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Vancouver Island

Coordinates:49°36′N125°30′W / 49.6°N 125.5°W /49.6; -125.5
From Wikipedia, the free encyclopedia
Largest island in British Columbia, Canada
"Quadra and Vancouver Island" redirects here. For the nearby island named solely after the Spanish explorer, seeQuadra Island.
Not to be confused with the city ofVancouver, located on the mainland.

Vancouver Island
Terra satellite image of Vancouver Island, 2003
Vancouver Island with major cities and towns labelled
Geography
LocationNorth Pacific Ocean, on the coast of southernBritish Columbia
Coordinates49°36′N125°30′W / 49.6°N 125.5°W /49.6; -125.5
Area32,100 km2 (12,400 sq mi)
Area rank11th largest in Canada
43rd largest worldwide
Highest elevation2,195 m (7201 ft)
Highest pointGolden Hinde[1]
Administration
Canada
ProvinceBritish Columbia
Largest settlementSaanich (pop. 117,735, part ofGreater Victoria, 397,237[2])
Demographics
DemonymVancouver Islander
Population864,864[3] (2021)
Pop. density27.64/km2 (71.59/sq mi)

Vancouver Island is an island in the northeasternPacific Ocean and part of the Canadianprovince ofBritish Columbia. The island is 456 km (283 mi) in length, 100 km (62 mi) in width at its widest point,[4] and 32,100 km2 (12,400 sq mi) in total area, while 31,285 km2 (12,079 sq mi) are of land. The island is the largest by area and the most populous[citation needed] along the west coasts of theAmericas.

The southern part of Vancouver Island and some of the nearbyGulf Islands are the only parts of British Columbia orWestern Canada to lie south of the49th parallel. The southeast part of the island has one of the warmest climates in Canada, and since the mid-1990s has been mild enough in a few areas to growMediterranean crops such asolives andlemons.[5]

The population of Vancouver Island was 864,864 as of 2021.[3] Nearly half of that population (~400,000) live in the metropolitan area ofGreater Victoria on the southern tip of the island, which includesVictoria, the capital of British Columbia. Other notable cities and towns on Vancouver Island includeNanaimo,Campbell River,Courtenay,Port Alberni andParksville, all on or near the east coast.

Indigenous peoples have inhabited Vancouver Island for thousands of years,[6] long before the arrival of Spanish and British naval expeditions in the late 18th century. The Spanish and British conjointly named itQuadra's and Vancouver's Island in commemoration of the friendly negotiations held in 1792 between the Spanish commander ofFort San Miguel inNootka Sound,Juan Francisco de la Bodega y Quadra, and British naval captainGeorge Vancouver, during theNootka Crisis. (Bodega y Quadra's name was eventually dropped.) It is one of several North American locations named after George Vancouver, who between1791 and 1794 explored thePacific Northwest.

Vancouver Island is theworld's 43rd largest island,Canada's 11th largest island, andCanada's second most populous island after theIsland of Montreal.

History

[edit]

Indigenous peoples

[edit]
Main article:Indigenous peoples of the Pacific Northwest Coast

Vancouver Island has been the homeland of manyindigenous peoples for thousands of years.[6] The groupings, by language, are theKwakwakaʼwakw (also known as theKwakiutl),Nuu-chah-nulth, and variousCoast Salish peoples. While there is some overlap, Kwakwakaʼwakw territory includes northern and northwestern Vancouver Island and adjoining areas of the mainland, the Nuu-chah-nulth span most of the west coast, while the Coast Salish cover the southeastern Island and southernmost extremities along theStrait of Juan de Fuca. Their cultures are connected to the natural resources abundant in the area.

Kwakwakaʼwakw

[edit]
Main article:Kwakwakaʼwakw
A Kwakwakaʼwakw wedding ceremony in 1914

TheKwakwakaʼwakw today number about 5,500, who live in British Columbia on northern Vancouver Island and the mainland. They are also known asKwakiutl in English, from one of their tribes, but they prefer their autonymKwakwakaʼwakw. Their indigenous language, part of theWakashan family, isKwakʼwala. The name Kwakwakaʼwakw means "speakers of Kwakʼwala". The language is now spoken by less than 5% of the population—about 250 people. Today, 17 separate tribes make up the Kwakwakaʼwakw. Some Kwakwakaʼwakw groups are now extinct. Kwakʼwala is aNorthern Wakashan language, a grouping shared with Haisla, Heiltsuk and Wuikyala. Kwakwakaʼwakw centres of population on Vancouver Island include communities such asFort Rupert,Alert Bay andQuatsino, the Kwakwakaʼwakw tradition of thepotlatch was banned by the federal government of Canada in 1885, but has been revived in recent decades.

Nuu-chah-nulth

[edit]
Main article:Nuu-chah-nulth

TheNuu-chah-nulth (pronounced [nuːʧanˀuɬ]), are indigenous peoples in Canada. Their traditional home is on the west coast of Vancouver Island. In pre-contact and early post-contact times, the number of nations was much greater, but as in the rest of the region,smallpox and other consequences of contact resulted in the disappearance of some groups and the absorption of others into neighbouring groups.

They were among the first Pacific peoples north of California to come into contact with Europeans, as the Spanish, Americans and British attempted to secure control of the Pacific Northwest and the trade in otter pelts, withNootka Sound becoming a focus of these rivalries. The Nuu-chah-nulth speak aSouthern Wakashan language and are closely related to theMakah of theOlympic Peninsula,Washington state and theDitidaht.

Coast Salish

[edit]
Main article:Coast Salish

TheCoast Salish are the largest of the southern groups. They are a loose grouping of many tribes with numerous distinct cultures and historically speak one of theCoast Salish languages. On Vancouver Island, Coast Salish peoples' territory traditionally spans from the northern limit of theStrait of Georgia on the east side of Vancouver Island and covers most of southern Vancouver Island. Distinct nations within the Coast Salish peoples on Vancouver Island include theStz'uminus, theKʼómoks of theComox Valley area, theCowichan of theCowichan Valley, theEsquimalt, theSaanich of theSaanich Peninsula, theSonghees of the Victoria area and theSnuneymuxw in the Nanaimo area.

