Victoria Island
Large Arctic island straddling Nunavut and Northwest Territories.
Victoria Island, part of Canada’s Arctic Archipelago, sits across the border between Nunavut and the Northwest Territories. It ranks as the world’s eighth-largest island and, with an area of 219,191.31 square kilometres, is Canada’s second-largest. That makes it twice the size of Newfoundland, a bit bigger than Great Britain, and a bit smaller than Honshu. The western third of the island belongs to the Northwest Territories’ Inuvik Region; the rest falls within Nunavut’s Kitikmeot Region. Its 2,168 residents live in just two communities: Cambridge Bay in Nunavut, the larger one, and Ulukhaktok in the Northwest Territories. The island was named for Queen Victoria, who reigned over Britain from 1837 to 1901; features called “Prince Albert” honour her husband.
Long before Europeans arrived, the Thule culture lived here. On the Wollaston Peninsula, archaeologists have found five prehistoric qamutiik (sleds) from the Neoeskimo culture, dating between 1250 and 1573 AD. The Inuinnaqtun name for the island is Kitlineq, and the local Inuit are known as Kitlinermiut (Copper Inuit). The first European to see the southwest coast was John Richardson in 1826; he called it “Wollaston Land.” In 1839, Peter Warren Dease and Thomas Simpson followed the southeast coast and named it “Victoria Land.” A map John Barrow published in 1846 showed a blank space north of these two “lands” all the way to “Banks Land” (the north coast of Banks Island). John Rae charted the entire south coast in 1851, connecting the two named areas. Robert McClure’s men circumnavigated most of Banks Island in 1850 and 1851, separating it from the rest of Victoria Land, and also mapped the island’s northwest and west coasts. In 1905, Godfred Hansen—one of Roald Amundsen’s crew—charted the east coast as far as Cape Nansen. Later, in 1916 and 1917, Storker T. Storkerson, part of Vilhjalmur Stefansson’s Canadian Arctic Expedition, charted the northeast coast and spotted the Storkerson Peninsula. The first recorded people to walk across Victoria Island were Clark Carter and Chris Bray in 2008; they had failed an earlier attempt at the 1,000-kilometre trek in 2005, then returned to finish the remaining 660 kilometres three years later.
To the north lies Viscount Melville Sound; to the east are M’Clintock Channel and Victoria Strait. On the west are Amundsen Gulf and Banks Island, separated from Victoria by the Prince of Wales Strait. Running along the south, from west to east, are the Dolphin and Union Strait, Austin Bay, Coronation Gulf, and the Dease Strait. These southern waterways—and sometimes the Prince of Wales Strait—form part of the disputed Northwest Passage. Canada claims them as internal waters; other nations argue they are territorial or international waters.
The island is a jumble of peninsulas, with a deeply indented coastline full of inlets. In the east, the Storkerson Peninsula points north, ending at the Goldsmith Channel, which separates Victoria from Stefansson Island. Hadley Bay, a major inlet, divides the Storkerson Peninsula from the north-central area. Another broad peninsula, Prince Albert Peninsula, juts out in the north, ending at the Prince of Wales Strait. In the south, the Wollaston Peninsula points west, separated from the island’s centre by Prince Albert Sound. The highest point, 655 metres above sea level, is in the Shaler Mountains in the north-central region. Southeast of there, just north of Cambridge Bay, lies Tahiryuaq (formerly Ferguson Lake), the island’s largest lake at 562 square kilometres. Andrew Hund, in his book *Antarctica and the Arctic Circle*, noted that the island’s shape resembles a stylized maple leaf, Canada’s national symbol. Victoria Island also contains the world’s largest island within an island within an island.
The climate is polar (Köppen classification ET): no month averages 10°C or higher. Summers are cool and rainy, with pleasant days and chilly nights. Winters are long, dark, and cold; October sees the most snow. Snowfall and frost can occur any time of year. Rain falls mainly in summer, when temperatures briefly rise above freezing for a few months before dropping back into a nine-month winter. Springs are sunny but still very cold. Autumns are short and crisp, with cloud cover increasing in August and September being almost constantly overcast. In Cambridge Bay, the sun stays below the horizon (polar night) from about November 30 to January 11, and above it (midnight sun) from May 19 to July 22.
The Dolphin-Union caribou herd—locally called Island Caribou—is a migratory population of barren-ground caribou (*Rangifer tarandus groenlandicus*) that lives on Victoria Island and the nearby mainland. These animals are endemic to Canada. Each year they cross the Dolphin and Union Strait on sea ice, moving from summer grazing on Victoria Island to winter grazing on the Nunavut–Northwest Territories mainland. This seasonal sea-ice crossing is unusual for North American caribou; the only other caribou that do it are the smaller Peary caribou, which also live on Victoria Island. Besides caribou, the island supports a rich lichen flora that forms the base of tundra food webs. A 2018–2019 survey around Cambridge Bay and the nearby area documented this lichen diversity.
