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Buckner Mountain (sometimes called Mount Buckner) is a tall peak in the North Cascades of Washington state and in the Stephen Mather Wilderness of North Cascades National Park. At 9,114 feet (2,778 m) in elevation it is the highest in Skagit County and one of about ten of Washington's non-volcanic peaks above 9,000 feet high.[1] It is ranked as the 14th highest peak in the state,[3] and the third highest peak in North Cascades National Park.[4]

Buckner Mountain
Buckner Mountain from Sahale Mountain
Highest point
Elevation9,114 ft (2,778 m)[1]
Prominence3,034 ft (925 m)[1]
Parent peakGoode Mountain
Coordinates48°29′42″N 120°59′52″W[2]
Geography
Buckner Mountain
Location of Buckner Mountain in Washington
Buckner Mountain
Buckner Mountain (the United States)
LocationChelan and Skagit Counties, Washington, United States
Parent rangeNorth Cascades
Topo mapGoode Mountain
Climbing
First ascentLewis Ryan, 1901-08-01[1]

Description


The mountain has two summits of nearly the same elevation, separated by a ridgeline of a few hundred feet. Sources differ over the exact height of the southwestern summit. The current United States Geological Survey quadrangle shows the southwest summit to have an elevation between 9080 and 9119 feet. According to Peakbagger.com the southwestern peak is the higher one, at 9,114 ft (2,778 m), based on Edward Earl's pixel analysis of the height of the peak as derived from a digital photograph. The broader northeastern peak is agreed to be 9,112 ft (2,777 m).[5] Noted climber Fred Beckey also claims in his Cascade Alpine Guide books that the Southwest summit is two feet higher but gives no source for the claim and this approximation is second-hand since Beckey has never summitted Buckner. Most mountain climbers visit the southwest peak since it is arrived at first via the standard Horseshoe Basin route.[1]

Buckner Mountain, with a prominence of 3,034 feet (925 m), is the 51st most prominent peak in Washington state.[6] The nearest higher peak is Goode Mountain, 4.13 miles (6.65 km) to the east.[1]

Buckner Mountain is located on the border between Chelan and Skagit counties. It is connected to Horseshoe Peak, Boston Peak, and Sahale Mountain to the west by Ripsaw Ridge, which marks the county line for several miles. Cascade Pass is located a few miles south of Sahale Mountain. Boston Glacier, the largest glacier of the North Cascades,[4] covers the entire region north of Ripsaw Ridge. South of Ripsaw Ridge the terrain slopes down into the vast Horseshoe Basin, from which some the headwater tributaries of the Stehekin River flow. Long high ridges extend from Buckner Mountain east to Park Creek Pass, and south to Booker Mountain and Park Creek Ridge. Other glaciers near Buckner Mountain include Thunder Glacier, to the north, and Buckner Glacier, to the south.[7]

Buckner Mountain marks the boundary between the Skagit River watershed, to the west, and the Columbia River watershed, to the east, via the Columbia's tributaries: Chelan River, Chelan Lake and Stehekin River.

Buckner Mountain is named for Henry Freeland Buckner, who in the early 20th century managed a mining company which had claims in Horseshoe Basin, southwest of the peak.[4]


Climate


Buckner from southwest
Buckner from southwest

Buckner Mountain is located in the marine west coast climate zone of western North America.[8] Most weather fronts originate in the Pacific Ocean, and travel northeast 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 snowfall onto the Cascades (Orographic lift). 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.[8] Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.[8]


Geology


The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks and ridges, deep glacial valleys, and granite spires. 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.[9] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted.[9] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.[9]

North face of Buckner from the Boston Glacier
North face of Buckner from the Boston Glacier

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.[9] The "U"-shaped cross section of the river valleys are 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.


Recreation


Buckner Mountain is one of the more accessible high peaks of Washington, being located just east of Cascade Pass and a well-maintained trail. Boston Glacier, on the mountains northern face, has become one of the best known ice climbs in the North Cascades.[1]


See also



References


  1. "Mount Buckner, Washington". Peakbagger.com. Retrieved 2009-06-06.
  2. "Buckner Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior.
  3. Howbert, Jeff. "Washington 100 Highest Peaks". The Northwest Peakbaggers Asylum.
  4. "Buckner Mountain". Peakware.com. Archived from the original on 2010-02-07. Retrieved 2009-06-06.
  5. "Mount Buckner-Northeast Peak, Washington". Peakbagger.com. Retrieved 2009-06-06.
  6. Howbert, Jeff. "All Washington Peaks with 2000 Feet of Prominence". The Northwest Peakbaggers Asylum.
  7. USGS topographic maps accessed from USGS GNIS website
  8. Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  9. Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.



На других языках


[de] Buckner Mountain

Der Buckner Mountain (gelegentlich Mount Buckner genannt) ist ein hoher Berg in den North Cascades im US-Bundesstaat Washington. Er liegt in der Stephen Mather Wilderness des North Cascades National Park. Mit 9.114 ft (2.778 m) Höhe ist er der höchste Punkt im Skagit County und einer der zehn höchsten nicht-vulkanischen Gipfel in Washington.[1] Er ist der vierzehnthöchste Gipfel im Bundesstaat[2] und der dritthöchste im North Cascades National Park.[3]
- [en] Buckner Mountain

[fr] Buckner Mountain

Buckner Mountain (parfois mont Buckner) est une montagne située sur le territoire des comtés de Chelan et de Skagit au nord de l'État de Washington aux États-Unis. Culminant à 2 777 mètres d'altitude, la montagne qui appartient à la partie nord de la chaîne des Cascades est une des plus hautes montagnes au sein du parc national des North Cascades. La montagne tire son nom d’Henry Freeland Buckner, un propriétaire d’une exploitation minière de la région[2].

[it] Monte Buckner

Il monte Buckner (in inglese Buckner Mountain o Mount Buckner) è una vetta compresa nella catena delle Cascate, localizzata nello stato del Washington e altresì nella riserva integrale di Stephen Mather, nel parco nazionale delle North Cascades. Con i suoi 2778 m s.l.m., è la maggiore cima della contea di Skagit e una delle circa dieci vette non vulcaniche di Washington oltre i 2743 m (9000 piedi) di altezza.[1] È classificata come la 14ª cima più alta dello stato e la terza del parco nazionale delle North Cascades.[2][3]



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