Jump to content

Mount Lowell

Coordinates: 52°30′15″N 117°49′56″W / 52.50417°N 117.83222°W / 52.50417; -117.83222
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Denelson83 (talk | contribs) at 01:27, 17 August 2021 (Link NTS map sheet ID). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Mount Lowell
Mount Lowell seen from Fryatt Valley area
Highest point
Elevation3,150 m (10,330 ft)[1]
Prominence370 m (1,210 ft)[1]
Parent peakBrussels Peak (3161 m)[1]
ListingMountains of Alberta
Coordinates52°30′15″N 117°49′56″W / 52.50417°N 117.83222°W / 52.50417; -117.83222[1]
Geography
Mount Lowell is located in Alberta
Mount Lowell
Mount Lowell
Location of Mount Lowell in Alberta
Mount Lowell is located in Canada
Mount Lowell
Mount Lowell
Mount Lowell (Canada)
LocationAlberta, Canada
Parent rangeCanadian Rockies
Topo mapNTS 83C12 Athabasca Falls
Geology
Type of rockSedimentary
Climbing
First ascent1927 Alfred Ostheimer[2]
Easiest routeMountaineering via South Ridge[1]
Mt. Christie (left), Brussels Peak (center), Mt. Lowell (right)

Mount Lowell is a 3,150-metre (10,330 ft) mountain summit located in the Athabasca River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. The name has not been officially adopted yet for this peak. It is situated at the head of Fryatt Creek Valley on the same high ridge as Mount Christie, Xerxes Peak, and Brussels Peak which is the nearest higher peak, 2.0 km (1.2 mi) to the north.[1] Mount Lowell can be seen from the Icefields Parkway.

History

The first ascent of the mountain was made in 1927 by Alfred Ostheimer with guides Hans Fuhrer and J. Weber.[2] Alfred Ostheimer named the peak after A. Lawrence Lowell who was a mountaineer and the president of Harvard University when Ostheimer climbed it.[2]

Geology

Mount Lowell is composed of sedimentary rock laid down from the Precambrian to Jurassic periods, then pushed east and over the top of younger rock during the Laramide orogeny.[3]

Climate

Based on the Köppen climate classification, Mount Lowell is located in a subarctic climate with long, cold, snowy winters, and short mild summers.[4] Temperatures can drop below -20°C with wind chill factors below -30°C. Precipitation runoff from Mount Lowell drains into Fryatt Creek and Lick Creek, both tributaries of the Athabasca River.

See also

References

  1. ^ a b c d e f "Mount Lowell". Bivouac.com. Retrieved 2019-02-07.
  2. ^ a b c "Mount Lowell". cdnrockiesdatabases.ca. Retrieved 2021-02-25.
  3. ^ Gadd, Ben (2008), Geology of the Rocky Mountains and Columbias
  4. ^ 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.