Twisp Mountain

Weather fronts originating in the Pacific Ocean travel east toward the Cascade Mountains. As fronts approach the North Cascades, 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. As a result, the North Cascades experience high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche 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.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.

In addition to Twisp Mountain, the Twisp name is applied to Twisp River, Twisp Pass, and the community of Twisp. The common explanation is that Twisp comes from the Okanagan placename /txʷəc'p/,{{cite book|url=https://books.google.com/books?id=5XfxzCm1qa4C&pg=PA526|title=Native American placenames of the United States|last=Bright|first=William|publisher=University of Oklahoma Press|year=2004|isbn=978-0-8061-3598-4|page=526|author-link=William Bright|access-date=11 April 2011}} which possibly translates to wasp, yellowjacket, or the sound made by a wasp.{{Cite web|url=https://historylink.org/File/9943|title=Twisp — Thumbnail History|last=West|first=Karen|date=October 5, 2011|website=HistoryLink.org|access-date=August 18, 2019}} This mountain's toponym has been officially adopted by the United States Board on Geographic Names.

The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, ridges, and deep glacial valleys. 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 ecoregions in this area.

The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch.{{cite book|last=Kruckeberg|first=Arthur|title=The Natural History of Puget Sound Country|publisher=University of Washington Press|year=1991}} With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.

During the Pleistocene 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. Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades.

{{Portal|Mountains}}

Geography of the North Cascades

{{reflist}}

• Weather: [https://www.yr.no/en/forecast/daily-table/2-5814309/United%20States/Washington/Okanogan/Twisp%20Mountain Twisp Mountain]
• [https://www.nps.gov/noca/index.htm North Cascades National Park] National Park Service

Category:Mountains of Chelan County, Washington

Category:Mountains of Okanogan County, Washington

Category:North Cascades National Park

Category:North Cascades of Washington (state)

Category:Two-thousanders of the United States