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44-649: It is preceded by the remaining central segment of Forestry Trunk Road, Highway 734 begins south of the Red Deer River to the southwest of Sundre , and is succeeded by Highway 40 , which also used to be part of Forestry Trunk Road. The highway ends north of the Pembina River . Forestry Trunk Road was a north-south resource road that ran from the Crowsnest Highway ( Highway 3 ) in southern Alberta to Highway 43 in northern Alberta . Over time, some segments of

88-428: A consonant , can be written four ways, each direction representing its corresponding vowel . Some dialects of Cree have up to seven vowels, so additional diacritics are placed after the syllabic to represent the corresponding vowels. Finals represent stand-alone consonants. The Cree language also has two semivowels . The semivowels may follow other consonants or be on their own in a word. The following tables show

132-461: A complex polysynthetic morphosyntax. A common grammatical feature in Cree dialects, in terms of sentence structure, is non-regulated word order. Word order is not governed by a specific set of rules or structure; instead, "subjects and objects are expressed by means of inflection on the verb". Subject, Verb, and Object (SVO) in a sentence can vary in order, for example, SVO, VOS, OVS, and SOV. Obviation

176-802: A full-stop glyph ( ⟨᙮⟩ ) or a double em-width space has been used between words to signal the transition from one sentence to the next. For Plains Cree and Swampy Cree , Standard Roman Orthography (SRO) uses fourteen letters of the ISO basic Latin alphabet to denote the dialect's ten consonants ( ⟨p⟩ , ⟨t⟩ , ⟨c⟩ , ⟨k⟩ , ⟨s⟩ , ⟨m⟩ , ⟨n⟩ , ⟨w⟩ , ⟨y⟩ and ⟨h⟩ ) and seven vowels ( ⟨a⟩ , ⟨i⟩ , ⟨o⟩ , ⟨ā⟩ , ⟨ī⟩ , ⟨ō⟩ and ⟨ē⟩ ). Upper case letters are not used. For more details on

220-539: A provincial highway. Another former segment of Forestry Trunk Road, now the third segment of Highway 40, begins at Highway 1A to the west of Cochrane and ends 46 km (29 mi) later at an intersection with Highway 579. Highway 40 continues as the central remaining segment of Forestry Trunk Road for 27 km (17 mi) to a point 8 km (5.0 mi) prior to the Red Deer River. The road then continues for 268 km (167 mi) as Highway 734 to north of

264-1136: A south-east direction, and while it flows through Dinosaur Provincial Park it turns east and flows to the Alberta/Saskatchewan border, which it crosses at Empress . It flows for 16 km (9.9 mi) through Saskatchewan before it merges into the South Saskatchewan River . The waters of Ewing Lake, Little Fish Lake also flow into the Red Deer River. Sport fish include: walleye , northern pike , sauger , lake whitefish , yellow perch , burbot , lake sturgeon , mountain whitefish , goldeye , brown trout , bull trout , rainbow trout , brook trout , and cutthroat trout . Other fish include: emerald shiner , river shiner , spottail shiner , flathead chub , longnose dace , quillback (quillback carpsucker), longnose sucker , white sucker , shorthead redhorse , silver redhorse , perch , spoonhead sculpin , lake chub , northern pearl dace , northern redbelly dace , finescale dace , fathead minnow and brook stickleback . The Red Deer River

308-484: A total length of 724 km (450 mi) and a drainage area of 45,100 km (17,400 sq mi). Its mean discharge is 70 m /s (2,500 cu ft/s). The river is named for the translation of a native term for the river, wâwâskêsiw sîpiy, which means "elk river" in the Cree language . "Red deer" was an alternative name for elk , referring to a closely related Eurasian species . Communities located along

