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The Chilliwack Batholith is a large batholith that forms much of the North Cascades in southwestern British Columbia, Canada and the U.S. state of Washington. The geological structure is named after the Chilliwack River Valley, where it outcrops in many places.
The Chilliwack Batholith forms much of the North Cascades in southwestern British Columbia, Canada and the U.S. state of Washington. The geological structure is primarily named after the City of Chilliwack, where it is the most notable geological feature.
Mount McGuire is a 2,008-metre (6,588-foot) mountain summit located in the Cascade Mountains of southwestern British Columbia, Canada.It is situated 4 km (2 mi) north of the Canada–United States border, 19 km (12 mi) southeast of Chilliwack, and 7.4 km (5 mi) northwest of Canadian Border Peak, which is its nearest higher peak. [4]
The Canadian Cascade Arc, also called the Canadian Cascades, is the Canadian segment of the North American Cascade Volcanic Arc.Located entirely within the Canadian province of British Columbia, it extends from the Cascade Mountains in the south to the Coast Mountains in the north.
The geology of British Columbia is a function of its location on the leading edge of the North American continent. The mountainous physiography and the diversity of the different types and ages of rock hint at the complex geology , which is still undergoing revision despite a century of exploration and mapping.
Mount Grant 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 the subduction of the Farallon Plate starting 29 million years ago.
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.
Mount Barr is a mountain in the Skagit Range of the Cascade Mountains of southern British Columbia, Canada, located on the northeast side of Wahleach Lake and just southwest of Hope. It is a ridge highpoint with an elevation of 1,907 m (6,257 ft). Mount Barr is one of several magmatic features just north of the Chilliwack batholith.