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Cracker Creek Cone is a small cinder cone in northwestern British Columbia.A large lava flow that partly filled Ruby Creek may have originated from this cone. The lower west side of the cone appears to be partly covered by glacial till suggesting that the cone is older than the most recent glacial advances down Ruby Creek.
This is a list of provincial parks in the Canadian province of Alberta. They are maintained by Alberta Parks . For a list of protected areas in Alberta, see the List of protected areas of Alberta .
[1] [2] It includes the Macdonald Range in British Columbia and Montana west of the Flathead River and east of the Wigwam River, the Clark Range straddling the British Columbia-Alberta-Montana borders east of the Flathead River, the Galton Range in British Columbia and Montana on the west side of the Wigwam River, and the Lewis Range in Alberta ...
Volcanic Creek Cone is a small cinder cone 20 kilometres (12 miles) northeast of Atlin in northwestern British Columbia. There are two cinder cones and a lava flow at least 3 kilometres (2 miles) long which is present below parts of the tree covered area. The subdued form of Volcanic Creek cone is visible directly below the largest snow patch.
Williams Cone is a satellite cone of Mount Edziza, located 36 km (22 mi) east of Telegraph Creek. It lies just off the northern edge of the Tencho Icefield and is one of the many postglacial cinder cones that lie on the Mount Edziza volcanic complex .
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This article related to a mountain, mountain range, or peak in British Columbia, Canada is a stub. You can help Wikipedia by expanding it.
There is no universally accepted hierarchical division of the Canadian Rockies into subranges. [1] [2] For ease of navigation only, this article follows [1] and divides the Canadian Rockies into Far Northern Rockies, Northern Continental Ranges, Central Main Ranges, Central Front Ranges and Southern Continental Ranges, each of these subdivided in distinct areas and ranges.