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447:). As a result, 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 months, there is often little or no cloud cover during the summer.
415:, and many others. This mountain was named for Billy McGregor, a Stehekin Valley resident who had a cabin and homestead at the base of this mountain during the 1890s. In May 1901, Billy disappeared overnight from a boat docked in Lake Chelan, and was never seen or heard from again.
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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 the various climate differences. These climate differences lead to vegetation variety defining the
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traverses the western base of this mountain, and the strenuous 7.7-mile (12.4 km) McGregor
Mountain Trail gains 6,400 feet (1,920 m) of elevation to take hikers within a half-mile of the summit. Reaching the summit requires exposed
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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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is needed if the trail remains covered by snowpack. The summit was the site of an old fire lookout cabin from 1923 until 1955, but now has a radio
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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 since the southern aspect of the mountain rises 6,600 feet above this river in approximately two miles. The famous
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Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. page 289.
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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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McGregor
Mountain's south aspect. Enlarge to see the repeater visible on the summit
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Ladies of the Lake: Tales of
Transportation, Tragedy, and Triumph on Lake Chelan
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The North
Cascades features some of the most rugged topography in the
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for the
National Park Service. The views from the top include
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originating in the
Pacific Ocean travel northeast toward the
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in the northern Methow
Mountains, on the shared border of
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338:state. McGregor Mountain is situated northwest of
829:Places adjacent to McGregor Mountain (Washington)
362:from the mountain drains into tributaries of the
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725:McGregor Mountain Trail, National Park Service
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27:Mountain in Washington (state), United States
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587:Sandalee Glacier and McGregor in upper left
156:Location of McGregor Mountain in Washington
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758:The Natural History of Puget Sound Country
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318:is an 8,143-foot (2,482-metre) elevation
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706:United States Department of the Interior
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954:Mountains of Chelan County, Washington
379:the final 1,100 feet (330 m), and an
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189:McGregor Mountain (the United States)
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348:Lake Chelan National Recreation Area
697:Geographic Names Information System
467:with craggy peaks and ridges, deep
739:, Point Publishing, 1998, page 50.
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760:. University of Washington Press.
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553:Geology of the Pacific Northwest
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949:Mountains of Washington (state)
702:United States Geological Survey
660:"McGregor Mountain, Washington"
631:"McGregor Mountain - 8,143' WA"
558:Geography of the North Cascades
44:Southeast aspect, from Stehekin
159:Show map of Washington (state)
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969:North American 2000 m summits
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192:Show map of the United States
964:North Cascades National Park
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515:about 50 million years ago.
344:North Cascades National Park
235:North Cascades National Park
80:6.91 mi (11.12 km)
60:8,143 ft (2,482 m)
18:McGregor Mountain (Cascades)
756:Kruckeberg, Arthur (1991).
350:. The closest community is
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70:2,162 ft (659 m)
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497:volcanic igneous activity
439:. As fronts approach the
423:McGregor Mountain has an
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431:on its northern slopes.
108:48.408178°N 120.798239°W
871:Glacier Peak Wilderness
787:McGregor Mountain Trail
607:McGregor in upper right
593:in lower half of frame)
505:continental lithosphere
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113:48.408178; -120.798239
789:National Park Service
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548:Mountains portal
489:North American Plate
774:McGregor Mountain:
692:"McGregor Mountain"
427:which supports the
372:Pacific Crest Trail
231:Protected area
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780:McGregor Mountain
735:Tom Hackenmiller,
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368:Topographic relief
50:Highest point
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882:McGregor Mountain
776:Mountain Forecast
437:Cascade Mountains
316:McGregor Mountain
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183:McGregor Mountain
150:McGregor Mountain
33:McGregor Mountain
16:(Redirected from
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433:Weather fronts
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364:Stehekin River
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328:North Cascades
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921:Tupshin Peak
911:Bonanza Peak
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709:. Retrieved
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638:. Retrieved
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511:created the
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405:Tupshin Peak
389:Glacier Peak
315:
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282:Type of rock
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243:Parent range
846:Corteo Peak
520:Pleistocene
518:During the
397:Corteo Peak
340:Lake Chelan
111: /
99:120°47′54″W
86:Coordinates
938:Categories
851:Rainy Peak
711:2020-05-16
640:2024-04-08
614:References
478:ecoregions
393:Black Peak
377:scrambling
336:Washington
307:Scrambling
215:Washington
96:48°24′29″N
66:Prominence
409:Dome Peak
124:Geography
76:Isolation
56:Elevation
535:See also
529:faulting
509:terranes
385:repeater
352:Stehekin
294:Climbing
262:Topo map
564:Gallery
507:called
501:oceanic
473:granite
451:Geology
419:Climate
381:ice axe
326:of the
286:Skagit
276:Geology
203:Country
525:Uplift
485:Eocene
471:, and
360:runoff
320:massif
288:gneiss
225:Chelan
221:County
794:PBase
330:, in
211:State
527:and
503:and
346:and
267:USGS
334:of
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589:(
20:)
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