Lytton | |
---|---|
Village | |
The Corporation of the Village of Lytton [1] | |
Location of Lytton in British Columbia | |
Coordinates: 50°13′52″N121°34′53″W / 50.23111°N 121.58139°W | |
Country | Canada |
Province | British Columbia |
Regional district | Thompson–Nicola |
Incorporated | 1945 |
Government | |
• Governing body | Lytton Village Council |
• Mayor | Denise O'Connor |
Area | |
• Total | 6.54 km2 (2.53 sq mi) |
Elevation | 195 m (640 ft) |
Population (2021) | |
• Total | 210 |
Time zone | UTC−08:00 (PST) |
• Summer (DST) | UTC−07:00 (PDT) |
Website | lytton.ca |
Lytton is a village of about 250 residents in southern British Columbia, Canada, on the east side of the Fraser River and primarily the south side of the Thompson River, where it flows southwesterly into the Fraser. The community includes the Village of Lytton and the surrounding community of the Lytton First Nation, whose name for the place is Camchin, also spelled Kumsheen ("river meeting").
During heat waves, Lytton is often the hottest spot in Canada despite its location north of 50°N in latitude. In three consecutive days of June 2021, it broke the all-time record for Canada's highest temperature, ending at 49.6 °C (121.3 °F) on June 29. This is the highest temperature ever recorded north of 45°N and higher than the all-time records for Europe and South America. The next day (June 30), a wildfire swept through the valley, destroying the majority of the town.
The Lytton area has been inhabited by the First Nations people for over 10,000 years. [2] [3] It was one of the earliest locations settled by immigrants in the Southern Interior of British Columbia. The town was founded during the Fraser Canyon Gold Rush of 1858–59, when it was known as "The Forks."
The people of the Nlakaʼpamux First Nation lived on the site before the town of Lytton was founded. [4] Lytton was on the route of the Fraser Canyon Gold Rush in 1858. The same year, it was named after Edward Bulwer-Lytton, the British Colonial Secretary and a novelist. [5] For many years, Lytton was a stop on major transportation routes, namely, the River Trail beginning in 1858, Cariboo Wagon Road in 1862, the Canadian Pacific Railway in the 1880s, the Cariboo Highway in the 1920s, and the Trans Canada Highway in the 1950s. The town is much less important since the construction of the Coquihalla Highway in 1987, which uses a more direct route to the BC Interior.
In 2015, Lytton was featured on the CBC television show Still Standing with host Jonny Harris. [6]
On June 30, 2021, the day after Lytton set a Canadian all-time high temperature record of 49.6 °C (121.3 °F), a wildfire swept through the community, destroying most structures. [7] All villagers were ordered to evacuate. Local MP Brad Vis said 90% of the village burned down. [8] Two people died. [9]
In the year since the fire, only a quarter of the properties were cleared of ash and debris. There was incessant wrangling between local residents who wanted to restore buildings and power immediately, and the local council who wanted fire-prevention standards in place. Coupled with inadequate insurance payouts and local record-breaking floods, residents were running out of time to restore the village. They were further hampered when another wildfire took out six residences across the river in July 2022. [10]
Novelist Edward Bulwer-Lytton was a friend and contemporary of Charles Dickens and was one of the pioneers of the historical novel, exemplified by his most popular work, The Last Days of Pompeii . He is best remembered today for the opening line to the novel Paul Clifford, which begins "It was a dark and stormy night..." and is considered by some to be the worst opening sentence in the English language. [11] Bulwer-Lytton is also responsible for sayings such as "The pen is mightier than the sword" from his play Richelieu . Though he was a popular author in the 19th century, fewer people today are aware of his prodigious body of literature, which spans many genres. In the 21st century, he may be better known as the namesake for the Bulwer-Lytton Fiction Contest (BLFC), sponsored annually by the English Department at San Jose State University, which challenges entrants "to compose the opening sentence to the worst of all possible novels."