352-593: A work. The vowel ē /eː/ , used in southern Plains Cree, is always long and the grapheme ⟨e⟩ is never used. In northern Plains Cree the sound has merged with ī , and thus ⟨ē⟩ is not used at all. The use of unmarked ⟨o⟩ and marked ⟨ō⟩ for the phonemes /u/ and /oː/ emphasizes the relationship that can exist between these two vowels. There are situations where o can be lengthened to ō , as for example in ᓂᑲᒧ! nikamo! 'sing (now)!' and ᓂᑲᒨᐦᑲᐣ! nikamōhkan! 'sing (later)!'. In alphabetic writing,

396-548: Is February, with an average of 8.6 mm (0.34 in) of precipitation, while the wettest is June, with an average of 68.9 mm (2.71 in). Cree language Cree ( / k r iː / KREE ; also known as Cree– Montagnais – Naskapi ) is a dialect continuum of Algonquian languages spoken by approximately 86,475 indigenous people across Canada in 2021, from the Northwest Territories to Alberta to Labrador . If considered one language, it

440-458: Is also a key aspect of the Cree language(s). In a sense, the obviative can be defined as any third-person ranked lower on a hierarchy of discourse salience than some other (proximate) discourse-participant. "Obviative animate nouns, [in the Plains Cree dialect for instance], are marked by [a suffix] ending –a , and are used to refer to third persons who are more peripheral in the discourse than

484-499: Is not phonologically transparent, which means gender must be learned along with the noun. As is common in polysynthetic languages, a Cree word can be very long, and express something that takes a series of words in English. For example: kiskinohamātowikamikw know. CAUS . APPL . RECP .place kiskinohamātowikamikw know.CAUS.APPL.RECP.place 'school' ( lit. 'knowing-it-together-by-example place') This means that changing

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528-574: Is the aboriginal language with the highest number of speakers in Canada. The only region where Cree has any official status is in the Northwest Territories , alongside eight other aboriginal languages. There, Cree is spoken mainly in Fort Smith and Hay River . Endonyms are: Cree is believed to have begun as a dialect of the Proto-Algonquian language spoken between 2,500 and 3,000 years ago in

572-642: Is the water source for the City of Red Deer and the surrounding area. Pipelines cross under the river and there have been leaks disrupting access to potable water. Increased water flow of the Red Deer River system during heavy rainfall in June 2008 eroded supporting soil, freely exposing a section of Pembina Pipeline Corporation's Cremona crude oil pipeline to the Red Deer River currents. About 75 to 125 barrels (11,900 to 19,900 L; 2,600 to 4,400 imp gal; 3,200 to 5,200 US gal) of crude oil flowed upstream from

616-530: Is used in Eastern dialects where s and š are distinct phonemes. In other dialects, s is used even when pronounced like [ʃ] . ⟨l⟩ and ⟨r⟩ are used natively in Moose and Attikamek Cree, but in other dialects only for loanwords. The stops, p , t , k , and the affricate, c , can be pronounced either voiced or unvoiced, but the symbols used for writing these sounds all correspond to

660-409: Is very difficult to make definite statements about how different groups emerged and moved around, because there are no written works in the languages to compare, and descriptions by Europeans are not systematic; as well, Algonquian people have a tradition of bilingualism and even of outright adopting a new language from neighbours. A traditional view among 20th-century anthropologists and historians of

704-619: The fur trade posits that the Western Woods Cree and the Plains Cree (and therefore their dialects) did not diverge from other Cree peoples before 1670, when the Cree expanded out of their homeland near James Bay because of access to European firearms. By contrast, James Smith of the Museum of the American Indian stated, in 1987, that the weight of archeological and linguistic evidence puts

748-466: The original Algonquian homeland , an undetermined area thought to be near the Great Lakes. The speakers of the proto-Cree language are thought to have moved north, and diverged rather quickly into two different groups on each side of James Bay . The eastern group then began to diverge into separate dialects, whereas the western grouping probably broke into distinct dialects much later. After this point it

