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is significant as the summit rises 1,585 metres (5,200 feet) above
Silverhope Creek in five kilometres (3.1 miles) and 1,128 metres (3,700 feet) above the Sumallo in three kilometres (1.86 mile). The mountain's toponym was officially adopted on April 7, 1955, by the
372:. 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
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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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which is the nearest higher neighbor. Precipitation runoff from the peak's west slope drains to the
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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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via
Silverhope Creek, whereas the north and east slopes drain into the
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The North
Cascades feature some of the most rugged topography in the
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is a 2,169-metre (7,116-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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634:Lance Corporal James Adam Forddred:
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368:with craggy peaks, ridges, and deep
16:Mountain in British Columbia, Canada
793:Two-thousanders of British Columbia
311:and 3 km (2 mi) north of
479:"Mount Forddred, British Columbia"
330:Geographical Names Board of Canada
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683:Places adjacent to Mount Forddred
620:. University of Washington Press.
813:Yale Division Yale Land District
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450:Geography of the North Cascades
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445:Geography of British Columbia
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535:Geographical Names Data Base
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173:Show map of British Columbia
170:Location in British Columbia
49:2,169 m (7,116 ft)
616:Kruckeberg, Arthur (1991).
303:which is a subrange of the
82:2.97 km (1.85 mi)
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393:volcanic igneous activity
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646:Mount Forddred (photo):
540:Natural Resources Canada
59:127 m (417 ft)
401:continental lithosphere
203:Mount Forddred (Canada)
122:49.20250°N 121.28667°W
33:North aspect, centered
568:BC Geographical Names
440:Mountains portal
385:North American Plate
127:49.20250; -121.28667
118: /
640:Weather forecast:
325:Topographic relief
206:Show map of Canada
39:Highest point
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317:Fraser River
301:Skagit Range
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273:Skagit River
251:Skagit Range
245:Parent range
765:Mount Payne
507:Bivouac.com
412:Pleistocene
410:During the
313:Mount Payne
295:Description
125: /
113:121°17′12″W
100:Coordinates
70:Mount Payne
65:Parent peak
787:Categories
695:Eaton Peak
574:2023-08-20
545:2023-08-20
512:2023-08-20
488:2023-08-20
456:References
374:ecoregions
291:, Canada.
110:49°12′09″N
55:Prominence
138:Geography
78:Isolation
72:(2,468 m)
45:Elevation
427:See also
421:faulting
405:terranes
262:Topo map
235:District
225:Province
403:called
397:oceanic
360:Geology
340:Climate
217:Country
88:Listing
648:Flickr
595:
417:Uplift
381:Eocene
334:Sardis
220:Canada
344:Most
593:ISBN
419:and
399:and
309:Hope
270:92H3
287:of
267:NTS
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