In 1858, Governor James Douglas named the town after Bulwer-Lytton "as a merited compliment and mark of respect." Bulwer-Lytton served as Colonial Secretary. As governor of the then-colony, Douglas would have reported to him. [12] : 158
On August 30, 2008, the Village of Lytton invited Henry Lytton Cobbold, the great-great-great-grandson of Edward Bulwer-Lytton, to defend the great man's honour by debating Professor Scott Rice, the sponsor of the BLFC, on the literary and political legacies of his great ancestor. [13] The debate received wide media coverage including The Globe and Mail , The New York Times , The Guardian , CBC's As It Happens , and many local and regional media outlets. The debate was moderated by Mike McArdell of Global TV. Lytton Cobbold provided a spirited and crowd-inspiring defence of his ancestor, and despite a factual and well-researched presentation by Rice, Lytton Cobbold emerged as the crowd favourite by a wide margin. In the end, Rice begrudgingly admitted to an admiration of Bulwer-Lytton. This event was held as part of the Village of Lytton's BC150 celebrations, which marked the 150th anniversary of the date that the community received its name, in addition to the province-wide celebration of the establishment of the original Colony of British Columbia on August 2, 1858.
In the 2021 Census of Population conducted by Statistics Canada, Lytton had a population of 210 living in 104 of its 118 total private dwellings, a change of -15.7% from its 2016 population of 249. With a land area of 6.73 km2 (2.60 sq mi), it had a population density of 31.2/km2 (80.8/sq mi) in 2021. [14]
Another 1,700 people in the immediate area live in rural areas and on reserves of the neighbouring six Nlaka'pamux communities.[ which? ]
802 members out of 1,970 registered members of the Lytton First Nation live on reserves immediately adjacent to the municipality. [15]
Lytton experiences an inland hot-summer mediterranean climate (Csa), using the -3 °C isotherm, or a dry-summer continental climate (Dsa), using the 0 °C isotherm. During summer heat waves, Lytton is often the hottest spot in Canada, despite its location north of 50°N in latitude. Because of the dry summer air and a relatively low elevation of 195 m (640 ft), summer afternoon shade temperatures frequently reach 35 °C (95 °F) and occasionally top 40 °C (104 °F). Lytton holds the record for the highest temperature ever recorded in Canada with a record high of 49.6 °C (121.3 °F) on June 29 of the 2021 Western North America heat wave. [16] [17] [18] This occurred after having already broken records multiple times during the previous days of that heat wave. This is the world's highest temperature ever recorded north of the 45th parallel. The previous record was 121 °F (49.4 °C) in Steele, North Dakota on July 6, 1936. Lytton has recorded a higher temperature than all but 4 U.S. states, with only Arizona, California, New Mexico, and Nevada ever recording higher temperatures. Lytton has also recorded higher temperatures than all of Europe and South America have ever recorded. [19] [20] [21]
Before the 2021 heat wave occurred, Lytton, along with the nearby community of Lillooet, shared the second-highest temperature ever recorded in Canada. [22] On July 16 and 17, 1941, the temperature reached a then-record 44.4 °C (111.9 °F) on both days in both communities. [23] The coldest temperature ever recorded in Lytton was −31.7 °C (−25.1 °F) on January 18, 1950. [24] While reporting on the new records in 2021, Global News noted that the official Environment and Climate Change Canada weather station is located in the shade and is about 1 °C (1.8 °F) cooler than the rest of the village. [25] Hot summer temperatures are made more tolerable by low humidity. The heat can be intense under usually clear skies and sunlight, or by the valley's radiant slopes. Forest fires are not uncommon during the summer.
Lytton's climate is also characterised by relatively short and mild winters (although average monthly temperatures in December and January are just below freezing), with Pacific maritime influence during the winter ensuring thick cloud cover much of the time. Cold snaps originating from arctic outflow occur from time to time, but tend to be short-lived, and mountains to the north usually block extreme cold from penetrating the Fraser Canyon.