792-469: The proximate third person". For example: Sam Sam wâpam- ew see- 3SG Susan- a Susan- 3OBV Sam wâpam- ew Susan- a Sam see-3SG Susan-3OBV "Sam sees Susan." The suffix -a marks Susan as the obviative, or 'fourth' person, the person furthest away from the discourse. The Cree language has grammatical gender in a system that classifies nouns as animate or inanimate. The distribution of nouns between animate or inanimate

836-480: The syllabaries of Eastern and Western Cree dialects, respectively: Speakers of various Cree dialects have begun creating dictionaries to serve their communities. Some projects, such as the Cree Language Resource Project, are developing an online bilingual Cree dictionary for the Cree language. Cree syllabics has not commonly or traditionally used the period ( ⟨.⟩ ). Instead, either

880-488: The y dialect, refer to their language as nēhi y awēwin , whereas Woods Cree speakers say nīhi th awīwin , and Swampy Cree speakers say nēhi n awēwin . Another important phonological variation among the Cree dialects involves the palatalisation of Proto-Algonquian *k : East of the Ontario–Quebec border (except for Atikamekw), Proto-Algonquian *k has changed into /tʃ/ or /ts/ before front vowels. See

924-578: The 4a plant hardiness zone . Summers are typically warm and rainy with cool nights. Winters are typically long, cold, and very dry. Empress is located in the steppe region known as Palliser's Triangle and experiences a semi-arid climate (Köppen climate classification BSk ). Winters are long, cold and dry, while summers are short, but with average daytime highs that are warm to hot, though nighttime lows are cool. Spring and autumn are quite short, essentially transition periods between winter and summer. Wide diurnal temperature ranges are regular, due to

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968-569: The Cree as far west as the Peace River Region of Alberta before European contact. The Cree dialect continuum can be divided by many criteria. Dialects spoken in northern Ontario and the southern James Bay, Lanaudière, and Mauricie regions of Quebec differentiate /ʃ/ (sh as in sh e ) and /s/ , while those to the west have merged the two phonemes as /s/ and in the east the phonemes are merged as either /ʃ/ or /h/ . In several dialects, including northern Plains Cree and Woods Cree,

1012-545: The Pembina River, north of the Elk River Indian reserve, where it becomes the fourth segment of Highway 40. Over its course, the central segment of Forestry Trunk Road combined with Highway 734 provides access to Ram Falls Provincial Park and numerous campgrounds, and intersects Highway 579, Highway 584 , Highway 591 , Highway 752 , and Highway 11 (David Thompson Highway) west of Nordegg . This stretch also crosses

1056-757: The Plains Cree [j] that is [ð] in Rocky Cree as ⟨ý⟩ . Similarly, in dictionaries focused on Western Swampy Cree, Woods Cree may readily substitute ⟨ē⟩ with ⟨ī⟩ , while materials accommodating Woods Cree will indicate the Western Swampy Cree [n] that is [ð] in Woods Cree as ⟨ń⟩ . Atikamekw uses ⟨c⟩ [ ʃ ], ⟨tc⟩ [ t͡ʃ ], and ⟨i⟩ [ j ] (which also serves as ⟨i⟩ [ i ]). Eastern James Bay Cree prefers to indicate long vowels (other than [eː] ) by doubling

1100-636: The Red Deer River include Sundre , Red Deer , Drumheller , and Empress , The city of Brooks , as well as Dinosaur Provincial Park , are also located in the Red Deer River Basin. A glacial flood about 18,000 years ago eroded out a portion of this basin and apparently all or most of the scenic badlands bearing the dinosaur and other Cretaceous fossils. Joseph Tyrrell discovered a huge coal seam here in 1883, besides large dinosaur skeletons. In June 2013, Alberta, Canada, experienced heavy rainfall that triggered catastrophic flooding throughout much of

1144-532: The Red Deer River. Red Deer has a humid continental climate ( Köppen Dfb ), with something of a semi-arid influence due to the city's location within Palliser's Triangle . The highest temperature ever recorded in Red Deer was 37.2 °C (99.0 °F) on 8 July 1906, 2 July 1924, and 28 & 29 June 1937. The lowest recorded temperature was −50.6 °C (−59.1 °F) on 17 December 1924. The city lies in