European exploration

[edit]

Europeans began to explore the island in 1774 when rumours of Russianfur traders caused Spain to send a number of expeditions to assert itslong-held claims to the Pacific Northwest. The first expedition was that of theSantiago, under the command ofJuan José Pérez Hernández. In 1775, a second Spanish expedition under theSpanish Peruvian captainJuan Francisco de la Bodega y Quadra was sent. By 1776, Spanish exploration had reachedBucareli Bay including the mouth of theColumbia River betweenOregon andWashington, andSitka Sound.[7]

Vancouver Island came to the attention of Britain afterthe third voyage of CaptainJames Cook, who spent a month during 1778 atNootka Sound, on the island's western coast. Cook claimed it for Great Britain.Maritime fur trader,John Meares arrived in 1786 and set up a single-buildingtrading post near the native village ofYuquot (Friendly Cove), at the entrance to Nootka Sound in 1788.[8] The fur trade began expanding into the island, eventually leading to permanent settlement.[9]

Dispute over sovereignty

[edit]

The island was further explored by Spain in 1789 withEsteban José Martínez, who established the settlement ofYuquot and the artillery battery ofFort San Miguel atFriendly Cove, which Spain called Puerto de San Lorenzo de Nuca. This was to be the only Spanish settlement, as well as a whaling factory inRed Bay, Labrador, in what would later be Canada. Asserting their claim of exclusive sovereignty and navigation rights, the Spanish force seized thePortuguese-flagged British ships.[8]

British naval captainGeorge Vancouver was sent to Nootka Sound in 1792 in order to negotiate a settlement. His Spanish counterpart in the negotiations was Juan Francisco de la Bodega y Quadra, who was commandant ofSanta Cruz de Nuca in 1792. Vancouver had sailed as a midshipman with Cook. The negotiations between Vancouver and Bodega y Quadra ended in a deadlock with nothing resolved. Vancouver insisted the entire Spanish establishment be turned over, but Bodega y Quadra held that there were no buildings seized in 1789, and the only possible land was a tiny and useless cove nearby. The two decided to refer the entire matter back to their respective governments. The friendly meeting between Bodega y Quadra and Vancouver led the former to propose that the island be named after both: "Quadra and Vancouver Island", which became the original name. While we know this island today as "Vancouver Island", the British explorer had not intentionally meant to name such a large body of land solely after himself.[10] In his September 1792 dispatch log report for the British Admiralty, Captain Vancouver reveals that his decision here was rather meant to honour a request by Bodega y Quadra that Vancouver:

would name some port or island after us both in commemoration of our meeting and friendly intercourse that on that occasion had taken place (Vancouver had previously feted Bodega y Quadra on his ship); ...and conceiving no place more eligible than the place of our meeting, I have therefore named this land ... The Island of Quadra and Vancouver.[11]

Bodega y Quadra wrote, however, that it was Vancouver who made the suggestion of combining their names to designate some geographical feature.[12]

Dionisio Alcalá Galiano was the first European to circumnavigate Vancouver Island

In 1792, the Spanish explorerDionisio Alcalá Galiano and his crew were the first Europeans to circumnavigate Vancouver Island.[13] On April 8, 1806, CaptainJohn D'Wolf ofBristol, Rhode Island, sailed theJuno toNahwitti (Newettee), a small inlet in the northwestern promontory of Vancouver's Island. The captain described Newettee as one of the southernmost harbours frequented by American fur traders at51 degrees north and128 degrees west. He relates that since CaptainRobert Gray ofTiverton, Rhode Island, had sailed theColumbia River in 1792, the trade of the northwest coast had been almost entirely in the hands of Boston merchants, so much so that the natives called all traders "Boston Men".[14]

A settlement was not successfully negotiated and ownership of the island remained in dispute between theKingdom of Great Britain and theSpanish Empire in the early 1790s. The two countries nearly began a war over the issue; the confrontation became known as theNootka Crisis. That was averted when both agreed to recognize the other's rights to the area in the firstNootka Convention in 1790, a first step to peace.[15] Finally, the two countries signed the second Nootka Convention in 1793 and the third Convention in 1794. As per that final agreement, the Spanish dismantled their fort at Nootka and left the area, giving the British sovereignty over Vancouver Island and the adjoining islands (including theGulf Islands).[8]

For decades,Quadra's and Vancouver's Island was the most prominent name on maps of the coast, and appeared on most British, French and Spanish maps of the period. But as Spanish interests in the region dwindled, so did the use of Bodega y Quadra's name. TheHudson's Bay Company played a major part in the transition; by 1824 'Vancouver's Island' had become the usual designation in its correspondence for the island.[16]

A quarter of a century later, Vancouver Island had become such a well-known geographical feature that the founding of theColony of Vancouver Island in 1849 gave this name full official status.[17] Period references to "Vancouver" referred to Vancouver Island until the naming of the city of Vancouver in 1885.

British settlement

[edit]
The Great Seal of the Island of Vancouver and its Dependencies was designed byBenjamin Wyon, Chief Engraver of Her Majesty's Seals, c. 1849. The symbolic badge he designed was the basis for the flag of Vancouver Island, which is still unofficially flown today.[18]
Theflag of Vancouver Island was authorized in 1865 (colonies could place their badges upon the fly of a blue ensign). This flag uses the Colonial Seal of Vancouver Island from 1849. The flag was probably never actually flown in colonial times but is used today as an unofficial representative flag.[19]

By March 1843, James Douglas of the Hudson's Bay Company and a missionary had arrived and selected an area for settlement. Construction of the fort began in June of that year.[9] This settlement was afur trading post originally named Fort Albert (afterwardFort Victoria). The fort was located at theSonghees settlement of Camosack (Camosun), 200 m (660 ft) northwest of the present-dayEmpress Hotel onVictoria's Inner Harbour.

In 1846, theOregon Treaty, which ended theOregon boundary dispute, was signed by the British and the United States to settle the question of the U.S.Oregon Country borders.[20] The Treaty made the 49th parallel latitude north the official border between the two countries. In order to ensure that Britain retained all of Vancouver Island and the southern Gulf Islands, however, it was agreed that the border would swing south around that area.[21]

In 1849, theColony of Vancouver Island was established. The Colony was leased to the Hudson's Bay Company (HBC) for an annual fee of seven shillings; the company's responsibility in return was to increase the population by promoting colonization. The first independent settler arrived that year: Captain Walter Grant started a homestead inSooke. Following the brief governorship ofRichard Blanshard,James Douglas,Chief Factor of the Hudson's Bay post, assumed the role in 1851.

The island's first legislative assembly was formed in 1856.[22] Government buildings were built and were occupied in 1859; the replacement, today'sParliament Buildings, were opened in 1898.[9]

Fort Victoria had become an important base when prospectors, miners and merchants began arriving for theFraser Canyon Gold Rush in 1858. The Hudson's Bay lease expired in 1859 and the island reverted to Great Britain. The burgeoning town was incorporated as Victoria in 1862. Victoria became the capital of the colony of Vancouver Island, retaining this status when the island was amalgamated with the mainland in 1866.[9]

A British naval base, includingEsquimalt Royal Navy Dockyard and a naval hospital, was established atEsquimalt in 1865 and eventually taken over by theCanadian military.[22] Today, asCFB Esquimalt, it is the home port of theMaritime Forces Pacific and parts are designated asNational Historic Sites of Canada.

