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Steep-sided glacial fjord adjacent to the city of Vancouver in southwestern British Columbia. Wikipedia

  • Burrard Inlet

    Relatively shallow-sided coastal fjord in southwestern British Columbia, Canada. Formed during the last Ice Age, it separates the City of Vancouver and the rest of the low-lying Burrard Peninsula (to the south) from the slopes of the North Shore Mountains, home to the communities of West Vancouver and the City and District of North Vancouver. Wikipedia

  • History of Vancouver

    One that extends back thousands of years, with its first inhabitants arriving in the area following the Last Glacial Period. Situated in British Columbia, Canada; with its location near the mouth of the Fraser River and on the waterways of the Strait of Georgia, Howe Sound, Burrard Inlet, and their tributaries. Wikipedia

  • Howe Sound

    Roughly triangular sound, that joins a network of fjords situated immediately northwest of Vancouver, British Columbia. Situated between West Vancouver and the Sunshine Coast. Wikipedia

  • Toba Inlet

    One of the lesser, but still principal, inlets of the British Columbia Coast. Fourth in the series north from the 49th parallel which begins with Burrard Inlet, which is the harbour for the city of Vancouver. Wikipedia

  • List of fjords in Canada

    Fjords in Canada are long, narrow inlets characterized by steep sides, created in a valley carved by glacial activity. A fjord can have two or more basins separated by sills. Wikipedia

  • Courtenay, British Columbia

    City on the east coast of Vancouver Island, in the Canadian province of British Columbia. Largest community and only city in the area commonly known as the Comox Valley, and the seat of the Comox Valley Regional District, which replaced the Comox-Strathcona Regional District. Wikipedia


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