Lytton receives 430.6 mm (16.95 in) [26] of annual precipitation on average, making it much drier than communities to the south but certainly wetter than some of the driest spots in the BC interior, such as Ashcroft, Kamloops, Spences Bridge, and Osoyoos. It has the driest summers in the interior of British Columbia and one of the driest summers of all places in Canada. Maximum precipitation occurs in the cooler months, with late autumn and early winter constituting the wettest time of the year.
Climate data for Lytton WMO ID: 71765; coordinates 50°13′28″N121°34′55″W / 50.22444°N 121.58194°W ; elevation: 225 m (738 ft); 1991–2020 normals, extremes 1921–present | |||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Record high humidex | 16.3 | 15.4 | 24.2 | 30.7 | 38.0 | 49.9 | 45.3 | 41.9 | 37.8 | 28.3 | 18.0 | 14.7 | 49.9 |
Record high °C (°F) | 16.5 (61.7) | 18.3 (64.9) | 24.7 (76.5) | 33.9 (93.0) | 40.4 (104.7) | 49.6 (121.3) | 44.4 (111.9) | 42.2 (108.0) | 39.6 (103.3) | 29.9 (85.8) | 22.8 (73.0) | 17.8 (64.0) | 49.6 (121.3) |
Mean daily maximum °C (°F) | 1.9 (35.4) | 6.0 (42.8) | 10.8 (51.4) | 16.5 (61.7) | 22.0 (71.6) | 24.8 (76.6) | 29.5 (85.1) | 29.5 (85.1) | 23.9 (75.0) | 14.7 (58.5) | 6.7 (44.1) | 1.8 (35.2) | 15.7 (60.3) |
Daily mean °C (°F) | −1.1 (30.0) | 1.9 (35.4) | 5.8 (42.4) | 10.4 (50.7) | 15.5 (59.9) | 18.7 (65.7) | 22.6 (72.7) | 22.4 (72.3) | 17.4 (63.3) | 10.1 (50.2) | 3.7 (38.7) | −0.9 (30.4) | 10.5 (50.9) |
Mean daily minimum °C (°F) | −4.1 (24.6) | −2.1 (28.2) | 0.8 (33.4) | 4.3 (39.7) | 8.9 (48.0) | 12.5 (54.5) | 15.6 (60.1) | 15.2 (59.4) | 10.8 (51.4) | 5.5 (41.9) | 0.6 (33.1) | −3.6 (25.5) | 5.4 (41.7) |
Record low °C (°F) | −31.7 (−25.1) | −25.0 (−13.0) | −21.1 (−6.0) | −7.8 (18.0) | −3.9 (25.0) | 4.4 (39.9) | 6.1 (43.0) | 6.7 (44.1) | −2.2 (28.0) | −18.1 (−0.6) | −27.7 (−17.9) | −30.6 (−23.1) | −31.7 (−25.1) |
Record low wind chill | −34.1 | −27.3 | −23.6 | −9.3 | −1.4 | 0.0 | 0.0 | 0.0 | 0.0 | −9.8 | −28.1 | −36.7 | −36.7 |
Average precipitation mm (inches) | 58.7 (2.31) | 43.2 (1.70) | 31.2 (1.23) | 20.8 (0.82) | 20.6 (0.81) | 17.8 (0.70) | 18.7 (0.74) | 25.4 (1.00) | 29.0 (1.14) | 41.2 (1.62) | 60.3 (2.37) | 63.9 (2.52) | 430.6 (16.95) |
Average rainfall mm (inches) | 42.2 (1.66) | 34.7 (1.37) | 24.6 (0.97) | 20.8 (0.82) | 20.6 (0.81) | 17.8 (0.70) | 18.7 (0.74) | 25.4 (1.00) | 29.0 (1.14) | 40.0 (1.57) | 48.0 (1.89) | 41.6 (1.64) | 363.3 (14.30) |
Average snowfall cm (inches) | 19.4 (7.6) | 11.0 (4.3) | 6.2 (2.4) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 1.4 (0.6) | 12.8 (5.0) | 25.9 (10.2) | 76.6 (30.2) |
Average precipitation days (≥ 0.2 mm) | 11.5 | 10.5 | 8.8 | 7.2 | 8.6 | 7.2 | 6.4 | 6.4 | 7.6 | 10.5 | 13.0 | 12.1 | 109.6 |
Average rainy days (≥ 0.2 mm) | 7.8 | 7.9 | 8.2 | 7.2 | 8.6 | 7.2 | 6.4 | 6.4 | 7.6 | 10.3 | 11.0 | 5.8 | 94.2 |
Average snowy days (≥ 0.2 cm) | 5.5 | 3.6 | 1.6 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.4 | 3.5 | 8.1 | 22.7 |