Union and Confederation

[edit]

The economic situation of the colony declined following theCariboo Gold Rush of 1861–1862, and pressure grew for amalgamation of the colony with the mainlandcolony of British Columbia (which had been established in 1858). The two colonies were merged in 1866 into theUnited Colonies of Vancouver Island and British Columbia by the Act for the Union of the colonies, passed by theImperial Parliament.[9]Arthur Kennedy was appointed governor of the united entity. (He would leave office in 1866 and later became Governor of the West African Settlements,British West Africa.)[23] Victoria became the capital but the legislative assembly was located inNew Westminster on theLower Mainland. The capital was moved to Victoria in 1868.[9]

Confederation

[edit]

By 1867,Canada was established by the first of theBritish North America Acts, theConstitution Act, 1867 and the United Colonies joined Canada on 20 July 1871 through theBritish Columbia Terms of Union, following negotiations that secured the interests of the colonial elite in relation to a rail connection that would unite the colonies with the rest of Canada, establish Indian lands policy that would effectively perpetuate BC's pre-Confederation practices, and enshrine colonial officials' security of position.[24] Victoria was named the capital of the province ofBritish Columbia. Three delegates were appointed to the federal government.[22][9]

Geography

[edit]
Topographic map of Vancouver Island

Vancouver Island is located in the southwestern corner of the province of British Columbia. It is separated from the mainland of British Columbia byJohnstone Strait andQueen Charlotte Strait on the north and northeast, and by theStrait of Georgia on the southeast, which along with theStrait of Juan de Fuca along its southwest separate it from the United States.[25] West of the island is the open Pacific Ocean, while to its north isQueen Charlotte Sound.[26] TheStraits of Georgia andJuan de Fuca are now officially part of theSalish Sea, which also includesPuget Sound.[27]

TheVancouver Island Ranges run most of the length of the island, dividing it into a wet and rugged west coast and a drier, more rolling east coast. The highest point in these ranges and on the island is theGolden Hinde, at 2,195 m (7,201 ft).[28] Located near the centre of Vancouver Island in 2,500 km2 (970 sq mi)Strathcona Provincial Park, it is part of a group of peaks that include the only glaciers on the island, the largest of which is theComox Glacier.[29] The west coast shoreline is rugged and in many places mountainous, characterized by its manyfjords, bays, and inlets. The interior of the island has many lakes (Kennedy Lake, north ofUcluelet, is the largest) and rivers.[30]

The49th parallel north crosses the island just north ofLadysmith on the east and Ucluelet on the west, while the50th parallel north passes through Campbell River.

Southern Vancouver Island is typically considered to refer to the area south ofCourtenay, whileNorthern Vancouver Island, or the northern region of the island, begins in the area an hour north ofCampbell River towardsSayward.[31] Those cities and the area between Southern and Northern Vancouver Island, such asNanaimo,Parksville,Qualicum Beach,Deep Bay, andPort Alberni, make up the Central Island region".[32]

Lakes

[edit]

Rivers

[edit]
Main article:List of rivers of British Columbia § Rivers of Vancouver Island

There are a number of rivers draining the island, some of which though short are large in volume. Among the more notable rivers are theSomass River in theAlberni Valley, theNimpkish River in the North Island region, theEnglishman River up island from Nanaimo nearParksville, and theCowichan River whose basin forms theCowichan Valley region in the South Island region.

Climate

[edit]
Köppen climate types in Vancouver Island and the Gulf Islands

The climate of Vancouver Island is the mildest in Canada, with temperatures on the coast even in January being usually above 0 °C (32 °F). In summer, the warmest days usually have a maximum of 28–33 °C (82–91 °F). The southeastern part of the island notably has a warm summer (Csb)Mediterranean climate with numerousvineyards.

Therain shadow effect of the island's mountains, as well as the mountains ofWashington'sOlympic Peninsula, creates wide variation in precipitation. The west coast is considerably wetter than the east coast. Average annual precipitation ranges from 6,650 mm (262 in) atHucuktlis Lake on the west coast (making it the wettest place in North America) to only 608 mm (23.9 in) at Victoria Gonzales, the driest recording station in the provincial capital ofVictoria. Precipitation is heaviest in the autumn and winter. Snow is rare at low altitudes, but is common on the island's mountaintops in winter. Skiing is popular atMount Washington in the mid-island, with an elevation of 1,588 m (5,210 ft).

A notable feature of Vancouver Island is the extension of summer dryness to latitudes as high as50 °N. Only in the extreme north of the island nearPort Hardy is the rainfall of the driest summer month as much asone fifth that of the wettest months from November to March. West coasts of other continents at similar latitudes have a practically even distribution of rainfall throughout the year.

