Victoria Island

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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.