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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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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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state. The mountain is 1,459 meters high and is located at the western edge of the
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389:"Tenerife: desde las antípodas hasta la Luna | Diario de Avisos"
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of the river valleys is a result of that recent glaciation.
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from Mount
Teneriffe drains into tributaries of the
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16:Mountain in Washington (state), United States
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232:Mount Baker-Snoqualmie National Forest
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457:Mountains of King County, Washington
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254:Mount Teneriffe is located in the
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462:Mountains of Washington (state)
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321:Geography of Washington (state)
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366:. peakery.com. Archived from
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46:4,788 ft (1,459 m)
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218:is a mountain located in
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258:climate zone of western
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391:. diariodeavisos.com
84:47.5090°N 121.6952°W
230:on land managed by
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298:Epoch. During the
89:47.5090; -121.6952
36:Highest point
272:Cascade Mountains
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393:. Retrieved
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372:. Retrieved
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187:Parent range
300:Pleistocene
220:King County
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75:121°41′43″W
62:Coordinates
451:Categories
395:2016-11-27
374:2016-11-27
327:References
224:Washington
133:Washington
72:47°30′32″N
52:Prominence
100:Geography
42:Elevation
315:See also
309:faulting
240:Tenerife
208:Mount Si
200:Topo map
420:, p. 16
290:Geology
262:. Most
250:Climate
418:Beckey
305:Uplift
296:Eocene
280:runoff
244:Spain
307:and
205:USGS
242:in
222:of
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