Climate data forPort Renfrew
Climate ID: 1016335; coordinates48°35′30″N124°19′35″W / 48.59167°N 124.32639°W /48.59167; -124.32639 (Port Renfrew); elevation: 10.0 m (32.8 ft); 1981-2010 normals
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °C (°F)19.0
(66.2)
16.5
(61.7)
20.0
(68.0)
24.5
(76.1)
27.5
(81.5)
31.0
(87.8)
31.7
(89.1)
33.5
(92.3)
28.9
(84.0)
24.0
(75.2)
17.2
(63.0)
15.0
(59.0)
33.5
(92.3)
Mean daily maximum °C (°F)6.3
(43.3)
7.5
(45.5)
9.7
(49.5)
12.3
(54.1)
15.2
(59.4)
17.4
(63.3)
19.4
(66.9)
20.0
(68.0)
17.8
(64.0)
12.9
(55.2)
8.5
(47.3)
5.9
(42.6)
12.7
(54.9)
Daily mean °C (°F)4.1
(39.4)
4.6
(40.3)
6.2
(43.2)
8.4
(47.1)
11.1
(52.0)
13.4
(56.1)
15.3
(59.5)
15.6
(60.1)
13.4
(56.1)
9.6
(49.3)
6.1
(43.0)
3.8
(38.8)
9.3
(48.7)
Mean daily minimum °C (°F)1.8
(35.2)
1.6
(34.9)
2.7
(36.9)
4.3
(39.7)
6.9
(44.4)
9.4
(48.9)
11.0
(51.8)
11.1
(52.0)
9.0
(48.2)
6.3
(43.3)
3.7
(38.7)
1.6
(34.9)
5.8
(42.4)
Record low °C (°F)−12.5
(9.5)
−10.5
(13.1)
−6.7
(19.9)
−2.5
(27.5)
0.0
(32.0)
1.7
(35.1)
5.0
(41.0)
2.2
(36.0)
−0.6
(30.9)
−3.5
(25.7)
−11.5
(11.3)
−11.1
(12.0)
−12.5
(9.5)
Averageprecipitation mm (inches)555.7
(21.88)
376.6
(14.83)
362.3
(14.26)
258.7
(10.19)
154.7
(6.09)
107.9
(4.25)
50.5
(1.99)
82.4
(3.24)
123.9
(4.88)
371.2
(14.61)
579.7
(22.82)
481.0
(18.94)
3,504.6
(137.98)
Average rainfall mm (inches)544.0
(21.42)
362.0
(14.25)
356.0
(14.02)
258.1
(10.16)
154.6
(6.09)
107.9
(4.25)
50.5
(1.99)
82.4
(3.24)
123.9
(4.88)
371.0
(14.61)
575.4
(22.65)
468.9
(18.46)
3,454.7
(136.01)
Average snowfall cm (inches)11.8
(4.6)
14.6
(5.7)
6.3
(2.5)
0.6
(0.2)
0.1
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.2
(0.1)
4.3
(1.7)
12.1
(4.8)
50.0
(19.7)
Average precipitation days(≥ 0.2 mm)22.818.422.319.316.713.99.09.611.118.823.122.4207.3
Average rainy days(≥ 0.2 mm)22.117.822.019.316.713.99.09.611.118.822.821.5204.7
Average snowy days(≥ 0.2 cm)2.92.22.00.330.040.00.00.00.00.081.02.511.1
Source:Environment and Climate Change Canada[33]
Climate data forUniversity of Victoria (Oak Bay /Saanich)
WMO ID: 71783; coordinates48°27′25″N123°18′17″W / 48.45694°N 123.30472°W /48.45694; -123.30472 (University of Victoria); elevation: 60.1 m (197 ft); 1991–2020 normals
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record highhumidex19.616.621.925.331.341.940.435.033.431.120.520.940.4
Record high °C (°F)15.2
(59.4)
16.5
(61.7)
21.0
(69.8)
25.0
(77.0)
28.8
(83.8)
37.9
(100.2)
37.6
(99.7)
34.5
(94.1)
30.2
(86.4)
23.5
(74.3)
19.0
(66.2)
16.5
(61.7)
37.6
(99.7)
Mean daily maximum °C (°F)8.2
(46.8)
8.8
(47.8)
11.0
(51.8)
14.0
(57.2)
17.9
(64.2)
20.6
(69.1)
23.7
(74.7)
23.5
(74.3)
20.0
(68.0)
14.3
(57.7)
10.3
(50.5)
8.0
(46.4)
15.0
(59.0)
Daily mean °C (°F)5.8
(42.4)
5.9
(42.6)
7.5
(45.5)
9.8
(49.6)
12.9
(55.2)
15.4
(59.7)
17.7
(63.9)
17.7
(63.9)
15.0
(59.0)
10.7
(51.3)
7.6
(45.7)
5.5
(41.9)
11.0
(51.8)
Mean daily minimum °C (°F)3.4
(38.1)
2.9
(37.2)
3.9
(39.0)
5.5
(41.9)
7.9
(46.2)
10.2
(50.4)
11.7
(53.1)
11.8
(53.2)
10.1
(50.2)
7.2
(45.0)
4.7
(40.5)
3.1
(37.6)
6.9
(44.4)
Record low °C (°F)−11.7
(10.9)
−7.2
(19.0)
−4.1
(24.6)
−0.6
(30.9)
0.2
(32.4)
5.1
(41.2)
6.2
(43.2)
7.2
(45.0)
3.6
(38.5)
−2.1
(28.2)
−9.5
(14.9)
−11.2
(11.8)
−11.2
(11.8)
Record lowwind chill−15.4−11.8−9.0−1.70.00.00.00.00.0−3.3−12.4−14.5−15.4
Averageprecipitation mm (inches)109.6
(4.31)
59.6
(2.35)
52.6
(2.07)
35.6
(1.40)
29.2
(1.15)
19.7
(0.78)
10.7
(0.42)
15.6
(0.61)
30.4
(1.20)
77.2
(3.04)
123.2
(4.85)
97.8
(3.85)
661.2
(26.03)
Average precipitation days(≥ 0.2 mm)18.715.117.213.211.29.14.85.211.117.821.419.3164.0
Averagerelative humidity (%)(at 1500LST)83.375.570.563.860.858.055.557.865.776.681.982.869.3
Source:Environment and Climate Change Canada[34]
Climate data forNorth Saanich (Victoria International Airport)
WMO ID: 1018620; coordinates48°38′50″N123°25′33″W / 48.64722°N 123.42583°W /48.64722; -123.42583 (Victoria International Airport); elevation: 19.5 m (64 ft); 1991–2020 normals, extremes 1940–present
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record highhumidex17.417.121.126.133.634.739.636.834.727.020.017.742.6
Record high °C (°F)16.1
(61.0)
18.3
(64.9)
21.4
(70.5)
26.3
(79.3)
31.5
(88.7)
39.4
(102.9)
36.3
(97.3)
34.4
(93.9)
31.2
(88.2)
27.6
(81.7)
18.3
(64.9)
16.1
(61.0)
39.4
(102.9)
Mean daily maximum °C (°F)7.5
(45.5)
8.7
(47.7)
10.8
(51.4)
13.7
(56.7)
17.5
(63.5)
20.2
(68.4)
22.7
(72.9)
22.6
(72.7)
19.7
(67.5)
14.3
(57.7)
9.9
(49.8)
7.3
(45.1)
14.6
(58.3)
Daily mean °C (°F)4.6
(40.3)
5.0
(41.0)
6.8
(44.2)
9.1
(48.4)
12.6
(54.7)
15.2
(59.4)
17.2
(63.0)
17.1
(62.8)
14.5
(58.1)
10.2
(50.4)
6.5
(43.7)
4.4
(39.9)
10.3
(50.5)
Mean daily minimum °C (°F)1.6
(34.9)
1.4
(34.5)
2.7
(36.9)
4.6
(40.3)
7.6
(45.7)
10.1
(50.2)
11.7
(53.1)
11.6
(52.9)
9.2
(48.6)
6.0
(42.8)
3.0
(37.4)
1.5
(34.7)
5.9
(42.6)
Record low °C (°F)−15.6
(3.9)
−15.0
(5.0)
−10.0
(14.0)
−3.9
(25.0)
−1.1
(30.0)
2.1
(35.8)
4.1
(39.4)
4.4
(39.9)
−1.1
(30.0)
−4.4
(24.1)
−13.3
(8.1)
−14.4
(6.1)
−15.6
(3.9)
Record lowwind chill−19.1−23.7−13.9−6.7−5.30.00.00.00.0−9.1−19.4−25.1−25.1
Averageprecipitation mm (inches)155.3
(6.11)
84.5
(3.33)
79.9
(3.15)
48.2
(1.90)
36.5
(1.44)
29.2
(1.15)
19.5
(0.77)
24.2
(0.95)
35.7
(1.41)
96.1
(3.78)
146.0
(5.75)
146.1
(5.75)
901.2
(35.48)
Average rainfall mm (inches)144.2
(5.68)
78.5
(3.09)
76.3
(3.00)
47.7
(1.88)
36.5
(1.44)
29.2
(1.15)
19.5
(0.77)
24.2
(0.95)
35.7
(1.41)
95.9
(3.78)
141.8
(5.58)
137.0
(5.39)
866.6
(34.12)
Average snowfall cm (inches)11.2
(4.4)
7.1
(2.8)
3.7
(1.5)
0.5
(0.2)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.2
(0.1)
3.6
(1.4)
12.4
(4.9)
38.6
(15.2)
Average precipitation days(≥ 0.2 mm)19.815.217.013.711.69.55.45.58.014.118.919.4158.1
Average rainy days(≥ 0.2 mm)18.914.516.813.711.69.55.45.58.014.018.519.0155.5
Average snowy days(≥ 0.2 cm)2.01.61.20.10.00.00.00.00.00.00.91.77.4
Averagerelative humidity (%)(at 1500LST)78.469.965.360.558.456.355.456.460.769.776.679.365.6
Mean monthlysunshine hours70.895.5145.3191.3241.5251.7318.1297.5228.6136.972.858.92,108.8
Percentagepossible sunshine2633.339.546.751.252.265.466.960.340.726.222.744.3
Source:Environment and Climate Change Canada[35] (June maximum)[36] (sun 1981–2010)[37]
Climate data forComox (Comox Airport)
WMO ID: 71893; coordinates49°43′N124°54′W / 49.717°N 124.900°W /49.717; -124.900 (Comox Airport); elevation: 25.6 m (84 ft); 1991–2020 normals, extremes 1991–present
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record highhumidex16.215.819.626.231.637.340.440.333.726.020.917.740.4
Record high °C (°F)16.7
(62.1)
16.3
(61.3)
19.6
(67.3)
26.8
(80.2)
31.7
(89.1)
38
(100)
35.2
(95.4)
33.6
(92.5)
31.7
(89.1)
22.9
(73.2)
17.8
(64.0)
17.4
(63.3)
35.2
(95.4)
Mean daily maximum °C (°F)6.3
(43.3)
7.2
(45.0)
9.5
(49.1)
12.9
(55.2)
17.2
(63.0)
19.9
(67.8)
23.1
(73.6)
23.0
(73.4)
19.1
(66.4)
12.9
(55.2)
8.7
(47.7)
6.2
(43.2)
13.8
(56.8)
Daily mean °C (°F)3.9
(39.0)
4.2
(39.6)
6.1
(43.0)
9.0
(48.2)
12.9
(55.2)
15.7
(60.3)
18.5
(65.3)
18.3
(64.9)
14.8
(58.6)
9.6
(49.3)
5.9
(42.6)
3.7
(38.7)
10.2
(50.4)
Mean daily minimum °C (°F)1.5
(34.7)
1.2
(34.2)
2.6
(36.7)
5.0
(41.0)
8.6
(47.5)
11.5
(52.7)
13.7
(56.7)
13.5
(56.3)
10.5
(50.9)
6.3
(43.3)
3.1
(37.6)
1.3
(34.3)
6.6
(43.9)
Record low °C (°F)−21.1
(−6.0)
−16.1
(3.0)
−13.9
(7.0)
−4.4
(24.1)
−2.8
(27.0)
0.5
(32.9)
5.0
(41.0)
3.3
(37.9)
−1.7
(28.9)
−4.8
(23.4)
−13.3
(8.1)
−15.0
(5.0)
−21.1
(−6.0)
Record lowwind chill−18.6−21.6−16.1−5.9−2.00.00.00.0−2.7−9.8−20.3−25.0−25.0
Averageprecipitation mm (inches)177.4
(6.98)
111.6
(4.39)
107.5
(4.23)
64.1
(2.52)
40.3
(1.59)
41.8
(1.65)
23.8
(0.94)
31.2
(1.23)
46.7
(1.84)
125.4
(4.94)
188.8
(7.43)
193.6
(7.62)
1,152.2
(45.36)
Average rainfall mm (inches)165.1
(6.50)
102.6
(4.04)
98.4
(3.87)
64.1
(2.52)
40.3
(1.59)
41.8
(1.65)
23.8
(0.94)
31.2
(1.23)
46.7
(1.84)
125.3
(4.93)
183.5
(7.22)
177.3
(6.98)
1,099.9
(43.30)
Average snowfall cm (inches)12.4
(4.9)
9.0
(3.5)
6.8
(2.7)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.1
(0.0)
5.5
(2.2)
16.9
(6.7)
50.8
(20.0)
Average precipitation days(≥ 0.2 mm)19.916.216.913.911.611.27.17.09.817.119.721.2171.6
Average rainy days(≥ 0.2 mm)18.915.016.313.911.611.27.17.09.817.019.420.2167.5
Average snowy days(≥ 0.2 cm)2.42.31.60.070.00.00.00.00.00.100.832.710.0
Averagerelative humidity (%)(at 1500LST)83.876.570.463.861.560.257.357.662.875.881.383.469.5
Mean monthlysunshine hours57.887.6125.2182.5230.7230.1300.0268.8226.9116.357.641.41,925.8
Percentagepossible sunshine21.630.734.044.348.547.461.160.159.834.721.016.340.0
Source:Environment and Climate Change Canada[38] (sun 1981–2010)[39]
Climate data forEstevan Point

