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  2. Chilliwack batholith - Wikipedia

    en.wikipedia.org/wiki/Chilliwack_batholith

    The geological structure is named after the Chilliwack River Valley, where it outcrops in many places. It does not outcrop anywhere near the City of Chilliwack. The Chilliwack Batholith is part of the Pemberton Volcanic Belt and is the largest mass of exposed intrusive rock in the Cascade Volcanic Arc. The age of the Chilliwack batholith ranges ...

  3. Canadian Cascade Arc - Wikipedia

    en.wikipedia.org/wiki/Canadian_Cascade_Arc

    The first volcanic event 29 million years ago formed intrusive rocks of the large Chilliwack batholith, which extends south into the U.S. state of Washington. [1] [9] In Canada, the batholith consists of rocks ranging from hypersthene quartz gabbro to albite granite. Three main plutons are present.

  4. Chilliwack - Wikipedia

    en.wikipedia.org/wiki/Chilliwack

    Chilliwack (/ ˈ tʃ ɪ l ə w æ k / CHIL-ə-wak) is a city of about 100,000 people and 261 km 2 (100 sq mi) in the Canadian province of British Columbia.It is located about 100 km (62 mi) east of the City of Vancouver in the Fraser Valley.

  5. Cascade Volcanoes - Wikipedia

    en.wikipedia.org/wiki/Cascade_Volcanoes

    The greatest mass of exposed Cascade Arc plumbing is the Chilliwack batholith, which makes up much of the northern part of North Cascades National Park and adjacent parts of British Columbia beyond. Individual plutons range in age from about 35 million years old to 2.5 million years old.

  6. Slesse Mountain - Wikipedia

    en.wikipedia.org/wiki/Slesse_Mountain

    Most of Mount Slesse is made up of granitic rocks related to the Chilliwack batholith, which intruded the region 26 to 29 million years ago after the major orogenic episodes in the region. This is part of the Pemberton Volcanic Belt , an eroded volcanic belt that formed as a result of the subduction of the Farallon Plate starting 29 million ...

  7. Mount Hatfield - Wikipedia

    en.wikipedia.org/wiki/Mount_Hatfield

    Mount Hatfield is related to the Chilliwack batholith, which intruded the region 26 to 29 million years ago after the major orogenic episodes in the region. This is part of the Pemberton Volcanic Belt, an eroded volcanic belt that formed as a result of subduction of the Farallon Plate starting 29 million years ago.

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