Average relative humidity (%) (at 1500 LST) | 73.1 | 58.0 | 48.1 | 37.5 | 34.6 | 36.4 | 31.5 | 31.2 | 38.7 | 55.8 | 72.2 | 75.7 | 49.4 |
Mean monthly sunshine hours | 56.0 | 81.6 | 143.0 | 186.7 | 224.2 | 243.8 | 265.2 | 244.2 | 182.0 | 121.8 | 55.7 | 48.1 | 1,852.2 |
Percent possible sunshine | 21.1 | 28.8 | 38.9 | 45.2 | 46.9 | 49.8 | 53.7 | 54.4 | 47.9 | 36.4 | 20.5 | 19.1 | 38.6 |
Source 1: Environment and Climate Change Canada [27] (rain/rain days, snow/snow days, precipitation/precipitation days and sun 1981–2010) [26] [28] [29] [30] [31] [32] | |||||||||||||
Source 2: CBC (June record high only) [18] |
Open coniferous forests of Douglas fir and ponderosa pine dominate the slopes around Lytton. Some black cottonwood is scattered among the conifers. Bunchgrass dominates the forest floor. Non-native trees cultivated in Lytton include black locust and Manitoba Maple.
Lytton lies on the Trans-Canada Highway as well as both the Canadian Pacific and Canadian National Railways. The Canadian National Railway crosses both the Fraser and Thompson Rivers on two large steel bridges at Lytton. Via the Trans-Canada, Lytton is approximately 265 km (165 mi) from the city of Vancouver, 111 km (69 mi) north of Hope, and 84 km (52 mi) south of Cache Creek and Ashcroft.
Highway 12 runs north from Lytton 62 km (39 mi) to Lillooet, connecting there to Highway 99, which leads southwest to Pemberton and Whistler and beyond to Vancouver, and northeast to its terminus at Lower Hat Creek (Carquile) at a junction with Highway 97 just north of Cache Creek.
The Lytton Ferry, a free reaction ferry, crosses the Fraser River at Lytton. On the river's west side are Indian reserve communities of the Lytton First Nation and the Stein Valley Nlaka'pamux Heritage Park via trails from the confluence of the Stein River with the Fraser. From the ferry, a route known as the West Side Road leads through the Nesikep and Texas Creek areas to Lillooet and BC Highway 99; the route south from the ferry is much more difficult but leads to North Bend-Boston Bar. When the ferry is out of service because of ice or low water levels on the Fraser River, pedestrian access is available via a walkway on the Canadian National Railway bridge crossing the river.
Via Rail's Canadian and the Rocky Mountaineer pass through Lytton but do not make any stops. Via Rail's closest stops are Ashcroft, 80 km (50 mi) to the north, and North Bend/Boston Bar, 44 km (27 mi) to the south.
The mayor of Lytton is Denise O'Connor, who was first elected in the 2022 municipal election.
Lytton is a corporate entity created under the Community Charter. Elections for Village Council are held every four years. The current Council comprises the following members:
Originally part of the Lillooet provincial riding, then part of Yale-Lillooet, Lytton is now in the provincial riding of Fraser-Nicola, represented by Jackie Tegart of BC United, who first won in the 2013 election.