WMO ID: 71894; coordinates49°23′00″N126°32′35″W / 49.38333°N 126.54306°W /49.38333; -126.54306 (Estevan Point CS); elevation: 5.8 m (19 ft); 1991–2020 normals, extremes 1908–present
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record highhumidex14.216.118.822.524.229.631.028.132.424.118.114.932.4
Record high °C (°F)17.2
(63.0)
17.2
(63.0)
21.0
(69.8)
22.0
(71.6)
26.0
(78.8)
30.5
(86.9)
28.9
(84.0)
27.5
(81.5)
26.5
(79.7)
21.1
(70.0)
22.0
(71.6)
15.0
(59.0)
30.5
(86.9)
Mean daily maximum °C (°F)8.2
(46.8)
8.6
(47.5)
9.5
(49.1)
11.4
(52.5)
14.0
(57.2)
15.8
(60.4)
17.4
(63.3)
17.8
(64.0)
16.7
(62.1)
13.2
(55.8)
10.2
(50.4)
8.2
(46.8)
12.6
(54.7)
Daily mean °C (°F)5.9
(42.6)
6.0
(42.8)
6.7
(44.1)
8.4
(47.1)
11.1
(52.0)
13.1
(55.6)
14.6
(58.3)
14.9
(58.8)
13.7
(56.7)
10.6
(51.1)
7.6
(45.7)
5.9
(42.6)
9.9
(49.8)
Mean daily minimum °C (°F)3.6
(38.5)
3.2
(37.8)
3.7
(38.7)
5.3
(41.5)
8.1
(46.6)
10.3
(50.5)
11.8
(53.2)
12.1
(53.8)
10.8
(51.4)
7.9
(46.2)
5.0
(41.0)
3.4
(38.1)
7.1
(44.8)
Record low °C (°F)−13.9
(7.0)
−10.6
(12.9)
−7.8
(18.0)
−3.3
(26.1)
0.0
(32.0)
2.8
(37.0)
4.4
(39.9)
5.0
(41.0)
−1.1
(30.0)
−4.4
(24.1)
−9.5
(14.9)
−11.7
(10.9)
−13.9
(7.0)
Record lowwind chill−16.3−11.5−12.2−5.70.00.00.00.00.0−5.3−14.4−18.4−18.4
Averageprecipitation mm (inches)445.3
(17.53)
288.4
(11.35)
299.1
(11.78)
256.8
(10.11)
133.7
(5.26)
119.0
(4.69)
74.3
(2.93)
112.2
(4.42)
161.6
(6.36)
335.1
(13.19)
454.4
(17.89)
430.7
(16.96)
3,110.5
(122.46)
Average rainfall mm (inches)443.0
(17.44)
284.2
(11.19)
295.4
(11.63)
255.9
(10.07)
133.7
(5.26)
119.0
(4.69)
74.3
(2.93)
112.2
(4.42)
161.6
(6.36)
335.1
(13.19)
453.3
(17.85)
429.2
(16.90)
3,097
(121.93)
Average snowfall cm (inches)2.3
(0.9)
4.2
(1.7)
3.7
(1.5)
0.8
(0.3)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
1.0
(0.4)
1.5
(0.6)
13.5
(5.3)
Average precipitation days(≥ 0.2 mm)23.519.822.220.515.115.210.912.414.421.323.524.2222.9
Average rainy days(≥ 0.2 mm)23.119.422.020.415.115.210.912.414.421.323.424.0221.7
Average snowy days(≥ 0.2 cm)0.931.31.10.390.040.00.00.00.00.00.360.624.7
Averagerelative humidity (%)(at 1500LST)87.880.680.079.377.880.381.984.184.686.085.988.283.0
Mean monthlysunshine hours61.983.1115.7158.3206.2205.6232.9200.5170.5114.862.157.61,669.2
Percentagepossible sunshine23.029.131.538.543.442.347.644.945.034.222.622.535.4
Source:Environment and Climate Change Canada[40] (June maximum)[41] (sun 1981–2010)[42]

