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348:). As a result, the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. With its impressive height, Ice Box can have snow on it in late-spring and early-fall, and can be very cold in the winter.
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 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, the area around Ice Box is a bit drier than areas to the west. Summers can bring warm temperatures and occasional thunderstorms. Most
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from the mountain drains east into Ice Creek, or west into Box Creek. This peak is positioned between these two creeks, hence its name.
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that is 14.7 mi (23.7 km) west of Ice Box, began forming in the mid-Pleistocene. Due to
Glacier Peak's proximity to Ice Box,
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is 1.3 miles (2.1 km) to the southeast. Ice Box is situated 1.25 miles (2.01 km) south of Ice Lakes in the
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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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The North
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is an 8,112-foot (2,473-metre) mountain summit located in the
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Ice Box (right) from trail to Ice Lakes, (Peak 7919 to left)
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are set 1.9 miles (3.1 km) to the northeast, and
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16:Mountain in Washington (state), United States
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549:The Natural History of Puget Sound Country
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33:Ice Box (summit left) from Upper Ice Lake
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368:with craggy peaks, ridges, and deep
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551:. University of Washington Press.
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565:Ice Box reflected in Ice Lakes:
478:Geology of the Pacific Northwest
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599:Mountains of Washington (state)
473:Geography of Washington (state)
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161:Show map of Washington (state)
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614:North American 2000 m summits
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194:Show map of the United States
49:8,112 ft (2,473 m)
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547:Kruckeberg, Arthur (1991).
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191:Ice Box (the United States)
82:1.51 mi (2.43 km)
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439:View from Mt. Maude with
393:volcanic igneous activity
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110:48.112143°N 120.79555°W
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158:Location in Washington
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385:North American Plate
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571:Weather forecast:
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324:Lying east of the
39:Highest point
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383:Epoch. With the
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567:Flickr photo
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514:. Retrieved
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405:volcanic ash
397:Glacier Peak
395:persisted.
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266:class 3
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222:Parent range
577:Ice Box at
416:Pleistocene
414:During the
302:Chilly Peak
294:Mount Maude
113: /
101:120°47′44″W
88:Coordinates
70:Mount Maude
65:Parent peak
588:Categories
516:2020-06-11
484:References
447:upper left
374:ecoregions
213:Washington
98:48°06′44″N
55:Prominence
507:"Ice Box"
126:Geography
78:Isolation
45:Elevation
431:See also
425:faulting
306:Okanogan
253:Climbing
239:Topo map
205:Location
445:Ice Box
441:Freezer
352:Geology
326:Cascade
320:Climate
274:Ice Box
247:Trinity
185:Ice Box
152:Ice Box
22:Ice Box
421:Uplift
409:tephra
381:Eocene
314:runoff
215:, U.S.
284:, in
423:and
407:and
399:, a
244:USGS
288:of
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308:-
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