- area
- 219,191.31 km²
- rank
- Eighth-largest island in the world; second-largest in Canada
- population
- 2,168 (2021 census)
- highest_point
- 655 m in the Shaler Mountains
- largest_lake
- Tahiryuaq (formerly Ferguson Lake), 562 km²
- climate
- Polar climate (ET on Köppen classification)
- notable_feature
- Contains the world's largest island within an island within an island.
Lore & Background
Victoria Island was inhabited by the Thule culture, with five prehistoric qamutiik (sleds) belonging to the Neoeskimo culture being found on the Wollaston Peninsula, dating to 1250–1573 AD. The Inuinnaqtun name for the island is Kitlineq, with the local Inuit called Kitlinermiut (Copper Inuit). European exploration began in 1826 when John Richardson saw the southwest coast and called it 'Wollaston Land'. In 1839, Peter Warren Dease and Thomas Simpson followed its southeast coast and called it 'Victoria Land'. A map published by John Barrow in 1846 shows a complete blank from these two lands north to 'Banks Land'. In 1851 John Rae charted its entire south coast and connected the two 'lands'. In 1850 and 1851 Robert McClure circumnavigated most of Banks Island, thereby separating it from the rest of Victoria Land, and his men charted the northwest and west coasts of Victoria Island. Godfred Hansen charted its east coast as far as Cape Nansen in 1905, and in 1916 and 1917 Storker T. Storkerson charted its northeast coast, sighting the Storkerson Peninsula. In 2008 Clark Carter and Chris Bray became the first recorded people to walk across Victoria Island, completing the remaining 660 km after a failed 1,000 km attempt in 2005.
Reader's Guide
Victoria Island is a large, sparsely populated Arctic landmass that straddles two Canadian territories and contains key historical and geographical features. Its coastline is heavily indented with peninsulas and inlets, including the Storkerson Peninsula, Prince Albert Peninsula, and Wollaston Peninsula. The island's southern waterways, including the Dolphin and Union Strait and Prince of Wales Strait, form part of the disputed Northwest Passage, which the Government of Canada claims are Canadian Internal Waters, while other nations state they are either territorial waters or international waters. The island supports the Dolphin-Union caribou herd, a migratory population of barren-ground caribou that seasonally crosses sea ice, a rare behavior among North American caribou. A 2018–2019 survey around Cambridge Bay and the nearby Wellington Inlier documented 237 lichen species (186 collected during the survey and 51 from earlier records), including 35 not previously reported from the Canadian Arctic Archipelago. The island's population of 2,168 is divided between Cambridge Bay (Nunavut) and Ulukhaktok (Northwest Territories). Its polar climate features no month having an average temperature of 10 °C or higher, with polar night from approximately November 30 to January 11 and midnight sun from May 19 to July 22 at Cambridge Bay.
Did You Know?
- Victoria Island is just double the size of Newfoundland and slightly larger than the island of Great Britain.
- The Inuinnaqtun name for the island is Kitlineq, and the local Inuit are called Kitlinermiut (Copper Inuit).
- Five prehistoric qamutiik (sleds) from the Neoeskimo culture, dating to 1250–1573 AD, were found on the Wollaston Peninsula.
- The Dolphin-Union caribou herd is one of only two North American caribou populations that seasonally cross sea ice.
- A 2018–2019 survey documented 237 lichen species on the island, including 35 not previously reported from the Canadian Arctic Archipelago.
Scale, Shape, and Geographic Identity
Victoria Island ranks as the eighth-largest island on Earth and holds the distinction of being Canada's second-largest, spanning 219,191.31 km². To put that in perspective, it is just double the size of Newfoundland (108,878.06 km²), slightly larger than the island of Great Britain (218,634.50 km²), but smaller than Honshu (228,296.26 km²). The landmass straddles a political boundary: its western third lies in the Inuvik Region of the Northwest Territories, while the remainder is part of Nunavut's Kitikmeot Region. Only 2,168 people call it home, split between Cambridge Bay and Ulukhaktok. Geographically, the island is defined by its heavily indented coastline with many inlets and a constellation of peninsulas. The Storkerson Peninsula points northwards in the east, the broad Prince Albert Peninsula ends at the Prince of Wales Strait in the north, and the Wollaston Peninsula points westwards in the south. The Shaler Mountains in the north-central region crown the island at 655 m, while Tahiryuaq (formerly Ferguson Lake), with an area of 562 km², is the largest lake on the island. Andrew Hund noted the island resembles a stylized maple leaf, and it contains the world's largest island within an island within an island.
