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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 last glacial retreat in the area began about 14,000 years ago and was north of the Canada–US border by 10,000 years ago. The U-shaped cross section
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originating in the
Pacific Ocean travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snow onto the Cascades
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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.
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is significant as the summit rises nearly 3,600 feet (1,097 meters) above the Middle Fork
Snoqualmie River in approximately one mile (1.6 km). The nearest higher peak is
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in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the
Cascade Range.
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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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of the river valleys is a result of that recent glaciation.
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is a 4,523-foot (1,379-metre) mountain summit located in
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286:state. It is located at the western edge of the
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330:climate zone of western North America. Most
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485:The Natural History of Puget Sound Country
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317:The Pulpit (left) with Preacher Mountain
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515:Mount Baker-Snoqualmie National Forest
292:Mount Baker-Snoqualmie National Forest
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505:Mountains of King County, Washington
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487:. University of Washington Press.
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154:Show map of Washington (state)
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520:North American 1000 m summits
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184:Show map of the United States
46:4,523 ft (1,379 m)
483:Kruckeberg, Arthur (1991).
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419:"The Pulpit - 4,523' WA"
398:"The Pulpit, Washington"
106:47.521416°N 121.551844°W
56:483 ft (147 m)
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111:47.521416; -121.551844
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290:on land managed by
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360:Epoch. During the
341:maritime influence
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296:Topographic relief
36:Highest point
328:marine west coast
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67:Preacher Mountain
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259:Easiest route
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426:. Retrieved
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268:class 4
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225:Parent range
362:Pleistocene
280:King County
109: /
97:121°33′07″W
84:Coordinates
62:Parent peak
499:Categories
442:The Pulpit
428:2024-04-10
377:References
284:Washington
276:The Pulpit
265:Scrambling
207:Washington
178:The Pulpit
148:The Pulpit
94:47°31′17″N
52:Prominence
30:The Pulpit
19:The Pulpit
345:avalanche
122:Geography
74:Isolation
42:Elevation
371:faulting
252:Climbing
238:Topo map
468:, p. 16
352:Geology
322:Climate
195:Country
466:Beckey
367:Uplift
358:Eocene
304:runoff
213:County
203:State
369:and
243:USGS
217:King
282:of
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
