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Ibex Peak, is a 2,039-metre (6,690-foot) granitic horn located in the North Cascades of southwestern British Columbia, Canada. It is situated 13 km (8 mi) west-northwest of Coquihalla Summit, and 1 km (1 mi) northwest of Steinbok Peak. Its nearest higher peak is Alpaca Peak, 6.2 km (4 mi) to the east.[3] Precipitation runoff from the peak drains into tributaries of the Anderson River. The mountain was named for the ibex, as part of the ungulate theme for several other nearby peaks that were submitted by Philip Kubik of Vancouver.[4] The mountain's name was officially adopted on February 5, 1976, by the Geographical Names Board of Canada.[2]

Ibex Peak
Steinbok Peak (left) and Ibex Peak (right)
Highest point
Elevation	2,039 m (6,690 ft)[1]
Prominence	474 m (1,555 ft)[1]
Parent peak	Guanaco Peak (2127 m)[1]
Listing	Mountains of British Columbia
Coordinates	49°38′52″N 121°15′38″W[2]
Geography
Ibex Peak Location in British Columbia Show map of British Columbia Ibex Peak Ibex Peak (Canada) Show map of Canada
Location	British Columbia, Canada
District	Yale Division Yale Land District
Parent range	North Cascades
Topo map	NTS 92H11 Spuzzum[2]
Climbing
First ascent	1962 by Asger Bentzen, Hamish Mutch, Glenn Woodsworth, Bob Woodsworth[1]
Easiest route	Scramble via northwest slope[1]

Geology

The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch.[5] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted.[5] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.[5]

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape.[5] The "U"-shaped cross section of the river valleys are a result of recent glaciation. Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area.

The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks and ridges, deep glacial valleys, and granite spires. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to various climate differences which lead to vegetation variety defining the ecoregions in this area.

Climate

Based on the Köppen climate classification, Ibex Peak is located in the marine west coast climate zone of western North America.[6] Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Range where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the Cascade Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for climbing Ibex Peak.

Climbing Routes

Established climbing routes on Ibex Peak:[1]

• Northwest Slope - class 3 First ascent 1962
• Southwest Ridge - class 5.9 FA 1981
• East Ridge/Face - class 5.10 FA 1982
• Trivial Pursuits - class 5.10+ FA 1995
• South Face (Proof Is In The Pudding)- class 5.10c FA 2003

See also

• Geography of the North Cascades
• Geology of British Columbia

References

External links

• Weather: Ibex Peak

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