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39-587: Fort Simpson ( Slavey language : Łı́ı́dlı̨ı̨ Kų́ę́ "place where rivers come together") is a village, the only one in the entire territory, in the Dehcho Region of the Northwest Territories , Canada. The community is located on an island at the confluence of the Mackenzie and Liard rivers. It is approximately 500 km (310 mi) west of Yellowknife . Both rivers were traditionally trade routes for

78-402: A subarctic climate ( Köppen Dfc ) with long, cold winters and warm but short summers. July temperatures are unusually warm for such northerly areas, which demonstrates the extreme continental nature of the area's climate. However, the heat quickly turns into cold winters when daylight hours turn drastically shorter. Transition seasons are extremely short, and the year is on average dominated by

117-595: A dry winter, are found in parts of East Asia, like China, where the Siberian High makes the winters colder than places like Scandinavia or Alaska interior but extremely dry (typically with around 5 millimeters (0.20 in) of rainfall equivalent per month), meaning that winter snow cover is very limited. The Dwc climate can be found in: In the Southern Hemisphere, small pockets of the Lesotho Highlands and

156-484: A population of 1,100 living in 452 of its 572 total private dwellings, a change of -8.5% from its 2016 population of 1,202 . With a land area of 77.89 km (30.07 sq mi), it had a population density of 14.1/km (36.6/sq mi) in 2021. In 2016, 890 people identified as Indigenous peoples . Of these the majority, 770, of the residents are First Nations with 95 Métis and 20 Inuit . The main languages are South Slavey and English. Fort Simpson has

195-535: A separate phoneme. Prenasalized stops /ᵐb, ⁿd/ may appear in Slavey proper. The most pronounced difference is however the realization of a series of consonants that varies greatly in their place of articulation: In Slavey proper, these are dental affricates and fricatives; comparative Athabaskan work reveals this to be the oldest sound value. Mountain has labials, with the voiceless stop coinciding with pre-existing /p/ . Bearlake has labialized velars, but has lenited

234-465: A subarctic climate, receives an average rain-equivalent of 101.91 inches (2,588.5 mm) of precipitation per year. Coastal areas of Khabarovsk Krai also have much higher precipitation in summer due to orographic influences (up to 175 millimetres (6.9 in) in July in some areas), whilst the mountainous Kamchatka peninsula and Sakhalin island are even wetter, since orographic moisture isn't confined to

273-478: A very specific morpheme order in the verb in which the stem must come last. The morpheme order is shown in the following chart. A Slavey verb must minimally have positions 13 and 14 to be proper. Here are some examples: Slavey marks gender by means of prefixation on the verb theme. There are three different genders, one of which is unmarked; the other two are marked by prefixes [go-] and [de-] . However, only certain verb themes allow gender prefixes. [go-]

312-464: Is based largely on the way each one pronounces the old Proto-Athapaskan sounds *dz *ts *ts’ *s and *z. The consonant inventories in the dialects of Slavey differ considerably. The table above lists the 30 consonants common to most or all varieties. Hare lacks aspirated affricates (on red background), which have lenited into fricatives, whereas Mountain lacks /w/ (on blue). In addition, for some speakers of Hare, an alveolar flap /ɾ/ has developed into

351-507: Is excessive. The frost-free season is very short, varying from about 45 to 100 days at most, and a freeze can occur anytime outside the summer months in many areas. The first D indicates continentality, with the coldest month below 0 °C (32 °F) (or −3 °C (27 °F)). The second letter denotes precipitation patterns: The third letter denotes temperature: Most subarctic climates have little precipitation, typically no more than 380 mm (15 in) over an entire year due to

390-652: Is found in the following areas: Further north and east in Siberia, continentality increases so much that winters can be exceptionally severe, averaging below −38 °C (−36 °F), even though the hottest month still averages more than 10 °C (50 °F). This creates Dfd climates, which are mostly found in the Sakha Republic : In the Southern Hemisphere , the Dfc climate is found only in small, isolated pockets in

429-626: Is hosted by the Open Sky Creative Society, a multi-disciplinary arts organization serving artists working in the Dehcho region. The Dene of the community are represented by the Łı́ı́dlı̨ı̨ Kų́ę́ First Nation and the Métis by Fort Simpson Métis Local 52. Both groups belong to the Dehcho First Nations . In the 2021 Census of Population conducted by Statistics Canada , Fort Simpson had

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468-603: Is known as the "Beavertail Jamboree". This is a winter carnival which includes traditional games, snowmobile races, and talent shows. The other festival is the "Open Sky Festival" which is held annually on or around the Canada Day long weekend . The Open Sky Festival is a multi-disciplinary arts festival which has occurred annually since 2001. Festival events include musical, theatrical, and other performances as well as traditional Dehcho Dene Crafts, visual arts, new media exhibitions, workshops, and demonstrations. The Open Sky festival