Geology

[edit]
See also:Insular Belt
The centre of Vancouver Island contains high mountains, such asGolden Hinde.

Vancouver Island is mostly made up ofvolcanic andsedimentary rock which were formed offshore on the now disappearedKulaoceanic plate. Around 55 million years ago during thePaleogene Period, amicroplate of the Kula Platesubducted below theNorth Americancontinental margin with great strain. Avolcanic arc on the surface of the Kula Plate was thusaccreted and fused onto the western edge of North America. Theseterranes were subjected to extreme warping from continued subduction of the Kula plate, leading to the formation of the distortedInsular Mountains. Much of the central mountainous region aroundStrathcona Park is part of theKarmutsen Formation, which is a sequence oftholeiiticpillow basalts andbreccias. Since Vancouver Island has become anaccretionary wedge on the North American continent, the Kula Plate has fully subducted beneath it and the remnants of theFarallon Plate, theJuan de Fuca Plate, are now subducting below the island. This process has led to Vancouver Island being one of the most seismically active regions in Canada. TheCascadia subduction zone off the coast of the island forms a section of theRing of Fire. The area has been known to hostmegathrust earthquakes in the past, the last being theCascadia earthquake of 1700. TheForbidden Plateau, in the east of theVancouver Island Ranges, was theepicentre of the1946 Vancouver Island earthquake that registered 7.3 on themoment magnitude scale, the strongest ever recorded on land in Canada.[43]

Vancouver Island was the location of the observation of theepisodic tremor and slip (ETS) seismic phenomenon.

Ecology

[edit]
The western side of Vancouver Island hosts a rainforest.

Vancouver Island lies in thetemperate rainforestbiome. On the southern and eastern portions of the island, this is characterized byDouglas fir,western red cedar,arbutus (or madrone),Garry oak,salal,Oregon grape, andmanzanita; moreover, Vancouver Island is the location where the Douglas fir was first recorded byArchibald Menzies.[44] Vancouver Island is also the location where some of the tallest Douglas fir were recorded. This southeastern portion of the island is the most heavily populated region of Vancouver Island and a major area for recreation. The northern, western, and most of the central portions of the island are home to theconiferous "big trees" associated with British Columbia's coast –western hemlock,western red cedar,Pacific silver fir,yellow cedar,Douglas fir,grand fir,Sitka spruce, andwestern white pine. It is also characterised bybigleaf maple,red alder,sword fern, andred huckleberry.

View from Mount Maguire inEast Sooke Regional Park towards Washington

The fauna of Vancouver Island is similar to that found on the mainland coast, with some notable exceptions and additions. For example,mountain goats,moose,coyotes,porcupines,skunks,chipmunks, and numerous species of small mammals, while plentiful on the mainland, are absent from Vancouver Island.Grizzly bears are absent from the island, whereblack bears are prevalent, but in 2016, a pair of grizzlies were sighted swimming between smaller islands off the coast nearPort McNeill.[45] Vancouver Island does support most of Canada'sRoosevelt elk, however, and several mammal species and subspecies, such as theVancouver Island marmot are unique to the island.Columbian black-tailed deer are plentiful, even in suburban areas such as inGreater Victoria, as well as the nativeDouglas squirrels. TheEastern grey squirrel is found in the south and is considered invasive for its voracious appetite and scaring away of the Douglas squirrels. The island has the most concentrated population ofcougars in North America. TheVancouver Island wolf, asubspecies of grey wolf, is found only on the north part of the island.[46]Harbour seals andriver otters are common.

