Macleod Peak

Macleod Peak
Macleod Peak
	South aspect
Highest point
Elevation	2,176 m (7,139 ft)
Prominence	420 m (1,378 ft)
Parent peak	Mount Outram (2,461 m)
Isolation	2.19 km (1.36 mi)
Listing	Mountains of British Columbia
Coordinates	49°19′43″N121°12′47″W / 49.32861°N 121.21306°W
Naming
Etymology	Alexander Harvey Macleod
Geography
	Macleod Peak Location in British Columbia Macleod Peak Macleod Peak (Canada)
Country	Canada
Province	British Columbia
District	Yale Division Yale Land District
Parent range	Hozameen Range ; Canadian Cascades
Topo map	NTS 92H6 Hope

Last updated January 07, 2024

Macleod Peak is a 2,176-metre (7,139-foot) mountain summit located in the Canadian Cascades of British Columbia, Canada.

Description

Macleod Peak is the third-highest summit of Manson Ridge which is a subrange of the Hozameen Range.^[1] It is situated 17 km (11 mi) southeast of Hope and 2.2 km (1 mi) west of Mount Hatfield which is the nearest higher neighbor.^[2] Precipitation runoff from the peak drains into Eight Mile and Eleven Mile creeks which are both tributaries of the Nicolum River. Topographic relief is significant as the summit rises 1,000 metres (3,280 feet) above Eleven Mile Creek in 1.5 kilometre (0.93 mile).

The mountain's toponym was officially adopted on April 7, 1955, by the Geographical Names Board of Canada.^[3]^[4] The mountain's name honors Royal Canadian Air Force Pilot Officer Alexander Harvey Macleod, from Sardis, who was killed in WWII action during air operations over Europe on October 15, 1944, at age 22.^[4]

Geology

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

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 leaving deposits of rock debris.^[5] The U-shaped cross sections 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.

Climate

Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall (orographic lift). As a result, the west side of the North Cascades experiences higher precipitation than the east side. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.^[6] As a result, the Cascade Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −10 °C with wind chill factors below −20 °C. The months of July through September offer the most favorable weather for viewing and climbing Macleod Peak.

Related Research Articles

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Remmel Mountain, also known as Mount Remmel, is a prominent 8,690-foot (2,650-metre) mountain summit located in Okanogan County in Washington state. It is the highest point in the Cathedral Range, which is a subrange of the Okanogan Range in the North Cascades. The mountain is situated 5 miles (8.0 km) south of the Canada–United States border, on the eastern side of the Cascade crest, in the Pasayten Wilderness, on land managed by the Okanogan–Wenatchee National Forest. The nearest higher peak is Mount Lago, 16.8 miles (27.0 km) to the west-southwest, and Amphitheater Mountain lies 3.6 miles (5.8 km) to the north. Remmel is the third-highest summit of the Okanogan Range following Mount Lago (8,745 ft), and Robinson Mountain (8,726 ft). These three peaks follow Jack Mountain {9,075 ft} as the highest peaks in the Pasayten Wilderness. Remmel is the most prominent mountain in the Pasayten Wilderness. Precipitation runoff from Remmel Mountain drains into the Chewuch River basin.

Apex Mountain is an 8,297-foot (2,529-metre) mountain summit located in Okanogan County in Washington state. It is part of the Okanogan Range which is a sub-range of the North Cascades and Cascade Range. The mountain is situated 2.5 miles (4.0 km) south of the Canada–United States border, on the east side of the Cascade crest, in the Pasayten Wilderness, on land managed by the Okanogan–Wenatchee National Forest. The nearest higher peak is Amphitheater Mountain, 2.35 miles (3.78 km) to the west-northwest. The Pacific Northwest Trail traverses the northern slopes of Apex Mountain as it crosses Apex Pass. Precipitation runoff from Apex Mountain drains west into Cathedral Creek, or east into Tungsten Creek, both tributaries of the Chewuch River.

Windy Peak is an 8,333-foot (2,540-metre) mountain summit located in Okanogan County in Washington state. It is part of the Okanogan Range which is a sub-range of the North Cascades and Cascade Range. The mountain is situated 5 miles (8.0 km) south of the Canada–United States border, on the east side of the Cascade crest, in the Pasayten Wilderness, on land managed by the Okanogan–Wenatchee National Forest. The nearest higher peak is Haystack Mountain, 9.24 miles (14.87 km) to the northwest in Canada. Precipitation runoff from Windy Peak drains into tributaries of the Methow River and Similkameen River.

Castle Peak is a prominent 8,306-foot (2,532-metre) mountain summit located in the Hozameen Range of the North Cascades, on the shared border between Okanogan County and Whatcom County of Washington state. The mountain is situated 1 mile (1.6 km) south of the Canada–United States border, on the Cascade crest, in the Pasayten Wilderness, on land managed by the Okanogan–Wenatchee National Forest. The nearest higher peak is Jack Mountain, 14.8 miles (23.8 km) to the south-southwest. Castle Peak is the second highest summit of the Hozameen Range following Jack Mountain. Castle Peak is the fifth-most prominent mountain in the Pasaten Wilderness. Precipitation runoff from the mountain drains east into Castle Creek, a tributary of the Similkameen River, or west into tributaries of the Skagit River.

