Diadem Peak
Diadem Peak from Icefields Parkway
Highest point
Elevation3,371 m (11,060 ft)[1][2][3]
Prominence211 m (692 ft)[2]
Parent peakMount Woolley (3405 m)[2]
ListingMountains of Alberta
Coordinates52°18′38″N 117°25′15″W / 52.31056°N 117.42083°W / 52.31056; -117.42083[4]
Geography
Diadem Peak is located in Alberta
Diadem Peak
Diadem Peak
CountryCanada
ProvinceAlberta
Protected areaJasper National Park
Parent rangeWinston Churchill Range
Topo mapNTS 83C6 Sunwapta Peak[4]
Climbing
First ascent1898 by Collie, Stutfield and Woolley
Easiest routerock/snow/glacier climb (South Ridge)

Diadem Peak is a peak located in the Sunwapta River Valley of Jasper National Park, Canada. Diadem Peak is essentially the high point of a ridge leading down from the slightly higher Mount Woolley (3,405 m (11,171 ft)). This peak was the first 11,000er north of the Columbia Icefield to be climbed and one of the few peaks in the Canadian Rockies to be climbed before 1900.

The mountain was named in 1898 by the first ascent team of J. Norman Collie, Hugh Stutfield and Hermann Woolley. Upon reaching the summit, they discovered a crown (diadem) of snow about 30 m (98 ft) high covering the almost flat layer of rocks on top.[1]

Climbing history

Diadem Peak (right) and Mount Woolley (left), from Parker Ridge

In the summer of 1898, J. Norman Collie, Hugh Stutfield and Herman Woolley, had made their way up Woolley Creek and initially had their sights on reaching the top of Mount Woolley by climbing the icefield that separates Mt. Woolley from Diadem Peak. However, after a brief downpour which forced them to seek shelter among some rocks, they had just begun preparing the rope for ascending the icefield when a large collapse of ice from the summit made them switch their objective to Diadem Peak. The party ascended the southeast ridge along loose shale and ice, eventually finding a small rock rib that took them to the summit on August 25. Collie recorded an initial elevation of 11,500 feet (3,505 m) using a mercurial barometer. With the use of crampons, the difficulties of the southeast ridge route are reduced by following a shallow snow gully up much of the way.[5]

In 1962, William Buckingham and Bill Hooker, ascended Diadem Peak by what is now known as the South Ridge route. This route initially traverses loose rock ledges to reach a snow/ice couloir which is followed until the glacier levels off and is no longer fractured. Traversing left across rock to the glacier, the route follows the glacier up to the Woolley-Diadem col where Diadem's summit is reached after an easy ascent up the ridge.[5] Jim Elzinga and Jeff Marshall made the first ascent up a mixed route on the North face of Diadem in July 1981. This route is known as "Humble Horse" (IV, 5.7, W4).[5]

Geology

Mushroom Peak (left) and Diadem Peak (right) seen from the Icefields Parkway

Diadem Peak is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.[6] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[7]

Climate

Based on the Köppen climate classification, Diadem Peak is located in a subarctic climate with cold, snowy winters, and mild summers.[8] Temperatures can drop below -20 °C with wind chill factors below -30 °C.

See also

References

  1. 1 2 "Diadem Peak". cdnrockiesdatabases.ca. Retrieved 2004-06-05.
  2. 1 2 3 "Diadem Peak". Bivouac.com. Retrieved 2008-12-31.
  3. ↑ "Topographic map of Diadem Peak". opentopomap.org. Retrieved 2022-06-27.
  4. 1 2 "Diadem Peak". Geographical Names Data Base. Natural Resources Canada. Retrieved 2022-06-27.
  5. 1 2 3 Corbett, pp. 52-53
  6. ↑ Belyea, Helen R. (1960). The Story of the Mountains in Banff National Park (PDF). parkscanadahistory.com (Report). Ottawa: Geological Survey of Canada. Archived (PDF) from the original on 2015-10-02. Retrieved 2019-09-13.
  7. ↑ Gadd, Ben (2008), Geology of the Rocky Mountains and Columbias
  8. ↑ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN 1027-5606.
Sources
  • Corbett, Bill (2009) [First published 2004]. The 11,000ers of the Canadian Rockies. Rocky Mountain Books. ISBN 978-1-897522-40-0.
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