Mount Buckindy

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Mount Buckindy
Mount Buckindy.jpg
North aspect, from Hidden Lake Peaks
Highest point
Elevation 7,320 ft (2,231 m) [1]
Prominence 280 ft (85 m) [1]
Parent peak Mount Misch (7,435 ft) [2]
Isolation 0.62 mi (1.00 km) [2]
Coordinates 48°21′05″N121°12′22″W / 48.3515078°N 121.2061383°W / 48.3515078; -121.2061383 [3]
Geography
USA Washington relief location map.jpg
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Mount Buckindy
Location in Washington
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Mount Buckindy
Mount Buckindy (the United States)
Location Skagit County, Washington, U.S.
Parent range Cascade Range
North Cascades
Topo map USGS Downey Mountain
Geology
Type of rock mineralized Breccia pipe
Climbing
First ascent August 28, 1955, by Don Grimlund, Dave Nicholson, Win Trueblood [4]
Easiest route class 4 scrambling [5]

Mount Buckindy is a remote 7,320-foot-elevation (2,230-meter) mountain summit located in the North Cascades, in Skagit County of Washington state. [3] It is the second-highest point of the Buckindy Range, or Buckindy Ridge. It is set in the Glacier Peak Wilderness on land managed by the Mount Baker-Snoqualmie National Forest. It is situated 20 miles east-northeast of Darrington, Washington, and 17 miles north-northwest of Glacier Peak which is one of the Cascade stratovolcanoes. Precipitation runoff from Mount Buckindy drains south to the Suiattle River via Buck Creek and Downey Creek, and north to the Cascade River via Kindy Creek. Topographic relief is significant as the summit rises 4,700 feet (1,400 meters) above Kindy Creek in less than two miles. The mountain's toponym is a portmanteau of Buck and Kindy Creeks, and has been officially adopted by the United States Board on Geographic Names.

Contents

Climate

Mount Buckindy is located in the marine west coast climate zone of western North America. [6] 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. [6] This climate supports the Kindy and Goat Creek Glaciers as well as glacierets on this mountain's slopes. 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. [6]

Geology

The Buckindy Range seen from Eldorado Peak with summit of Mt. Buckindy centered at top Buckindy Range from Eldorado Peak.jpg
The Buckindy Range seen from Eldorado Peak with summit of Mt. Buckindy centered at top

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. [7] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. [7] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago. [7]

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. [7] 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. The rusty reddish color of Mount Buckindy and the Buckindy Range is due to mineralized breccia pipe. [6]

See also

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Gabriel Peak is a prominent 7,920-foot (2,410 m)-elevation mountain summit located in North Cascades National Park, in Skagit County of Washington state. It is part of the North Cascades which is a subset of the Cascade Range. The nearest higher neighbor is Cosho Peak, 2.7 miles (4.3 km) to the south, Beebe Mountain is set 2.5 miles (4.0 km) to the north, and Red Mountain is 3 miles (4.8 km) to the southwest. Precipitation runoff from this feature drains to Ross Lake via Gabriel and Panther Creeks. Like many North Cascade peaks, Gabriel Peak is more notable for its large, steep rise above local terrain than for its absolute elevation. Topographic relief is significant as it rises 4,700 feet (1,400 m) above the Panther Creek valley in approximately one mile. This geographical feature is named after the archangel Gabriel, which is a reference to Tommy Rowland who settled in the Skagit River area in 1895 and later pronounced himself the "Prophet Elisha." Mount Prophet, Genesis Peak, and nearby Elija Ridge were also named in association with Rowland.

<span class="mw-page-title-main">Mount Tommy Thompson</span> Mountain in Washington (state), United States

Mount Tommy Thompson is a 6,780-foot-elevation (2,070-meter) mountain summit located in Skagit County of Washington state. It is situated eight miles southeast of the town of Marblemount, within the Glacier Peak Wilderness, on land managed by Mount Baker–Snoqualmie National Forest, on the west slopes of the North Cascades Range. The nearest higher named neighbor is Snowking Mountain, 3.16 miles (5.09 km) to the southeast. Topographic relief is significant as the southwest aspect rises 3,670 feet above Slide Lake in less than two miles. Precipitation runoff from Mount Tommy Thompson drains into tributaries of the Skagit River.

<span class="mw-page-title-main">Mount Crowder (Washington)</span> Mountain in Washington (state), United States

Mount Crowder is a remote 7,082-foot (2,159-metre) mountain summit in the Picket Range of the North Cascades, in Whatcom County of Washington state. Mount Crowder is situated in North Cascades National Park and Stephen Mather Wilderness. Neighbors include Mount Fury, 1.64 mi (2.64 km) to the northeast, and Twin Needles is set 2.3 mi (3.7 km) to the southeast. Precipitation runoff from this peak drains south into headwaters of Goodell Creek, and northwest into Picket Creek which is a tributary of the Baker River. Topographic relief is significant as the summit rises 4,300 feet above Goodell Creek in approximately one mile.

References

  1. 1 2 "Mount Buckindy, Washington". Peakbagger.com.
  2. 1 2 "Buckindy. Mount - 7,340' WA". listsofjohn.com. Retrieved 2022-04-10.
  3. 1 2 "Mount Buckindy". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2022-04-10.
  4. The Mountaineer (1955), page 58.
  5. Mt. Buckindy, North Side - Mazamas.org
  6. 1 2 3 4 Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  7. 1 2 3 4 Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.