A Century of Charting an Elusive Coastline
For much of the nineteenth century, European maps showed Victoria Island as a gap of uncertainty. In 1826, John Richardson glimpsed the southwest shore and dubbed the territory 'Wollaston Land'. In 1839, Peter Warren Dease and Thomas Simpson traced the southeast coast and called it 'Victoria Land', yet a map published by John Barrow in 1846 still depicted a complete blank from these two lands north to 'Banks Land'. It was not until 1851 that John Rae charted the entire south coast and connected the two 'lands' into a single landmass. Around the same time, in 1850 and 1851, Robert McClure's expedition circumnavigated most of Banks Island, thereby separating it from the rest of Victoria Land, and his men charted the northwest and west coasts of Victoria Island. The eastern and northeastern coasts resisted mapping for another half-century. In 1905, Godfred Hansen, a member of Roald Amundsen's party, charted the east coast as far as Cape Nansen. Then in 1916 and 1917, Storker T. Storkerson, working under Vilhjalmur Stefansson's Canadian Arctic Expedition, finally charted the northeast coast and sighted the Storkerson Peninsula. The island's full traversal remained beyond reach until 2008, when Clark Carter and Chris Bray became the first recorded people to walk across Victoria Island, completing the remaining 660 km after their 1,000 km attempt in 2005 failed.
Indigenous Roots and Imperial Naming
Long before any European vessel rounded its shores, the Thule culture left its mark on Victoria Island. Five prehistoric qamutiik—traditional sleds belonging to the Neoeskimo culture—were recovered from the Wollaston Peninsula, dating them to the period between 1250 and 1573 AD. The island's Inuinnaqtun name is Kitlineq, reflecting the deep linguistic roots of the people who call themselves the Kitlinermiut, or Copper Inuit. The English name, however, carries a very different provenance. The island is named after Queen Victoria, the British sovereign from 1837 to 1901, while various geographic features bearing the name 'Prince Albert' are named after her consort, Albert. Today the island's human presence is concentrated in just two communities: Cambridge Bay in Nunavut, the larger of the two, and Ulukhaktok in the Northwest Territories. Together they house a population of 2,168, a small but enduring human footprint on a landmass that has witnessed millennia of Inuit habitation and centuries of imperial cartography.
Polar Seasons and a Fragile Tundra Web
Victoria Island sits firmly in the polar regime, classified as ET on the Köppen climate classification, meaning no single month ever averages 10 °C or above. At Cambridge Bay the sun vanishes entirely from approximately November 30 to January 11, plunging the community into polar night, then returns for an unbroken stretch of midnight sun from May 19 to July 22. Summers are typically cool and rainy, with pleasant days and chilly nights. Winters are cold, dark, and long, with October being the snowiest month. Snowfall and frosts are possible all year round. Rain is usually limited to the summer months, when the temperature shortly rises above freezing for a few months before dipping back down for another 9 months of winter. Springs are typically sunny but still very chilly. Autumns are short and crisp, with more frequent cloud cover starting to appear during August and with September being almost constantly cloudy. Ecologically, the island is anchored by the Dolphin-Union caribou herd, a migratory population of barren-ground caribou endemic to Canada. Each year these animals migrate across the Dolphin and Union Strait from their summer grazing on Victoria Island to their winter grazing area on the Nunavut-NWT mainland—a seasonal sea-ice crossing that is unusual for North American caribou. Beneath them, a rich lichen flora underpins tundra food webs. A 2018–2019 survey around Cambridge Bay and the nearby Wellington Inlier documented 237 lichen species (186 collected during the survey and 51 from earlier records), including 35 not previously reported from the Canadian Arctic Archipelago.
Frequently Asked Questions
What is Victoria Island?
Victoria Island is a massive landmass in the Canadian Arctic Archipelago that sits along the border between Nunavut and the Northwest Territories.
How big is Victoria Island and where does it rank?
Spanning approximately 219,191 square kilometers, it is the ninth-largest island globally and the third-largest in Canada.
Who is Victoria Island named after?
The island takes its name from Queen Victoria, the British monarch who reigned from 1837 to 1901, while several local geographic features honor her husband, Prince Albert.
What is the climate like on Victoria Island?
It falls under a polar climate classification (Köppen ET), meaning the island endures frigid temperatures and very limited precipitation throughout the year.
What are the notable geographic features of Victoria Island?
The Shaler Mountains contain the island's highest point at 655 meters above sea level, and Lake Taseko is its largest body of fresh water.
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