Federally, the town is in the riding of Mission—Matsqui—Fraser Canyon and is currently represented by Brad Vis of the Conservative Party of Canada, who was first elected in the 2019 elections.
The single main employer in the village produced forestry products and was forced to close because of market uncertainties in 2007.
Lytton is the self-proclaimed "River Rafting Capital of Canada" with Kumsheen Rafting Resort now the largest employer in the area. A provincial campsite, Skihist Provincial Park, adjacent to the Trans-Canada Highway six kilometres north of the village, has space for tenting as well as RVs and enjoys one of the few views available of Skihist Mountain, the highest summit of the Lillooet Ranges, across the Fraser to the west of Lytton. The privately run Jade Springs Restaurant, also east of the village on the Trans-Canada, burned down in the fire of June 2021.
School District 74 operated Lytton Elementary School which was lost in 2021 Lytton Creek Wildfire. [33] and Kumsheen Secondary School (Kumsheen ShchEma-meet School). [34]
Stein Valley Nlakapamux School is a registered member with the B.C. First Nations Schools Association. The School is mandated to provide instruction and courses approved by the B.C. Ministry of Education and BC Independent Schools.
Lillooet is a district municipality in the Squamish-Lillooet region of southwestern British Columbia. The town is on the west shore of the Fraser River immediately north of the Seton River mouth. On BC Highway 99, the locality is by road about 100 kilometres (62 mi) northeast of Pemberton, 64 kilometres (40 mi) northwest of Lytton, and 172 kilometres (107 mi) west of Kamloops.
Hope is a district municipality at the confluence of the Fraser and Coquihalla rivers in the province of British Columbia, Canada. Hope is at the eastern end of both the Fraser Valley and the Lower Mainland region, and is at the southern end of the Fraser Canyon. To the east, over the Cascade Mountains, is the Interior region, beginning with the Similkameen Country on the farther side of the Allison Pass in Manning Park. Located 154 kilometres (96 mi) east of Vancouver, Hope is at the southern terminus of the Coquihalla Highway and the western terminus of the Crowsnest Highway, locally known as the Hope-Princeton, where they merge with the Trans-Canada Highway. Hope is at the eastern terminus of Highway 7. As it lies at the eastern end of the Fraser Valley in the windward Cascade foothills, the town gets very high amounts of rain and cloud cover – particularly throughout the autumn and winter.
Yale is an unincorporated town in the Canadian province of British Columbia, which grew in importance during the Fraser Canyon Gold Rush.
Yale-Lillooet was a provincial electoral district for the Legislative Assembly of British Columbia, Canada.
The Fraser Canyon is a major landform of the Fraser River where it descends rapidly through narrow rock gorges in the Coast Mountains en route from the Interior Plateau of British Columbia to the Fraser Valley. Colloquially, the term "Fraser Canyon" is often used to include the Thompson Canyon from Lytton to Ashcroft, since they form the same highway route which most people are familiar with, although it is actually reckoned to begin above Williams Lake at Soda Creek Canyon near the town of the same name.
The Fraser Canyon Gold Rush, began in 1858 after gold was discovered on the Thompson River in British Columbia at its confluence with the Nicoamen River a few miles upstream from the Thompson's confluence with the Fraser River at present-day Lytton. The rush overtook the region around the discovery and was centered on the Fraser Canyon from around Hope and Yale to Pavilion and Fountain, just north of Lillooet.
The Lillooet Ranges are the southeasternmost subdivision of the Pacific Ranges of the Coast Mountains of British Columbia. They are located between the drainage of the Lillooet River and Harrison Lake on the west and the canyon of the Fraser River on the east, and by the lowland coastal valley of that river on the south.
The Clear Range is a small mountain range located in the angle of the Fraser and Thompson Rivers in south-central British Columbia, Canada. It has a small subdivision just northeast of that confluence named the Scarped Range. The Clear Range totals 16,270 km2 (6,280 sq mi) and is 75 km (47 mi) north to south and 35 km (22 mi) east to west. The Clear Range and its northward neighbour the Marble Range are both subranges of the Pavilion Range.
