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onto the
Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer
393:. 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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in this area. The history of the formation of the
Cascade Mountains dates back millions of years ago to the late
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danger. The months July through
September offer the most favorable weather for viewing or climbing this peak.
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Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
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months, there is often little or no cloud cover during the summer. Because of
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is set 4 miles (6.4 km) to the northeast on the opposite side of the
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The North
Cascades features some of the most rugged topography in the
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Beebe
Mountain (left) and Elija Ridge seen from the north at
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16:Mountain in Washington (state), United States
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582:The Natural History of Puget Sound Country
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527:United States Department of the Interior
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158:Location of Beebe Mountain in Washington
642:Mountains of Whatcom County, Washington
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273:is a 7,416-foot (2,260-metre) mountain
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313:via Granite Creek and Panther Creek.
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662:North Cascades of Washington (state)
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389:with craggy peaks, ridges, and deep
518:Geographic Names Information System
337:, and travel northeast toward the
289:. It is situated on the border of
191:Beebe Mountain (the United States)
14:
584:. University of Washington Press.
321:Beebe Mountain is located in the
293:. Its nearest higher neighbor is
33:Beebe Mountain seen from the east
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637:Mountains of Washington (state)
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523:United States Geological Survey
161:Show map of Washington (state)
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667:North American 2000 m summits
194:Show map of the United States
657:North Cascades National Park
615:North Cascades National Park
489:"Beebe Mountain - 7,416' WA"
468:"Beebe Mountain, Washington"
429:about 50 million years ago.
309:on the mountain drains into
291:North Cascades National Park
49:7,416 ft (2,260 m)
580:Kruckeberg, Arthur (1991).
82:1.56 mi (2.51 km)
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59:1,056 ft (320 m)
411:volcanic igneous activity
341:. As fronts approach the
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620:Beebe Mountain weather:
325:climate zone of western
419:continental lithosphere
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303:North Cascades Highway
110:48.66306°N 120.92417°W
617:National Park Service
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403:North American Plate
115:48.66306; -120.92417
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360:maritime influence
39:Highest point
622:Mountain Forecast
339:Cascade Mountains
333:originate in the
323:marine west coast
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593:External links
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472:Peakbagger.com
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427:North Cascades
409:, episodes of
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343:North Cascades
331:weather fronts
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271:Beebe Mountain
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223:Parent range
434:Pleistocene
432:During the
299:McKay Ridge
295:Elija Ridge
113: /
101:120°55′27″W
88:Coordinates
70:Elija Ridge
65:Parent peak
631:Categories
532:2020-07-27
498:2020-07-27
449:References
395:ecoregions
287:Washington
283:U.S. state
263:Scrambling
213:Washington
98:48°39′47″N
72:(7,739 ft)
55:Prominence
364:avalanche
311:Ross Lake
126:Geography
78:Isolation
45:Elevation
443:faulting
423:terranes
355:snowfall
250:Climbing
236:Topo map
205:Location
563:, p. 16
421:called
415:oceanic
370:Geology
329:. Most
317:Climate
281:in the
561:Beckey
439:Uplift
399:Eocene
307:runoff
275:summit
441:and
417:and
351:rain
241:USGS
353:or
285:of
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