Northern resident orcaSpringer with her first calf in 2013.

Residentorcas live in two major groups,one in the waters of the south island andone in the north, while a third group oftransient orcas roam much farther and avoid the resident orcas. Residents are watched from a distance and are numbered, with many being named as well.Humpback whales andgrey whales are often seen on their migration betweenAlaskan waters where they feed in the summer and southern waters such as aroundCalifornia andMexico where they give birth in the winter.

The island's rivers, lakes, and coastal regions are renowned for their fisheries oftrout,salmon, andsteelhead.

Humpback whale off the coast of Sooke

After near-total extirpation by fur traders in the 18th and 19th centuries,sea otters (Enhydra lutris) were protected by an international treaty in 1911. Despite protection, the remnant population off Vancouver Island died out with the last sea otter taken nearKyuquot in 1929. From 1969 to 1972, 89 sea otters were flown or shipped from Alaska to the west coast of Vancouver Island. This population expanded to over 3,000 as of 2005[update], and their range on the island's west coast expanded fromCape Scott in the north toBarkley Sound to the south.[47]

Demographics

[edit]

The majority of Vancouver Island's population lives in theCapital Regional District, more specifically in theprimate city and the provincial capital ofVictoria. With a population of 397,237 (2021),Greater Victoria is the island's largest population centre and one of its twocensus metropolitan areas. The island's other metropolitan area isNanaimo, which has a population of 115,459 as of 2021.[48] There are also five census agglomeration areas (Alberni Valley,Campbell River,Comox Valley,Cowichan Valley, andOceanside) as defined byStatistics Canada.

 
Largest population centres of Vancouver Island
According to the 2021 Census[49]
RankCity nameRegional districtPop.

Victoria


Nanaimo

1VictoriaCapital397,237
Courtenay


Duncan

2NanaimoNanaimo115,459
3CourtenayComox Valley63,282
4DuncanCowichan Valley47,582
5Campbell RiverStrathcona40,704
6ParksvilleNanaimo31,054
7Port AlberniAlberni-Clayoquot25,786
8LadysmithCowichan Valley15,501

Economy

[edit]

Technology

[edit]
Long Beach, Tofino

Within the island's largest city,Victoria, there is a significant IT and technology industry. According to the Victoria Advanced Technology Council website, over 800 technology companies operate in the Victoria area, with combined annual revenues of $1.95 billion.[50]

High-speed internet is delivered to the island byShaw Communications,Telus, and various local providers with their own networks. Wireless Internet connections can be found all over the island, many free for public use.

The island generates much of its own power at several hydroelectric stations, but increased demand has required the construction of severalhigh-voltage power cables, both HVDC and AC, connecting to the Canadian Mainland since 1968.[51]

Logging

[edit]
Fireworks on August 15th at the Tofino pier

Outside of Victoria, Vancouver Island's economy is largely dominated by theforestry industry. Many of thelogging operations are for export, although, historically, were for sawn lumber and pulp and paper operations. Recently, rotations are much shorter than the historical 80 years. Logging operations involvingold-growth forests such as those found inClayoquot Sound are controversial and, due to theClayoquot protests, gained international attention through the efforts ofactivists andenvironmental organizations. Another source of controversy all over the island are logging operations occurring in community watersheds.[52]

Fishing

[edit]

Fishing plays a large role in the lives of many islanders.Commercial fishing vessels operate out of the island's ports and harbours, and coastalfish farms produce many tons ofAtlantic salmon yearly.[53][54][55]

Tourism

[edit]
Campsite at Mystic Beach

In recent years the government of British Columbia has engaged in anadvertising program to draw more tourists to beach resorts in places such asTofino andUcluelet. Sport fishing,whale watching, hiking,scuba diving, surfing, and skiing are just a few things for which tourists visit Vancouver Island. Visitors also come to see Victoria's 19th-century architecture, and the many villages which line the coast such asCowichan Bay,Chemainus, andQualicum Beach. The cities of Victoria and Nanaimo also draw large numbers of visitors, and in 2022 the Vancouver Island tourism region generated $3.2 billion of gross spending in the region, accounting for approximately 18% of BC's total overnight spending.[56]

Food products

[edit]

Consumer food products companies also exist in the various cities and towns on Vancouver Island. Bakeries, dairies, food processing plants, breweries, wineries, of varying size and scope, are found all along the island. Some of these organizations have international customer reach.

Agriculture is confined primarily to the fertile soils found in low-lying areas on the southern and eastern portions of the island. Those areas have the best climate for agricultural production. The total amount of farmland area on Vancouver Island in 2021 was over 41,000 hectares (100,000 acres).[57]

Education

[edit]

Vancouver Island is home to a handful of universities, several colleges and trade-schools, hundreds of public schools, and a few dozen private schools (includingMontessori andWaldorf schools).

Universities

[edit]

Colleges

[edit]

Public school districts

[edit]

There are 12 school districts on Vancouver Island with several elementary, junior high, and high schools in each. Three school districts are in the Greater Victoria area and the other eight cover the rest of the island to the north. All public schooling falls under the jurisdiction of the British Columbia Ministry of Education.

Transport

[edit]

Sea

[edit]
See also:Vancouver Island fixed link

Marine transport is very important to Vancouver Island for access to the mainland of British Columbia and Washington. There are no bridges or tunnels connecting the island to the mainland, although the idea of building one has been brought up many times. Major technical issues and cost are the largest barriers to a fixed link currently,[58][59] though exact public support for the idea is not currently known. The only vehicle access to Vancouver Island is by ferry.BC Ferries,Washington State Ferries andPuget Sound Navigation Company (Black Ball Transport) operate the seven vehicle-ferry routes to the island.

In the 1860s a plan was started to link Vancouver Island to the mainland atBute Inlet, by a bridge, usingRipple Rock as a mid-support for the bridge. This plan continued through the years, and caused political opposition to destroying Ripple Rock until it was decided to destroy the rock to improve safety for mariners.[60]

BC Ferries

[edit]
BC FerriesMVSpirit of Vancouver Island, en route from Swartz Bay to Tsawwassen
Crossing time: 1 hour 35 minutes; 8 sailings per day year-round with added sailings depending on day and season)
  • Tsawwassen –Duke Point (13 km (8.1 mi) south of Nanaimo)
Crossing time: 2 hours; 8 round trips daily – varies in winter.
Crossing time: 1 hour 35 minutes; Sailings every 2 hours with extra sailings during the summer and holidays.
Crossing time: 35 minutes- 3 hours depending on island of departure; 4 or more trips daily.
Crossing time: 1 hour 20 minutes; 4 round trips daily.
Service daily or on alternate days; changes seasonally.