507-510: Is marked with an acute accent, and low tone is unmarked. Tones are both lexical and grammatical. Lexical: /ɡáh/ 'along' vs. /ɡàh/ 'rabbit' Slavey morphemes have underlying syllable structures in the stems: CV, CVC, CVnC, V, and VC. The prefixes of the stem occur as Cv, CVC, VC, CV, and C. Slavey alphabet (1973) Tone is indicated with an acute accent and the ogonek indicates nasalization. North Slavey alphabet South Slavey alphabet Slavey, like many Athabascan languages, has

546-655: Is spoken by the Sahtu (North Slavey) people in the Mackenzie District along the middle Mackenzie River from Tulita (Fort Norman) north, around Great Bear Lake , and in the Mackenzie Mountains of the Canadian territory of Northwest Territories . The dialect has around 800 speakers. Northern Slavey is an amalgamation of three separate dialects : South Slavey ( ᑌᓀ ᒐ Dené Dháh , Dene Yatıé or Dene Zhatıé )

585-816: Is spoken by the Slavey people, who were also known as Dehghaot'ine, Deh Cho, Etchareottine - "People Dwelling in the Shelter", in the region of Great Slave Lake , upper Mackenzie River ( Deh Cho - "Big River") and its drainage, in the District of Mackenzie, northeast Alberta , and northwest British Columbia . Some communities are bilingual, with the children learning Slavey at home and English when they enter school. Still other communities are monolingual in Slavey The dialect has around 1,000 speakers. Alternative names: Slavi, Slave, Dené, Mackenzian The division of Slavey dialects

624-492: Is used for nouns which mark location in either time or space. Some examples of these areal nouns are house (ko̜̒e̒), land (de̒h), river (deh), and winder (xay). The gender pronoun can be a direct object, an oblique object or a possessor. kú̜e̒ house go detl’e̒h 3SG .paints.area kú̜e̒ go detl’e̒h house 3SG.paints.area 'S/he is painting the house.' ko̜̒e̒ house go cha area.in   shelter ko̜̒e̒ go cha {} house area.in shelter 'in

663-534: The Hudson's Bay Company and the native Dene people of the area. Fort Simpson is the regional centre of the Dehcho and is the gateway to the scenic South Nahanni River and the Nahanni National Park Reserve . Fort Simpson can be reached by air, water and road and has full secondary and elementary school service. The Mackenzie Highway was extended to Fort Simpson in 1970-71. The central section of

702-542: The Hudson's Bay Company constructed a trading post , naming it for George Simpson , then the Governor of Rupert's Land . Until 1910 Fort Simpson was "a company town", with some participation by the Anglican and Roman Catholic Missions. The Dené know it as Łı́ı́dlı̨ı̨ Kų́ę́ , meaning the place where the rivers come together . It was designated a National Historic Site of Canada in 1969. Pope John Paul II attempted to visit

741-751: The Pacific Ocean , resulting in increased precipitation, especially during the winter months. This climate zone supports the presence of temperate rainforests, mostly on highest areas of the Valdivian rainforest in Chile and the subantarctic forest in Argentina. Climates classified as Dsc or Dsd , with a dry summer, are rare, occurring in very small areas at high elevation around the Mediterranean Basin , Iran , Kyrgyzstan , Tajikistan , Alaska and other parts of

780-683: The Snowy Mountains of Australia , the Southern Alps of New Zealand , and the Lesotho Highlands . In South America , this climate occurs on the western slope of the central Andes in Chile and Argentina , where climatic conditions are notably more humid compared to the eastern slope. The presence of the Andes mountain range contributes to a wetter climate on the western slope by capturing moisture from

819-640: The northwestern United States ( Eastern Washington , Eastern Oregon , Southern Idaho , California's Eastern Sierra ), the Russian Far East , Akureyri, Iceland , Seneca, Oregon , and Atlin, British Columbia . Turkey and Afghanistan are exceptions; Dsc climates are common in Northeast Anatolia , in the Taurus and Köroğlu Mountains , and the Central Afghan highlands . In the Southern Hemisphere,

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858-416: The subpolar oceanic climate , as the sea is approached where winter temperatures average near or above freezing despite maintaining the short, cool summers. In China and Mongolia, as one moves southwestwards or towards lower elevations, temperatures increase but precipitation is so low that the subarctic climate grades into a cold semi-arid climate . The Dfc climate, by far the most common subarctic type,

897-801: The Dsc climate is present in South America as a subarctic climate influenced by Mediterranean characteristics, often considered a high-altitude variant of the Mediterranean climate. It is located on the eastern slopes of the central Argentine Andes and in some sections on the Chilean side. While there are no major settlements exhibiting this climate, several localities in the vicinity experience it, such as San Carlos de Bariloche , Villa La Angostura , San Martín de los Andes , Balmaceda , Punta de Vacas , and Termas del Flaco . Climates classified as Dwc or Dwd , with

936-430: The coldest month should average below 0 °C (32 °F) (or −3 °C (27 °F)). Record low temperatures can approach −70 °C (−94 °F). With 5–7 consecutive months when the average temperature is below freezing, all moisture in the soil and subsoil freezes solidly to depths of many feet. Summer warmth is insufficient to thaw more than a few surface feet, so permafrost prevails under most areas not near

