Bedal Peak
   HOME

TheInfoList



OR:

Bedal Peak is a mountain
summit A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used only for ...
located in the
North Cascades The North Cascades are a section of the Cascade Range of western North America. They span the border between the Provinces and territories of Canada, Canadian province of British Columbia and the U.S. state of Washington (state), Washington and ...
, in
Snohomish County Snohomish County () is a county located in the U.S. state of Washington. With a population of 827,957 as of the 2020 census, it is the third-most populous county in Washington, after nearby King and Pierce counties, and the 72nd-most popul ...
of
Washington Washington most commonly refers to: * George Washington (1732–1799), the first president of the United States * Washington (state), a state in the Pacific Northwest of the United States * Washington, D.C., the capital of the United States ** A ...
state. The mountain is situated in the Henry M. Jackson Wilderness, on land managed by the
Mount Baker-Snoqualmie National Forest Mount is often used as part of the name of specific mountains, e.g. Mount Everest. Mount or Mounts may also refer to: Places * Mount, Cornwall, a village in Warleggan parish, England * Mount, Perranzabuloe, a hamlet in Perranzabuloe parish, ...
. The nearest higher neighbor is the
line parent A peak's line parent is the closest higher peak on the highest ridge leading away from the peak's "key col". A col is the lowest point on the ridge between two summits and is roughly synonymous with pass, gap, saddle and notch. The highest col ...
Sloan Peak Sloan Peak is a mountain in the North Cascades of Washington state. It rises about east of Everett, Washington and 12 miles southwest of Glacier Peak, one of the Cascade stratovolcanoes. It is located between the north and south forks of Sauk ...
, to the south-southeast. Precipitation runoff from the peak drains west to the South Fork Sauk River via Bedal Creek, as well as north and east into tributaries of the North Fork. The north and south forks merge at the northwest base of the mountain to form the Sauk River.
Topographic relief Terrain (), alternatively relief or topographical relief, is the dimension and shape of a given surface of land. In physical geography, terrain is the lay of the land. This is usually expressed in terms of the elevation, slope, and orientati ...
is significant as the summit rises above the Sauk River Valley and
Mountain Loop Highway The Mountain Loop Highway is a scenic byway in the U.S. state of Washington (U.S. state), Washington. It traverses the western section of the Cascade Range within Snohomish County, Washington, Snohomish County. The name suggests it forms a full ...
in approximately two miles.


History

This geographical feature's toponym has been officially adopted by the U.S. Board on Geographic Names to remember James Bedal (1862–1932), who settled at the base of the peak with his wife Susie in 1892. He worked for the National Forest Service. The
first ascent In mountaineering and climbing, a first ascent (abbreviated to FA in climbing guidebook, guide books), is the first successful documented climb to the top of a mountain or the top of a particular climbing route. Early 20th-century mountaineers a ...
of the summit was made circa 1921 by Harry Bedal who was the son of James. Harry is also credited with the first ascents of Sloan Peak and Three Fingers.


Climate

Bedal Peak is located in the
marine west coast An oceanic climate, also known as a marine climate or maritime climate, is the temperate climate sub-type in Köppen classification represented as ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring co ...
climate zone of western North America. Most
weather front A weather front is a boundary separating air masses for which several characteristics differ, such as air density, wind, temperature, and humidity. Disturbed and unstable weather due to these differences often arises along the boundary. For ins ...
s coming off the Pacific Ocean travel east toward the
Cascade Mountains The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as many of those in the ...
. 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 Orographic lift occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain. As the air mass gains altitude it quickly cools down adiabatically, which can raise the relative humidity to 100% and cr ...
). As a result, the west side of the North Cascades experiences 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 An avalanche is a rapid flow of snow down a Grade (slope), slope, such as a hill or mountain. Avalanches can be triggered spontaneously, by factors such as increased precipitation or snowpack weakening, or by external means such as humans, othe ...
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. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below or above .


Geology

The North Cascades feature some of the most rugged topography in the
Cascade Range The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington (state), Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as m ...
with craggy peaks, spires, ridges, and deep
glacial valley U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight s ...
s. 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 The Eocene ( ) is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (Ma). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes ...
Epoch. With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted.
Glacier Peak Glacier Peak or Dakobed (known in the Sauk-Suiattle dialect of the Lushootseed language as "Tda-ko-buh-ba" or "Takobia") is the most isolated of the five major stratovolcanoes (composite volcanoes) of the Cascade Volcanoes, Cascade Volcanic Arc ...
, a
stratovolcano A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with ...
that is east-northeast of Bedal Peak, began forming in the mid-
Pleistocene The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fin ...
.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. In addition, small fragments of the
oceanic Oceanic may refer to: *Of or relating to the ocean *Of or relating to Oceania **Oceanic climate **Oceanic languages **Oceanic person or people, also called "Pacific Islander(s)" Places * Oceanic, British Columbia, a settlement on Smith Island, ...
and
continental lithosphere A lithosphere () is the rigid, outermost rocky shell of a terrestrial planet or natural satellite. On Earth, it is composed of the crust and the lithospheric mantle, the topmost portion of the upper mantle that behaves elastically on time sc ...
called
terrane In geology, a terrane (; in full, a tectonostratigraphic terrane) is a crust fragment formed on a tectonic plate (or broken off from it) and accreted or " sutured" to crust lying on another plate. The crustal block or fragment preserves its d ...
s created the
North Cascades The North Cascades are a section of the Cascade Range of western North America. They span the border between the Provinces and territories of Canada, Canadian province of British Columbia and the U.S. state of Washington (state), Washington and ...
about 50 million years ago. During the
Pleistocene The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fin ...
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 area.


Gallery

File:Bedal Peak.jpg, Bedal Peak (centered) seen from Mt Dickerman. File:Bedal Peak in clouds.jpg, East aspect of Bedal Peak seen from Painted Mountain File:Glacier Peak and Sloan Peak.jpg, Glacier Peak (left), Bedal Peak (centered), and Sloan Peak (right) seen from the summit of Mt Dickerman. File:Sloan Peak to Mount Pugh.jpeg, View from summit of Sloan Peak with Bedal Peak lower left of center


See also

*
Geography of the North Cascades The geography of the North Cascades describes a range of rugged mountains in British Columbia, Canada and Washington, United States. In Canada, the range is officially named the Cascade Mountains but is commonly referred to as the Canadian Cascad ...


References


External links

* Bedal Peak
Mountain Forecast.com
* Bedal Peak
Mountaineers.org


{{Geographic Location 2 , Center = Bedal Peak , North = Mount Pugh , Northeast = North Fork Sauk River , East = Painted Mountain , Southeast = Sloan Creek , South =
Sloan Peak Sloan Peak is a mountain in the North Cascades of Washington state. It rises about east of Everett, Washington and 12 miles southwest of Glacier Peak, one of the Cascade stratovolcanoes. It is located between the north and south forks of Sauk ...
, Southwest = Sheep Mountain , West =
Mount Dickerman Mount Dickerman, or Dickerman Mountain, is a mountain in Mount Baker-Snoqualmie National Forest in Washington state. It is located northwest of Barlow Pass along the Mountain Loop Highway. A strenuous four mile trail leads from this highway t ...
, Northwest = Mount Forgotten Mountains of Snohomish County, Washington North Cascades of Washington (state) Mount Baker-Snoqualmie National Forest One-thousanders of the United States