Harrison Lake is the largest lake in the southern Coast Mountains of Canada, being about 250 square kilometres (95 mi²) in area. It is about 60 km (37 mi) in length and at its widest almost 9 km (5.6 mi) across. Its southern end, at the resort community of Harrison Hot Springs, is c. 95 km east of downtown Vancouver. East of the lake are the Lillooet Ranges while to the west are the Douglas Ranges. The lake is the last of a series of large north-south glacial valleys tributary to the Fraser along its north bank east of Vancouver, British Columbia. The others to the west are the Chehalis, Stave, Alouette, Pitt, and Coquitlam Rivers. Harrison Lake is a natural lake, not man-made. The lake is supplied primarily from the Lillooet River, which flows into the lake at the northernmost point.
Camchin, also spelled Kumsheen, is an anglicization of the ancient name for the locality and aboriginal village once located on the site of today's village of Lytton, British Columbia, Canada, whose name in Nlaka'pamuctsin is ƛ'q'əmcín. It also refers to the main Indian reserve community of the Lytton First Nation adjacent to the Village of Lytton and is found in the form "Kumsheen" in local business and school names.
Boston Bar is an unincorporated community in the Fraser Canyon of the Canadian province of British Columbia.
Clinton is a village in British Columbia, Canada, located approximately 40 km (25 mi) northwest of Cache Creek and 30 km south of 70 Mile House.
Skihist Mountain, also sometimes referred to as Skihist Peak, is the highest mountain in the Cantilever Range and in southwestern British Columbia, Canada. It is located on the southern boundary of Stein Valley Nlaka'pamux Heritage Park, about 20 km (12 mi) west of Lytton. It is the highest summit in the Lillooet Ranges, which lie between the Lillooet and Fraser Rivers, south of the Gates Valley and Seton and Anderson Lakes.
Fountain is an unincorporated rural area and Indian reserve community in the Fraser Canyon region of British Columbia, Canada, located at the ten-mile (16 km) mark from the town of Lillooet on BC Highway 99, which in that area is also on the route of the Old Cariboo Road and is located at the junction of that route with the old gold rush-era trail via Fountain Valley and the Fountain Lakes.
The Nlakaʼpamux or Nlakapamuk, also previously known as the Thompson, Thompson River Salish, Thompson Salish, Thompson River Indians or Thompson River people, and historically as the Klackarpun, Haukamaugh, Knife Indians, and Couteau Indians, are an Indigenous First Nations people of the Interior Salish language group in southern British Columbia. Their traditional territory includes parts of the North Cascades region of Washington.
The 2021 Western North America heat wave was an extreme heat wave that affected much of Western North America from late June through mid-July 2021. The heat wave affected Northern California, Idaho, Western Nevada, Oregon, and Washington in the United States, as well as British Columbia, and in its latter phase, Alberta, Manitoba, the Northwest Territories, Saskatchewan, and Yukon, all in Canada. It also affected inland regions of Central and Southern California, Nevada, and Montana, though the temperature anomalies were not as extreme as in the regions farther north.
A wildfire began on June 30, 2021 just south of the village of Lytton in the interior of British Columbia, Canada. The fire destroyed much of Lytton and caused two civilian fatalities, announced July 3. Several missing residents, still unaccounted for at that time, were later located. The fire, one of the 2021 British Columbia wildfires throughout the province, was facilitated by the 2021 Western North America heat wave.
Siwhe Mountain is a 2,843-metre (9,327-foot) summit located in British Columbia, Canada.
Kwoiek Peak is a 2,736-metre (8,976-foot) mountain summit located in British Columbia, Canada.
Antimony Mountain is a 2,668-metre (8,753-foot) mountain summit located in British Columbia, Canada.
270 - Seventh Street, PO Box 219, Lytton, BC, V0K 1Z0
PO Box 60, Lytton, BC, V0K 1Z0