| Caption: Hoodoos. Photographed on the banks of the Chilcotin River, in Farwell
Canyon, British Columbia, Canada. |
|
 |
| Facts: Hoodoos are an example of differential erosion typically by frost, wind or rain. They are composed of both hard and soft rock layers with the harder layers forming a sort of protection for the softer areas. Hoodoos, unlike "spires" rise in an uneven pattern and are often described as looking totem-pole like. They range in size from about 5 feet up to 150 feet. |
|
|
| Photographer: David Nunuk |
|
|
| File Info: |
| MEDIUM RES: JPEG, 7332x2385, 8.22MB, ARGB |
|
|
|
|
| Keywords:
hoodoos, erosion, BC, British Columbia, Canada, rock, rock formation, landscape, panoramic |
|
|
|
|
|
|
|
|
|