Washington State Ferries

[edit]
Crossing time: 2 hours (not counting stops in theSan Juan Islands)
Note that this ferry service is inactive.
According to the Washington State Department of Transport: International service to and from Sidney, B.C. remains suspended until further notice due to continued significant crewing and vessel availability challenges. There will be no service to and from Sidney through at least Spring of 2030.[61]

Black Ball Transport

[edit]
Crossing time: 1 hour 30 minutes; 1 to 4 round trips daily; changes seasonally.

Passenger-only service

[edit]
Crossing time: 1 hour 15 minutes; 3 to 6 round trips daily
Crossing time: 2 hour 45 minutes; 1 to 3 round trips daily

Rail

[edit]

Island Corridor Foundation (ICF) was established in 2006 for the purpose of owning and managing the former Esquimalt and Nanaimo (E&N) Rail Corridor on Vancouver Island now known as theIsland Rail Corridor. The ICF established a contract withSouthern Railway of British Columbia (SRY) to move all rail freight on the Island to and from the Lower Mainland. SRY assumed operational control fromRailAmerica in July 2006 and currently only offers local freight service on the Nanaimo segment of the Victoria–Courtenay mainline (called the Victoria Subdivision by the railroad). The Port Alberni branch line (called the Port Alberni Subdivision by the railroad) has been out of service since 2002. Passenger service, which had been operated byVIA Rail under contract, was halted in 2011 after it was identified that a portion of the line failed to meet operating requirements for passenger service. Since then, there have been ongoing efforts to secure funding from various levels of government to complete the necessary repairs, but the issue remains fluid.

Western Forest Products operated theEnglewood Railway which was Canada's lastlogging railway, running fromWoss toBeaver Cove on the northern end of the island. The formerCanadian National Railway line running from Victoria to the Cowichan Valley was abandoned in the late 1980s/early 1990s, and the former grade between Victoria and Sooke is now the multi-useGalloping Goose Regional Trail. TheBC Forest Discovery Centre has anarrow-gauge railway winding around the park, and theAlberni Pacific Railway operates a tour train during the summer from the restored E&N Railway station in Port Alberni to the McLean's Mill on former E&N Railway trackage that is now owned by the ICF.

Road

[edit]

There is one major north–south highway system on the island, which runs along the eastern side. It begins in Victoria asHighway 1 which is part of theTrans-Canada Highway system as far as Nanaimo. There,Highway 19 takes over and continues to Port Hardy. The route is a patchwork of two-, four-, and six-lane roadways between Victoria and Port Hardy. The engineering characteristics and traffic control systems of the roadway vary widely from one city or district to the next and include the following variations:

Trans-Canada Highway:

  1. Congested, heavily signalized four-lane urban core streets with heavypedestrian activity in Victoria and Duncan.
  2. Short four- to six-lanefreeways withinterchanges just west of Victoria and just south of Nanaimo.
  3. A mix of two-lane to four-lane winding mountainarterial highway over theMalahat pass.
  4. A moderate to heavily signalized four-lane divided arterial highway from Mill Bay to Nanaimo (interrupted by the Duncan urban core).

Highway 19:

  1. A moderately signalized expressway called the Nanaimo Parkway bypassing Nanaimo.
  2. A lightly signalized four-lane divided arterial highway from Nanaimo to Parksville.
  3. A stretch of four-lane high-speed freeway/expressway from Parksville to Campbell River.
  4. A moderate-speed two-lane arterial highway north from Campbell River to Port Hardy.[62]

Proposals have been made for amainland-to-island fixed link for over a century. Because of the extreme depth and soft seabed of the Georgia Strait, and the potential for seismic activity, a bridge or tunnel would face monumental engineering, safety, and environmental challenges at a prohibitive cost.[63]

Another north–south route isHighway 17 a four-lane divided highway that has a mix of interchanges and traffic lights. It connects Victoria with theSaanich Peninsula, terminating the Vancouver Island portion of its route at theSwartz Bay ferry terminal.

The main east–west routes are mostly two-lane but are generally free of the congestion seen on some of the four-lane highways. They comprise the following:

Vancouver Island is also well served by secondary routes, a growing number of which have efficientroundabouts in place of thetraffic lights that can back up traffic on the main highway routes. Numerous active and decommissionedlogging andforest service roads provide access to the backcountry.

Many communities are served by public and private transit. Greater Victoria is one of the few places in North America wheredouble-decker buses are used in the regular public transit system. Tofino Bus All Island Express serves all major cities on Vancouver Island.[64]

Air

[edit]

There are 52certified airports, registered aerodromes and heliports on Vancouver Island. This number includes sevenaerodromes and airports in Greater Victoria.[65]

Victoria International Airport, (IATA:YYJ,ICAO:CYYJ), is the major airport on Vancouver Island. In 2018, it was the11th busiest airport in Canada in terms of passenger movements (1,924,385).[66] As of 2020, carriers includeAir Canada Express,Air Canada Rouge,Air North,Alaska Airlines,Pacific Coastal Airlines,WestJet andWestJet Encore. They offer a variety of direct flights of short and medium distances including to and fromSeattle,Calgary,Edmonton, Vancouver,Whitehorse andToronto. Air Canada Rouge, Pacific Coastal Airlines,Sunwing Airlines,Swoop and WestJet offer seasonal services to several destinations including Mexico.

Other land-based airports with scheduled services areCampbell River,CFB Comox, (Comox Valley Airport),Nanaimo,Port Hardy,Qualicum Beach andTofino/Long Beach. In addition, there are seven water airports with scheduled services,Campbell River,Comox,Nanaimo Harbour,Port Alberni,Tofino Harbour,Victoria andVictoria Inner Harbour.

Much of thefloatplane traffic is downtown-to-downtown service between Victoria Inner Harbour, Nanaimo Harbour andVancouver Harbour, the primary carriers beingHarbour Air Seaplanes,Seair Seaplanes andCorilair. Harbour Air also flies to other areas around Vancouver, service toKenmore Air Harbor Seaplane Base on Seattle'sLake Union is provided byKenmore Air. Smaller airlines includeTofino Air, Pacific Seaplanes and Sunshine Coast Air. These carriers make several daily scheduled flights, weather permitting. Helicopter service is provided byHelijet in Victoria and various private operators elsewhere.

See also

[edit]

References

[edit]
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Further reading

[edit]

External links

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Vancouver Island at Wikipedia'ssister projects
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