Tiffany Mountain is an 8,245-foot (2,513-metre) mountain summit located in Okanogan County in Washington state. It is the highest point in the Tiffany Range, which is a sub-range of the Okanogan Range. The mountain is situated on the east side of the Cascade crest, on land managed by the Okanogan–Wenatchee National Forest. The nearest higher peak is Windy Peak, 18 miles (29 km) to the north. Precipitation runoff from Tiffany Mountain drains into tributaries of the Columbia River.

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Frosty Mountain is a 2,426-metre (7,959-foot) mountain summit located in the Canadian Cascades of southwestern British Columbia, Canada. It is situated 4 km (2 mi) south of Lightning Lake, 1.3 km (1 mi) north of the Canada–United States border, and 3.6 km (2 mi) north-northeast of Castle Peak, which is its nearest higher peak. Frosty Mountain is the highest peak in E. C. Manning Provincial Park, and is part of the Hozameen Range which is a subrange of the Cascade Range. It has a lower elevation subsidiary peak known as Frosty Mountain East which is labelled as Frosty Mountain on some maps. The Frosty Mountain name was officially adopted on March 31, 1924, by the Geographical Names Board of Canada. The peak was first climbed on September 2, 1904, by Sledge Tatum and George Loudon Jr., two members of a Boundary Survey group led by Edward C. Barnard. Precipitation runoff from the peak drains into headwaters of Frosty Creek, as well as other tributaries of the Similkameen River.

Mount Outram is a prominent 2,461-metre (8,074-foot) mountain summit located in the Canadian Cascades of southwestern British Columbia, Canada. It is the fourth-highest summit in the Hozameen Range, and highest point of the Manson Ridge subrange. It is situated 23 km (14 mi) southeast of Hope, and 14.5 km (9 mi) north-northeast of Silvertip Mountain, its nearest higher peak. Precipitation runoff from the peak drains into tributaries of the Coquihalla and Skagit Rivers. The mountain was known as Beaver Mountain as early as 1930 before being named for Sir James Outram, 1st Baronet, and being officially adopted October 6, 1936, by the Geographical Names Board of Canada. The first ascent of the mountain was made August 12, 1924, by Fred Perry, Herbert Selwood, Leslie Ford, and T.L. Thacker.

Yellow Aster Butte is a 6,241-foot (1,902-metre) Skagit Range summit located three miles south of the Canada–United States border, in Whatcom County of Washington state. It is situated within the Mount Baker Wilderness, on land managed by Mount Baker-Snoqualmie National Forest. The nearest higher neighbor is Winchester Mountain, 1.77 miles (2.85 km) to the east, and Mount Larrabee is set 2.3 miles (3.7 km) to the northeast. The summit offers views of Mount Larrabee, Tomyhoi Peak, American Border Peak, Canadian Border Peak, Mount Shuksan, and Mount Baker. Precipitation runoff on the north side of the mountain drains into Tomyhoi Creek, whereas the west side of the mountain drains into Damfino Creek, and the south slope is drained by Swamp Creek.

Baby Munday Peak is a 2,250-meter-elevation (7,382-foot) mountain summit located in the Cheam Range of British Columbia, Canada.

Knight Peak is a 2,235-meter-elevation (7,333-foot) mountain summit located in the Cheam Range of British Columbia, Canada.

Red Face Mountain is a 7,141-foot-elevation (2,177-meter) summit in Whatcom County of Washington state.

Grimface Mountain is a mountain summit in British Columbia, Canada.

Mount Hatfield is a 2,227-metre (7,306-foot) mountain summit located in the Canadian Cascades of British Columbia, Canada.

Mount Rideout is a 2,445-metre (8,022-foot) mountain summit located in the Canadian Cascades of British Columbia, Canada.

Mount Forddred is a 2,169-metre (7,116-foot) mountain summit located in the Canadian Cascades of British Columbia, Canada.

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References

1 2 3 4 "MacLeod Peak, British Columbia". Peakbagger.com. Retrieved 2023-08-19.
1 2 "Macleod Peak, Peakvisor.com" . Retrieved 2023-08-19.
1 2 "Macleod Peak". Geographical Names Data Base . Natural Resources Canada . Retrieved 2023-08-19.
1 2 "Macleod Peak". BC Geographical Names . Retrieved 2023-08-19.
1 2 3 4 Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.
↑ Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes, Vol. 3, Mountaineers Books (2008), ISBN 9781594854309.

External links

Pilot Officer Alexander Harvey MacLeod: Canadian Virtual War Memorial
Weather forecast: Macleod Peak

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[pb-1] 1 2 3 4 "MacLeod Peak, British Columbia". Peakbagger.com. Retrieved 2023-08-19.

[peakvisor-2] 1 2 "Macleod Peak, Peakvisor.com" . Retrieved 2023-08-19.

[cgndb-3] 1 2 "Macleod Peak". Geographical Names Data Base . Natural Resources Canada . Retrieved 2023-08-19.

[bcgnis-4] 1 2 "Macleod Peak". BC Geographical Names . Retrieved 2023-08-19.

[Kruckeberg-5] 1 2 3 4 Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.

[Beckey,_2008-6] Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes, Vol. 3, Mountaineers Books (2008), ISBN 9781594854309.

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