444:). 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. 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.
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period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. The U-shaped cross sections of the river valleys are a result of recent glaciation.
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in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North
Cascades area.
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is significant as the summit rises 1,000 metres (3,280 feet) above Eleven Mile Creek in 1.5 kilometre (0.93 mile).
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The history of the formation of the
Cascade Mountains dates back millions of years ago to the late
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from the peak drains into Eight Mile and Eleven Mile creeks which are both tributaries of the
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Macleod Peak is the third-highest summit of Manson Ridge which is a subrange of the
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The mountain's toponym was officially adopted on April 7, 1955, by the
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The North
Cascades features some of the most rugged topography in the
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is a 2,176-metre (7,139-foot) mountain summit located in the
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originate in the
Pacific Ocean, and travel east toward the
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created the North
Cascades about 50 million years ago.
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which is the nearest higher neighbor. Precipitation
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629:Cascade Alpine Guide, Climbing and High Routes
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349:Pilot Officer Alexander Harvey Macleod, from
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615:The Natural History of Puget Sound Country
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652:Pilot Officer Alexander Harvey MacLeod:
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365:with craggy peaks, ridges, and deep
322:and 2.2 km (1 mi) west of
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16:Mountain in British Columbia, Canada
802:Two-thousanders of British Columbia
343:Geographical Names Board of Canada
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617:. University of Washington Press.
822:Yale Division Yale Land District
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498:"MacLeod Peak, British Columbia"
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253:Yale Division Yale Land District
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695:Places adjacent to Macleod Peak
471:Geography of the North Cascades
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654:Canadian Virtual War Memorial
525:"Macleod Peak, Peakvisor.com"
466:Geography of British Columbia
345:. The mountain's name honors
93:Mountains of British Columbia
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553:Geographical Names Data Base
188:Show map of British Columbia
185:Location in British Columbia
49:2,176 m (7,139 ft)
613:Kruckeberg, Arthur (1991).
82:2.19 km (1.36 mi)
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59:420 m (1,378 ft)
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436:. As fronts approach the
390:volcanic igneous activity
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558:Natural Resources Canada
347:Royal Canadian Air Force
148:Alexander Harvey Macleod
398:continental lithosphere
122:49.32861°N 121.21306°W
586:BC Geographical Names
218:Macleod Peak (Canada)
461:Mountains portal
382:North American Plate
127:49.32861; -121.21306
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658:Weather forecast:
336:Topographic relief
221:Show map of Canada
39:Highest point
807:Canadian Cascades
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772:Eleven Mile Creek
434:Cascade Mountains
300:Canadian Cascades
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581:"Macleod Peak"
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548:"Macleod Peak"
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502:Peakbagger.com
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324:Mount Hatfield
316:Hozameen Range
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779:Mount Outram
775:Johnson Peak
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660:Macleod Peak
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296:Macleod Peak
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260:Parent range
212:Macleod Peak
179:Macleod Peak
70:Mount Outram
33:South aspect
22:Macleod Peak
409:Pleistocene
407:During the
310:Description
125: /
113:121°12′47″W
100:Coordinates
65:Parent peak
796:Categories
592:2023-08-19
563:2023-08-19
530:2023-08-19
507:2023-08-19
477:References
371:ecoregions
306:, Canada.
110:49°19′43″N
55:Prominence
153:Geography
144:Etymology
78:Isolation
72:(2,461 m)
45:Elevation
448:See also
418:faulting
402:terranes
277:Topo map
250:District
240:Province
424:Climate
400:called
394:oceanic
357:Geology
232:Country
88:Listing
635:
414:Uplift
378:Eocene
351:Sardis
328:runoff
235:Canada
138:Naming
428:Most
633:ISBN
416:and
396:and
320:Hope
288:Hope
285:92H6
302:of
282:NTS
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688:e
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.