词条 | East End of Rundle | ||
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| name = East End of Rundle (EEOR) | photo = East End Of Rundle.jpg | photo_caption = East End of Rundle seen from westbound Highway 1 | elevation_m = 2530 | elevation_ref = | prominence = | location = Alberta, Canada | range = South Banff Ranges, Canadian Rockies | map = Alberta#Canada | map_caption = Location in Alberta | map_size = 260 | label_position = right | coordinates = {{coord|51|05|00|N|115|25|05|W|type:mountain_region:CA| | topo = NTS 82O/3 | first_ascent = | easiest_route = easy/moderate scramble }} East End of Rundle (EEOR) is a mountain located immediately west of the town of Canmore, Alberta and immediately west of the Spray Lakes road in the Canadian Rockies. Mount Rundle occupies the space between Canmore and Banff on the southwest side of the Trans-Canada Highway. There is a scrambling route up from the Spray Lakes road. GeologyThe mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.[1] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[2] ClimateBased on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers.[3] Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Rundle drains into the Bow River which is a tributary of the Saskatchewan River. References1. ^{{cite journal|last1=Belyea|first1=Helen|title=The Story of the Mountains in Banff National Park|publisher=Geological Survey of Canada|date=1960}} 2. ^{{cite journal|title=Geology of the Rocky Mountains and Columbias |author=Gadd, Ben |year=2008}} 3. ^{{cite journal | author = Peel, M. C. |author2=Finlayson, B. L. |author3=McMahon, T. A. |last-author-amp=yes | year = 2007 | title = Updated world map of the Köppen−Geiger climate classification | journal = Hydrol. Earth Syst. Sci. | volume = 11 | pages = 1633–1644 | issn = 1027-5606}} See also
GalleryExternal links
1 : Mountains of Alberta |
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