1188-524: The Red Deer River. The southern segment is preceded and succeeded by the first and second segments of Highway 40 respectively, while the central segment is preceded by the third segment of Highway 40 and succeeded by Highway 734. The southern remaining segment of Forestry Trunk Road begins 3.8 km (2.4 mi) north of the Crowsnest Highway (Highway 3) as a continuation of the southernmost segment of Highway 40. Over its 99 km (62 mi) length,

1232-521: The Red Deer, James , Clearwater , Ram , North Saskatchewan , Blackstone , Brazeau , and Pembina rivers. Starting from the south end of Highway 40: Download coordinates as: Red Deer River The Red Deer River is a river in Alberta and a small portion of Saskatchewan , Canada. It is a major tributary of the South Saskatchewan River and is part of the larger Saskatchewan / Nelson system that empties into Hudson Bay . The river has

1276-418: The aridity and moderately high elevation. Low humidity is prevalent throughout the year. Annual precipitation is very low, with an average of 311.6 mm (12.27 in), and is heavily concentrated in the warmer months. On average, the coldest month is January, with a mean temperature of −12 °C (10 °F), while the warmest is July, with a mean temperature of 19.8 °C (67.6 °F). The driest month

1320-750: The break point under a Red Deer River channel, leaving an oily sheen on Gleniffer Reservoir and 6,800 kg (15,000 lb) of oil-soaked debris. The remediation was not completed until 2011. Heavy rains in early June 2012 caused a similar but larger leak on a Plains Midstream Canada 46-year-old pipeline on a Red Deer River tributary, Jackson Creek , Alberta ( 51°52′19″N 114°36′23″W  /  51.87194°N 114.60639°W  / 51.87194; -114.60639  ( Jackson Creek ) ) near Gleniffer Lake and Dickson Dam , which spilled approximately 1,000 and 3,000 barrels (160,000 and 480,000 L; 35,000 and 105,000 imp gal; 42,000 and 126,000 US gal) of light sour crude oil into

1364-504: The dialects which use syllabics as their orthography (including Atikamekw but excluding Kawawachikamach Naskapi), the term Montagnais then applies to those dialects using the Latin script (excluding Atikamekw and including Kawawachikamach Naskapi). The term Naskapi typically refers to Kawawachikamach (y-dialect) and Natuashish (n-dialect). The Cree dialects can be broadly classified into nine groups. Roughly from west to east: This table shows

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1408-884: The eastern slopes of the Canadian Rockies , in the Sawback Range near the Skoki Valley inside Banff National Park , and then flows east through the mountains and foothills region. It turns north-east before Sundre and flows to an artificial reservoir named Gleniffer Lake , created in 1983 by the Dickson Dam and keeps this heading to the city of Red Deer , where it turns east, and then south before Stettler . It flows south with its valley protected by provincial and regional parks such as Tolman Badlands Heritage Rangeland , Dry Island Buffalo Jump Provincial Park , Dry Island Corridor and Midland Provincial Park . At Drumheller it has

1452-609: The gravel road provides access to numerous public campgrounds, crosses the Oldman River , and intersects with Highway 532 . It also passes near the Bob Creek Wildland Provincial Park , Livingstone Falls, and the Don Getty Wildland Provincial Park before ending at its intersection with Highway 541 and the second segment of Highway 40, which was part of Forestry Trunk Road before being designated

1496-407: The language phonetically. Cree is always written from left to right horizontally. The easternmost dialects are written using the Latin script exclusively. The dialects of Plains Cree, Woods Cree, and western Swampy Cree use Western Cree syllabics and the dialects of eastern Swampy Cree, East Cree, Moose Cree, and Naskapi use Eastern Cree syllabics . In Cree syllabics, each symbol, which represents

