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      • The Fitzsimmons Range is a small mountain range on the northwestern edge of the Garibaldi Ranges in southwestern British Columbia, Canada, located between the valleys of Cheakamus Lake (SW) and Fitzsimmons Creek (NE).
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  2. The Fitzsimmons Range is a small mountain range on the northwestern edge of the Garibaldi Ranges in southwestern British Columbia, Canada, located between the valleys of Cheakamus Lake (SW) and Fitzsimmons Creek (NE). Its most famous summit is Whistler Mountain, which overlooks the resort town of Whistler and is one of the two mountains forming ...

    • Canada
    • Garibaldi Ranges
    • Geography
    • Geology
    • Ecology
    • Human History
    • Best Hikes in The Fitzsimmons Range
    • Major Cities and Towns

    The Fitzsimmons Range is a subrange of the Garibaldi Ranges of southwestern British Columbia, Canada. The most famous mountain in the Fitzsimmons Range is Mount Whistler, which is 2,181 m (7,156 ft) tall. Mount Whistler is also the most prominent peak in the range with 464 m (1,522 ft) of prominence. Aptly named, Mount Whistler overlooks the town o...

    Fitzsimmons Creek The Fitzsimmons Range contains various volcanic rocks that were deposited on the seafloor over the past 250 million years. The sediment on the sea floor was compacted by the weight of the underwater lava flows. About 170 million years ago, these sediments were compressed, folded, and buckled, to form the mountain ranges that we se...

    There are four ecological zones represented in the Fitzsimmons Range, each of which is characterized by its dominant plant species. The highest elevations of the range are part of the Alpine Tundra Zone. This zone includes communities of heather on otherwise barren peaks. The runoff from these glaciers often settles in low areas. Small communities ...

    Human habitation of the Fitzsimmons Range and surrounding area began about 10,000 years ago, shortly after the melting of the Pleistocene ice sheet. Obsidian mines that were used by Indigenous peoples for the past 10,000 years have been uncovered in Garibaldi Provincial Park. The range is the traditional territory of the Squamish, Lil’wat, and St’á...

    The Fitzsimmons Range is home to one of the world’s premiere ski destinations. It features breathtaking landscapes, forests, rivers, lakes, and glaciers. The following are several of popular hiking trails and attractions in the Fitzsimmons Range:

    Looking for a place to stay near the Fitzsimmons Range? Here are some of the best cities and towns to check out in the region:

  3. Fitzsimmons Range. Map of Fitzsimmons RangeClick on red triangle icons for links to other ranges. Other Ranges: To go to pages for other ranges either click on the map above, or on range names in the hierarchy snapshot below, which show the parent, siblings, and children of the Fitzsimmons Range.

  4. The Fitzsimmons Range is a subsection of the Garibaldi Ranges that covers the area between the valleys of Cheakamus Lake and Fitzsimmons Creek. Fitzsimmons Creek cuts between Whistler Mountain and Blackcomb Mountain and largely originates from the Fitzsimmons Glacier.

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  5. Whistler Mountain (Lillooet/Ucwalmícwts: Nsqwítsu) is a mountain in the Fitzsimmons Range of the Pacific Ranges of the Coast Mountains, located on the northwestern edge of Garibaldi Provincial Park. It is the location of the Whistler-Blackcomb ski resort and the town of Whistler, British Columbia, Canada.

  6. From Wikipedia, the free encyclopedia. The Fitzsimmons Range is a small mountain range on the northwestern edge of the Garibaldi Ranges in southwestern British Columbia, Canada, located between the valleys of Cheakamus Lake (SW) and Fitzsimmons Creek (NE). Its most famous summit is Whistler Mountain, which overlooks the resort town of Whistler ...

  7. The Fitzsimmons Range is a subsection of the Garibaldi Ranges that covers the area between the valleys of Cheakamus Lake and Fitzsimmons Creek . Fitzsimmons Creek cuts between Whistler Mountain and Blackcomb Mountain and largely originates from the Fitzsimmons Glacier.

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