To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Big Craggy Peak

From Wikipedia, the free encyclopedia

Big Craggy Peak
Big Craggy Peak seen from northeast
Highest point
Elevation8,478 ft (2,584 m)[1]
Prominence3,133 ft (955 m)[1]
Parent peakMonument Peak (8,592 ft)[1]
Isolation0.96 mi (1.54 km)[1]
ListingHighest Peaks in Washington
Coordinates48°45′46″N 120°19′41″W / 48.7629004°N 120.3280967°W / 48.7629004; -120.3280967[2]
Geography
Big Craggy Peak is located in Washington (state)
Big Craggy Peak
Big Craggy Peak
Location in Washington
Big Craggy Peak is located in the United States
Big Craggy Peak
Big Craggy Peak
Big Craggy Peak (the United States)
CountryUnited States
StateWashington
CountyOkanogan
Protected areaOkanogan–Wenatchee National Forest[3]
Parent rangeOkanogan Range
North Cascades
Cascade Range
Topo mapUSGS Billy Goat Mountain
Climbing
Easiest routeclass 2+ scrambling[1]

Big Craggy Peak is a prominent 8,478-foot (2,584-metre) mountain summit in western Okanogan County of Washington state, USA.[1] It is part of the Okanogan Range which is a subrange of the North Cascades. This remote mountain is located 12.5 mi (20.1 km) north-northeast of Mazama on land administered by the Okanogan–Wenatchee National Forest. Big Craggy has two subsidiary peaks, North Peak (8,205-ft), and West Craggy (8,372-ft), the latter set on the Pasayten Wilderness boundary. The nearest higher peak is Monument Peak, 10 miles (16 km) to the west-northwest.[3] Big Craggy Peak ranks 60th on Washington's highest 100 peaks, and 62nd on the "Bulger List".[3] Precipitation runoff from Big Craggy drains into Eightmile Creek which is a tributary of the Chewuch River. Topographic relief is significant as the summit rises approximately 4,400 feet (1,300 meters) above Eightmile Creek in 1.25 mile (2 km).

Climate

Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of 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.[4]

Geology

The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, spires, 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.

The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch.[5] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted.[5] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.[5]

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.[5] 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 area.

See also

References

  1. ^ a b c d e f "Big Craggy Peak - 8,478' WA". listsofjohn.com. Retrieved 2024-04-04.
  2. ^ "Big Craggy Peak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2024-04-04.
  3. ^ a b c "Big Craggy Peak, Washington". Peakbagger.com.
  4. ^ Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  5. ^ a b c d Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.

External links

This page was last edited on 4 April 2024, at 06:43
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.