975-613: The community in September 1984 as part of his Canadian tour, but was prevented from landing due to fog; in an address over the radio from Yellowknife , he promised to visit in the future. He did so in September 1987 near the end of the tour of the United States, making a side trip to Fort Simpson. There are two main annual festivals which occur in Fort Simpson. The first which is held in March

1014-633: The community is on an island near the south bank of the Mackenzie River, but industrial areas and rural residential areas are located along the highway as far as the Fort Simpson Airport , just beyond which is the Liard River ferry crossing. Fort Simpson was first started as a fur trading site in 1803 then named Fort of the Forks. The Village of Fort Simpson was a permanent settlement in July 1822 when

1053-406: The long summer days at such latitudes do permit some agriculture. In some areas, ice has scoured rock surfaces bare, entirely stripping off the overburden. Elsewhere, rock basins have been formed and stream courses dammed, creating countless lakes. Should one go northward or even toward a polar sea, one finds that the warmest month has an average temperature of less than 10 °C (50 °F), and

1092-423: The long winters and make use of the short summers. Trees are mostly limited to conifers , as few broadleaved trees are able to survive the very low temperatures in winter. This type of forest is also known as taiga , a term which is sometimes applied to the climate found therein as well. Even though the diversity may be low, the area and numbers are high, and the taiga (boreal) forest is the largest forest biome on

1131-425: The low temperatures and evapotranspiration . Away from the coasts, precipitation occurs mostly in the summer months, while in coastal areas with subarctic climates the heaviest precipitation is usually during the autumn months when the relative warmth of sea vis-à-vis land is greatest. Low precipitation, by the standards of more temperate regions with longer summers and warmer winters, is typically sufficient in view of

1170-512: The moderating effects of an ocean, generally at latitudes from 50°N to 70°N, poleward of the humid continental climates . Like other Class D climates, they are rare in the Southern Hemisphere, only found at some isolated highland elevations. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification Dfc , Dwc , Dsc , Dfd , Dwd and Dsd . This type of climate offers some of

1209-418: The most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below −50 °C (−58 °F) and in summer, the temperature may exceed 26 °C (79 °F). However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least 10 °C (50 °F) to fall into this category of climate, and

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1248-456: The planet, with most of the forests located in Russia and Canada . The process by which plants become acclimated to cold temperatures is called hardening . Agricultural potential is generally poor, due to the natural infertility of soils and the prevalence of swamps and lakes left by departing ice sheets , and short growing seasons prohibit all but the hardiest of crops. Despite the short season,

1287-403: The shelter of the house' ko̜̒e̒ house go deshįte̒ee area.floor ko̜̒e̒ go deshįte̒ee house area.floor 'floor of the house' Subarctic climate The subarctic climate (also called subpolar climate , or boreal climate ) is a continental climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from

1326-449: The southern boundary of this climate zone. Seasonal thaw penetrates from 2 to 14 ft (0.6 to 4.3 m), depending on latitude, aspect, and type of ground. Some northern areas with subarctic climates located near oceans (southern Alaska , northern Norway , Sakhalin Oblast and Kamchatka Oblast ), have milder winters and no permafrost, and are more suited for farming unless precipitation

1365-403: The subarctic climate grades into a tundra climate not at all suitable for trees. Southward, this climate grades into the humid continental climates with longer summers (and usually less-severe winters) allowing broadleaf trees ; in a few locations close to a temperate sea (as in northern Norway and southern Alaska ), this climate can grade into a short-summer version of an oceanic climate ,

1404-428: The very low evapotranspiration to allow a water-logged terrain in many areas of subarctic climate and to permit snow cover during winter, which is generally persistent for an extended period. A notable exception to this pattern is that subarctic climates occurring at high elevations in otherwise temperate regions have extremely high precipitation due to orographic lift . Mount Washington , with temperatures typical of

1443-533: The voiced fricative to coincide with pre-existing /w/ . The most complicated situation is found in Hare, where the plain stop is a labialized velar, the ejective member is replaced by a /ʔw/ sequence, the aspirated affricate has turned into a fricative /f/ , and both the voiceless and voiced fricatives have been lenited to /w/ . The following phonological and phonetic statements apply to all four dialects of Slavey. Slavey has two tones: In Slavey orthography, high tone

1482-514: The warmer months and creates large glaciers in Kamchatka. Labrador , in eastern Canada, is similarly wet throughout the year due to the semi-permanent Icelandic Low and can receive up to 1,300 millimetres (51 in) of rainfall equivalent per year, creating a snow cover of up to 1.5 metres (59 in) that does not melt until June. Vegetation in regions with subarctic climates is generally of low diversity, as only hardy tree species can survive

1521-531: The winter and to a lesser extent, summer. The average monthly temperatures range from −24.2 °C (−11.6 °F) in January to 17.4 °C (63.3 °F) in July. Most of the precipitation falls during the summer months. The highest temperature ever recorded in Fort Simpson was 36.6 °C (97.9 °F) on 25 July 1994 and 13 July 2014. The coldest temperature ever recorded was −56.1 °C (−69.0 °F) on 1 February 1947. Slavey language North Slavey

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