Mount Outram

{{short description|Mountain in Banff NP, Alberta, Canada}}

{{Use mdy dates|date=November 2019}}

{{Infobox mountain

| name = Mount Outram

| photo = Mountains in Banff.jpg

| photo_caption = Mount Outram seen from the Icefields Parkway

| elevation_m = 3245

| elevation_ref = {{cite bivouac|id=321|name=Mount Outram|accessdate=2019-02-23}}

| prominence_m = 735

| prominence_ref =

| range = Forbes Group, Central Icefields
Canadian Rockies

| location = Alberta, Canada

| parent_peak = Mount Forbes (3,617 m)

| listing = Mountains of Alberta

| map = Alberta#Canada

| map_caption = Location in Alberta##Location in Canada

| mapframe = yes

| mapframe-zoom = 8

| mapframe-caption = Interactive map of Mount Outram

| coordinates = {{coord|51|52|54|N|116|52|31|W|type:mountain_region:CA-AB_scale:100000|format=dms|display=inline,title}}

| coordinates_ref = {{cite cgndb|id=IANXM|name=Mount Outram|accessdate=2019-02-23}}

| topo = NTS {{Canada NTS Map Sheet|82|N|15}}

| rock = Sedimentary

| first_ascent = 1924 F.V. Field, W.0. Field, L. Harris, Edward Feuz Jr, J. Biner.{{cite peakfinder|id=1022|name=Mount Outram|access-date=2019-11-10}}

| easiest_route = Mountaineering

}}

Mount Outram is a {{Convert|3245|m|ft|abbr=off|adj=on}} mountain summit located in the Howse River Valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Forbes, {{convert|4.37|km|mi|abbr=on}} to the southwest.{{cite peakbagger|4487|Mount Outram, Alberta|accessdate=2019-11-10}} Glacier Lake is situated {{convert|4.0|km|mi|abbr=on}} to the north, and the Sir James Glacier lies below the south aspect of the peak. Mount Outram can be seen from the Icefields Parkway southwest of Saskatchewan Crossing, with optimum photography conditions in morning light.

History

Mount Outram was named in 1920 for James Outram (1864-1925), a mountaineer who made numerous first ascents in the Canadian Rockies including Mount Assiniboine, Chancellor Peak, Cathedral Mountain, and Mount Wilson.

The first ascent of the mountain was made in 1924 by F.V. Field, W.O. Field, and L. Harris, with guides Edward Feuz Jr. and J. Biner.

The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada.

Geology

Like other mountains in Banff Park, Mount Outram is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.{{Belyea-Banff-NP}} Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.{{cite book|title=Geology of the Rocky Mountains and Columbias |author=Gadd, Ben |year=2008}}

Climate

Based on the Köppen climate classification, Mount Outram is located in a subarctic climate zone with cold, snowy winters, and mild summers.{{cite journal | author = Peel, M. C. |author2=Finlayson, B. L. |author3=McMahon, T. A. | year = 2007 | title = Updated world map of the Köppen−Geiger climate classification | journal = Hydrol. Earth Syst. Sci. | volume = 11 |issue=5 | pages = 1633–1644 |doi=10.5194/hess-11-1633-2007 |doi-access=free |bibcode=2007HESS...11.1633P | issn = 1027-5606| url = https://hal.archives-ouvertes.fr/hal-00298818/file/hessd-4-439-2007.pdf }} Winter temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather conditions, summer months are best for climbing. Precipitation runoff from Mount Outram drains into tributaries of the Howse River.

Gallery

Mt. Outram, Banff National Park.jpg|Mount Outram

See also

{{stack|{{Portal|Mountains}}}}

References

{{reflist}}