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danger. 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. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade
428:. 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 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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Crest very rarely experience temperatures below 0 °F (−18 °C) or above 80 °F (27 °C).
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Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
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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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359:. The nearest higher peak is Buckeye Peak, 3.34 miles (5.38 km) to the west. Precipitation
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The North
Cascades features some of the most rugged topography in the
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coming off the
Pacific Ocean travel northeast toward the
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451:persisted. In addition, small fragments of the
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16:Mountain in Washington (state), United States
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391:climate zone of western North America. Most
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635:The Natural History of Puget Sound Country
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673:Mountains of Snohomish County, Washington
339:state. It is located four miles south of
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323:is a 5,825-foot-elevation (1,775-meter)
164:Location of Jumbo Mountain in Washington
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688:Mount Baker-Snoqualmie National Forest
353:Mount Baker-Snoqualmie National Forest
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424:with craggy peaks, ridges, and deep
378:Jumbo Mountain seen from Highway 530
197:Jumbo Mountain (the United States)
40:Jumbo Mountain seen from the north
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637:. University of Washington Press.
387:Jumbo Mountain is located in the
514:Geology of the Pacific Northwest
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668:Mountains of Washington (state)
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509:Geography of the North Cascades
167:Show map of Washington (state)
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693:North American 1000 m summits
327:near the western edge of the
200:Show map of the United States
568:"Jumbo Mountain, Washington"
541:"Jumbo Mountain WA - 5,825'"
467:about 50 million years ago.
351:on land administered by the
56:5,825 ft (1,775 m)
633:Kruckeberg, Arthur (1991).
88:3.34 mi (5.38 km)
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66:1,765 ft (538 m)
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449:volcanic igneous activity
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651:Jumbo Mountain weather:
349:Boulder River Wilderness
347:. It is situated in the
243:Boulder River Wilderness
19:Not to be confused with
457:continental lithosphere
116:48.195654°N 121.59959°W
21:Jumbo Mountain (Canada)
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341:Darrington, Washington
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345:Mountain Loop Highway
121:48.195654; -121.59959
441:North American Plate
365:Stillaguamish River
239:Protected area
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405:maritime influence
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46:Highest point
653:Mountain Forecast
397:Cascade Mountains
389:marine west coast
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646:External links
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572:Peakbagger.com
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465:North Cascades
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393:weather fronts
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321:Jumbo Mountain
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306:Easiest route
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548:. Retrieved
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284:Type of rock
272:Helena Ridge
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251:Parent range
472:Pleistocene
470:During the
119: /
107:121°35′59″W
94:Coordinates
72:Parent peak
662:Categories
550:2024-04-07
520:References
430:ecoregions
369:Sauk River
337:Washington
312:Scrambling
223:Washington
104:48°11′44″N
62:Prominence
409:avalanche
293:Sandstone
233:Snohomish
132:Geography
84:Isolation
52:Elevation
487:See also
481:faulting
461:terranes
357:elephant
299:Climbing
264:Topo map
616:, p. 16
601:, p. 15
459:called
453:oceanic
416:Geology
383:Climate
278:Geology
211:Country
614:Beckey
599:Beckey
477:Uplift
437:Eocene
361:runoff
325:summit
229:County
331:, in
289:Shale
219:State
479:and
455:and
367:and
291:and
269:USGS
335:of
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