Pitt Island (Canada)

For other places with the same name, see Pitt Island (disambiguation).

Pitt Island

Northern End of Pitt Island as seen from Grenville Channel
Pitt Island is located between Banks Island and the mainland.
Geography
Coordinates	53°30′00″N129°47′00″W / 53.50000°N 129.78333°W / 53.50000; -129.78333
Area	1,368 km2 (528 sq mi)
Length	90 km (56 mi)
Width	8 km (5 mi)
Highest elevation	962 m (3156 ft)
Administration
Canada
Province	British Columbia

Pitt Island is an island located on the north coast of British Columbia, Canada. ^[1] The island is of cultural and ecological importance. ^[2]

Pitt island is located between Banks Island, across Grenville Channel (part of the Inside Passage) from the mainland, and is separated from Banks Island by Principe Channel. ^[3] The island is mountainous and heavily dissected by valleys, fjords, and inlets and has an area of 1,368 square kilometres (528 sq mi), is 90 kilometres (56 mi) long, and ranges from 8 to 23 kilometres (5.0 to 14.3 mi) wide. Its highest point is at 962 metres (3,156 ft).

Pitt Island is the only island in British Columbia known to host a resident population of moose. ^[4]

History

The Gitxaala occupied the island in the past, with a fishing and hunting village for each family group, ^[5] and have identified this island as part the laxyuup(traditional territories and waters) ^[6] of the Gitxaala. ^[7]

Geology

Pitt Island lies within the Coast Range Arc, part of the broader Coast Mountains geological province formed by subduction and terrane accretion along the edge of North American Plate. The island is part of an ancient collage that makes up the British Columbia Coast, where multiple island arcs and seafloor were accreted onto the Continental margin over hundreds of millions of years. The Coast Range Intrusive Complex, which includes Pitt Island, formed primarily in the mid to late Mesozoic as subduction processes drove extensive magmatism and crustal growth ^[8] .

The dominant bedrock consists of intrusive rocks, mainly diorites and quartz diorites of acidic composition, that make up much of the island’s interior. These rocks represent magma that crystallized deep underground during the Cretaceous and were later exposed at the surface by tectonic uplift and erosion ^[8] . Like much of the coast, the island's superficial deposits, soils, colluvium, and glacial drift, were influenced by Pleistocene glaciation, which carved steep relief across the landscape ^[9] .

Features

• Anchor Mountain ^[10]
• Captain Cove ^[11]
• Holmes Lake ^[12]
• Hevenor Inlet ^[13]
• Newcombe Harbour ^[14]
• Pa-aat River ^[15]
• Port Stevens ^[16]
• Monckton Inlet ^[17]
• Mount Hulke ^[18]
• Mount Patterson ^[19]
• Mount Frank ^[20]
• Mount Saunders ^[21]
• Mount Shields ^[22]
• Wyndham Lake ^[23]
• Red Bluff Lake ^[24]

Protected Areas

• Union Passage Marine Provincial Park ^[25]
• Maxtaktsm'Aa/Union Passage Conservancy ^[26]
• Monckton Nii Luutiksm Conservancy ^[27]
• Pa-aat Conservancy ^[28]

References

1. "Pitt Island". Natural Resources Canada. February 16, 2021.
2. "Gitxaała Community‑led Planning and Management of the Pitt Island Mink Trap Watersheds". Watershed Security Fund. Watershed Security Fund. Retrieved 1 January 2026.
3. "Pitt Island". BC Geographical Names .
4. Price Michael H, Darimont Chris T, Winchester Neville N, Paquet Paul C (2005). "Facts from faeces: prey remains in Wolf, Canis lupus, faeces revise occurrence records for mammals of British Columbia's coastal archipelago". Canadian Field-Naturalist. 119 (2): 192–196. doi: 10.22621/cfn.v119i2.105 . Retrieved 2020-06-22.
5. Marsden, Susan (December 2011). The Gitkxaala, Their History, and Their Territories (Porcher Island, Banks Island, Pitt Island and Adjacent Islands) (PDF) (Report). Canadian Environmental Assessment Agency. Retrieved 2 January 2026.
6. Menzies, Charles R. (2016). ""Laxyuup: The Land and Ocean Territories of Gitxaała"". People of the Saltwater: An Ethnography of Git Lax M’oon. University of Nebraska Press. ISBN   9780803291706 . Retrieved 2026-01-02.
7. "Our Story". Gitxaała Enterprises Corporation. Gitxaała Nation. Retrieved 1 January 2026.
8. Warne, Jeff; Lloyd, John (May 1983). A Geophysical Report on a VLF-EM Survey on the Pit Claim for Ryan Exploration Ltd (Report). Vancouver, British Columbia: BC Ministry of Energy, Mines and Low Carbon Innovation, Assessment Report Indexing System (ARIS). Retrieved 27 December 2025.
9. Clague, John J.; Ward, Bob (2011). "Pleistocene Glaciation of British Columbia" (PDF). Quaternary Science Reviews. 15: 563–577. doi:10.1016/B978-0-444-53447-7.00044-1. In western British Columbia, ice streamed down fjords and valleys in the coastal mountains, producing erosional and depositional features characteristic of alpine and ice-sheet glaciation
10. "Anchor Mountain". BC Geographical Names .
11. "Captain Cove". BC Geographical Names .
12. "Holmes Lake". BC Geographical Names .
13. "Hevenor Inlet". BC Geographical Names .
14. "Newcombe Harbour". BC Geographical Names .
15. "Pa-aat River". BC Geographical Names .
16. "Port Stevens". BC Geographical Names .
17. "Monckton Inlet". BC Geographical Names .
18. "Mount Hulke". BC Geographical Names .
19. "Mount Patterson". BC Geographical Names .
20. "Mount Frank". BC Geographical Names .
21. "Mount Saunders". BC Geographical Names .
22. "Mount Shields". BC Geographical Names .
23. "Wyndham Lake". BC Geographical Names .
24. "Red Bluff Lake". BC Geographical Names .
25. "Union Passage Marine Park". BC Geographical Names .
26. "Maxtaktsm'Aa/Union Passage Conservancy". BC Geographical Names .
27. "Monckton Nii Luutiksm Conservancy". BC Geographical Names .
28. "Pa-aat Conservancy". BC Geographical Names .