwin or Eastern Ojibwe . Other local terms are listed in Ojibwe dialects . English terms include Ojibwe , with variants including Ojibwa and Ojibway . The related term Chippewa

7650-493: The two. Stacked together with other strata, individual stratum can form composite stratigraphic units that can extend over hundreds of thousands of square kilometers of the Earth 's surface. Individual stratum can cover similarly large areas. Strata are typically seen as bands of different colored or differently structured material exposed in cliffs , road cuts, quarries , and river banks. Individual bands may vary in thickness from

7740-626: The unrelated Siouan language Ho-Chunk (Winnebago) also used Ojibwe when dealing with Europeans and others. Other reports indicate that agents of the American government at Green Bay, Wisconsin , spoke Ojibwe in their interactions with Menominee, with other reports indicating that "the Chippewa, Menominee, Ottawa, Potawatomi, Sac, and Fox tribes used Ojibwe in intertribal communication...." Some reports indicate that farther west, speakers of non-Algonquian languages such as Ho-Chunk (Winnebago), Iowa , and Pawnee spoke Ojibwe as an "acquired language." In

7830-693: The widely-used double vowel system, fortis consonants are written with voiceless symbols: p, t, k, ch, s, sh . Lenis consonants have normal duration and are typically voiced intervocalically. Although they may be devoiced at the end or beginning of a word, they are less vigorously articulated than fortis consonants, and are invariably unaspirated. In the double vowel system, lenis consonants are written with voiced symbols: b, d, g, j, z, zh . All dialects of Ojibwe have two nasal consonants /m/ and /n/ , one labialized velar approximant /w/ , one palatal approximant /j/ , and either /ʔ/ or /h/ . All dialects of Ojibwe have seven oral vowels . Vowel length

7920-616: Was closed in 1696 by order of the king, when, due to a surplus of beaver pelts, the system of trading permits established in 1681 was abolished. On 17 April 1744, the Count of Maurepas , Minister of the Marine, informed the Canadian officials that Jean de La Porte was to be given the " fur ferme " (i.e. the profits) of Lac Alemipigon from that year forward as a reward for his services in New France. After

8010-732: Was established in 1914 by the International Joint Commission . The aboriginal population (primarily Ojibwe ) include the Animbiigoo Zaagi'igan Anishinaabek (Lake Nipigon Ojibway) First Nation, the Biinjitiwaabik Zaaging (Rocky Bay whose name changed in 1961 from McIntyre Bay Indian Band) Anishinaabek First Nation , the Bingwi Neyaashi (Sand Point) Anishinaabek First Nation , the Red Rock (Lake Helen) First Nation and

8100-662: Was filmed on the lake at the Biinjitiwaabik Zaaging Anishinaabek First Nation Reserve in the mid-1980s. The main line of the Canadian National Railway runs to the north of the lake. Another branch of the CNR touches the southeastern section of the lake at Orient Bay and Macdiarmid before heading inland to Beardmore . Ontario Highway 11 also skirts the southeastern section of the lake. Water travel between Lake Nipigon and Lake Superior

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