1540-453: The long vowels /eː/ and /iː/ have merged into a single vowel, /iː/ . In the Quebec communities of Chisasibi , Whapmagoostui , and Kawawachikamach , the long vowel /eː/ has merged with /aː/ . However, the most transparent phonological variation between different Cree dialects are the reflexes of Proto-Algonquian *l in the modern dialects, as shown below: The Plains Cree, speakers of

1584-490: The phonetic values of these letters or variant orthographies, see the § Phonology section above. The /ð/ sound of Woods Cree is written ⟨th⟩ , or ⟨ð⟩ in more recent material. Plains and Swampy material written to be cross-dialectical often modify ⟨y⟩ to ⟨ý⟩ and ⟨n⟩ to ⟨ñ⟩ when those are pronounced /ð/ in Swampy. ⟨š⟩

1628-511: The possible consonant phonemes in the Cree language or one of its varieties. In dictionaries focused on Eastern Swampy Cree, Western Swampy Cree may readily substitute ⟨sh⟩ with ⟨s⟩ , while Lowland Moose Cree may readily substitute ⟨ñ⟩ with their ⟨l⟩ . In dictionaries focused on Southern Plains Cree, Northern Plains Cree may readily substitute ⟨ē⟩ with ⟨ī⟩ , while materials accommodating Rocky Cree will indicate

1672-461: The road have been designated as parts of Highway 40 or Highway 734, while the northernmost segment between Highway 40 and Highway 43 is no longer named Forestry Trunk Road. Two segments of Forestry Trunk Road remain – a southern segment from the Municipality of Crowsnest Pass to Highway 541 to the southwest of Longview , and a short central segment from Highway 579 west of Cremona to south of

1716-478: The southern half of the province along the Bow , Elbow , Highwood , Oldman , and Red Deer rivers and tributaries. Twenty-four municipalities declared local states of emergency as water levels rose and numerous communities were placed under evacuation orders. The Royal Canadian Mounted Police stated four people may have drowned near High River . Over 100,000 people in the region were displaced. The river originates on

1760-493: The table above for examples in the * kīla column. Very often the Cree dialect continuum is divided into two languages: Cree and Montagnais. Cree includes all dialects which have not undergone the *k > /tʃ/ sound change (BC–QC) while Montagnais encompasses the territory where this sound change has occurred (QC–NL). These labels are very useful from a linguistic perspective but are confusing as East Cree then qualifies as Montagnais. For practical purposes, Cree usually covers

1804-444: The unvoiced pronunciation, e.g. ⟨p⟩ not ⟨b⟩ , ⟨t⟩ not ⟨d⟩ , etc. The phoneme /t͡s/ is represented by ⟨c⟩ , as it is in various other languages . Long vowels are denoted with either a macron , as in ⟨ā⟩ , or a circumflex , as in ⟨â⟩ . Use of either the macron or circumflex is acceptable, but usage should be consistent within

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1848-418: The use of punctuation has been inconsistent. For instance, in the Plains Cree dialect, the interrogative enclitic cî can be included in the sentence to mark a yes–no question such that this is sometimes considered to be sufficient without including a question mark (?). However, in many modern publications and text collections ( cf. The Counselling Speeches of Jim Kâ-Nîpitêhtêw (1998) ) full punctuation

1892-466: The vowel, while the western Cree use either a macron or circumflex diacritic; as [eː] is always long, often it is written as just ⟨e⟩ without doubling or using a diacritic. While Western Cree dialects make use of ⟨o⟩ and either ⟨ō⟩ or ⟨ô⟩ , Eastern Cree dialects instead make use of ⟨u⟩ and either ⟨uu⟩ , ⟨ū⟩ , or ⟨û⟩ . Cree features

1936-467: The word order in Cree can place emphasis on different pieces of the sentence. Wolfart and Carroll give the following example by transposing the two Cree words: Cree dialects, except for those spoken in eastern Quebec and Labrador , are traditionally written using Cree syllabics , a variant of Canadian Aboriginal syllabics , but can be written with the Latin script as well. Both writing systems represent

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