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473:), 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 Guanaco Peak.
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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
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period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape. The U-shaped cross section of the river valleys is 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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307:. It is the highest summit of the Anderson River Group, a subset of the North Cascades. It is situated 8 km (5 mi) northwest of
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Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification".
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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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party. The mountain's name was officially adopted on
February 5, 1976, by the
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The North
Cascades features some of the most rugged topography in the
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is a 2,127-metre (6,978-foot) mountain located in the
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33:Vicuna Peak (left) with Guanaco Peak (right)
469:where they are forced upward by the range (
648:The Natural History of Puget Sound Country
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518:Guanaco Peak seen from the summit of
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16:Mountain in British Columbia, Canada
708:Two-thousanders of British Columbia
409:with craggy peaks and ridges, deep
337:Geographical Names Board of Canada
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650:. University of Washington Press.
449:, Guanaco Peak is located in the
327:. The mountain was named for the
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728:Yale Division Yale Land District
566:"Guanaco Peak, British Columbia"
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221:Yale Division Yale Land District
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499:Geography of the North Cascades
69:Stoyoma Mountain (2267 m)
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447:Köppen climate classification
80:Mountains of British Columbia
615:Geographical Names Data Base
386:Vicuna and Guanaco in winter
379:about 50 million years ago.
160:Show map of British Columbia
157:Location in British Columbia
59:1,002 m (3,287 ft)
49:2,127 m (6,978 ft)
646:Kruckeberg, Arthur (1991).
504:Geology of British Columbia
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361:volcanic igneous activity
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620:Natural Resources Canada
453:climate zone of western
663:Hydrol. Earth Syst. Sci
369:continental lithosphere
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109:49.66194°N 121.14333°W
595:BC Geographical Names
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190:Guanaco Peak (Canada)
353:North American Plate
114:49.66194; -121.14333
321:East Anderson River
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691:Weather forecast:
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268:1981 Karl Ricker,
193:Show map of Canada
39:Highest point
713:Canadian Cascades
461:originate in the
451:marine west coast
309:Coquihalla Summit
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351:Epoch. With the
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610:"Guanaco Peak"
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590:"Guanaco Peak"
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570:Peakbagger.com
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542:"Guanaco Peak"
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377:North Cascades
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278:Easiest route
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693:Guanaco Peak
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375:created the
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333:first ascent
293:Guanaco Peak
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285:class 3
264:First ascent
228:Parent range
184:Guanaco Peak
151:Guanaco Peak
22:Guanaco Peak
546:Bivouac.com
520:Vicuna Peak
440:Alpaca Peak
436:Vicuna Peak
392:Pleistocene
390:During the
313:Vicuna Peak
112: /
100:121°08′36″W
87:Coordinates
65:Parent peak
702:Categories
625:2019-11-19
575:2019-11-19
551:2019-11-19
510:References
420:ecoregions
270:BCMC Party
97:49°39′43″N
55:Prominence
675:1027-5606
125:Geography
45:Elevation
477:See also
400:faulting
373:terranes
258:Climbing
241:Topo map
218:District
204:Location
457:. Most
426:Climate
415:granite
371:called
365:oceanic
343:Geology
329:guanaco
252:Spuzzum
75:Listing
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413:, and
396:Uplift
349:Eocene
317:runoff
305:Canada
212:Canada
249:92H11
671:ISSN
398:and
367:and
246:NTS
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
