Bear Mountain (North Cascades)
{{short description|Mountain in Washington (state), United States}}
{{Infobox mountain
| name = Bear Mountain
| other_name =
| etymology =
| native_name = {{native name|hur|Klahaihu}}{{cite book |last=Beckey |first=Fred W. |authorlink=Fred Beckey |title=Cascade Alpine Guide, Vol. 3, Rainy Pass to Fraser River |edition=3rd |year=2009 |publisher=Mountaineers Books |isbn=978-1-59485-136-0 |pages=126–131}}
| photo = Bear Mountain from Copper Ridge.jpg
| photo_caption = Bear Mountain (right) seen from Copper Ridge with its parent, Mt. Redoubt to left
| map =Washington#USA
| map_image =
| map_alt =
| map_caption =
| map_relief =
| map_size = 250
| mapframe = yes
| mapframe-zoom = 8
| mapframe-caption = Interactive map of Bear Mountain
| location = Whatcom County, Washington, U.S.
| label =
| label_position =right
| elevation =
| elevation_m =
| elevation_ft = 7931
| prominence =
| prominence_m =
| prominence_ft = 1388
| prominence_ref ={{cite peakbagger|1617|Bear Mountain|2018-09-30}}
| isolation =
| isolation_km =
| isolation_mi = 2.36
| isolation_ref =
| parent_peak = Mount Redoubt
| listing =
| translation =
| language =
| pronunciation =
| range = Cascade Range
| coordinates = {{coord|48|55|50|N|121|20|28|W|type:mountain_region:US-WA_scale:100000|format=dms|display=inline,title}}
| coordinates_ref = {{cite gnis|1503240|Bear Mountain|2018-09-30}}
| topo = USGS Mount Redoubt
| type =
| age = 26 to 29 million years
| rock = Skagit gneiss and granodiorite
| volcanic_arc =
| volcanic_belt = Pemberton Volcanic Belt
| volcanic_field =
| volcanic_arc/belt =
| last_eruption =
| first_ascent = 1939 Calder Bressler and William Thompson
| easiest_route = Northwest Ridge Class 3-4
| normal_route =
| access =
| child =
| embedded =
}}
Bear Mountain is a remote {{Convert|7931|ft|m|lk=off|abbr=off|adj=on}} mountain summit in the Skagit Range of the North Cascades of Washington state.{{cite book |last=Beckey |first=Fred W. |authorlink=Fred Beckey |title=Cascade Alpine Guide, Vol. 3, Rainy Pass to Fraser River |edition=3rd |year=2008 |publisher=Mountaineers Books |isbn=978-1-59485-136-0}} Bear Mountain is situated in North Cascades National Park. Its nearest higher peak is Mount Redoubt, {{convert|2.36|mi|km|abbr=on}} to the northeast. Precipitation runoff from Bear Mountain drains into Bear Creek and Indian Creek, both tributaries of the Chilliwack River. Access, either by the Chilliwack River Trail or from British Columbia, Canada, is difficult and takes two to three days.
Routes
- Diamond Life
- East Ridge
- North Buttress Direct
- North Buttress West
- North Face Buttress
- Northwest Buttress
- Northwest Ridge
- South Route
- The Diamond
- Ursa Major
- Ursa Minor
Climate
Bear Mountain is located in the marine west coast climate zone of western North America.{{cite book |last=Beckey |first=Fred W. |authorlink=Fred Beckey |title=Cascade Alpine Guide, Vol. 3, Rainy Pass to Fraser River |edition=3rd |year=2008 |publisher=Mountaineers Books |isbn=978-1-59485-136-0}} 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. 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. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.
Geology
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.
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 and shaped the landscape. 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:Bear Mountain and Mount Redoubt.jpg|Bear Mountain (left) and Redoubt (right)
See also
{{Portal|Mountains}}
References
{{reflist}}
External links
- [https://www.nps.gov/noca/index.htm North Cascades National Park] National Park Service
- [https://listsofjohn.com/peak/48925 Lists of john: Bear Mountain]
- [https://books.google.com/books?id=5S0EVRXtK6YC&pg=PA126 Cascade Alpine Guide: Bear Mountain (Ebook preview)]
- [https://pbase.com/nolock/image/46937739 Aerial photo of North Face: PBase]
{{Geographic Location 2
| Center = Bear Mountain
| North = Nodoubt Peak
| Northeast = Mount Redoubt
| ENE = Mox Peaks
| East = Cave Mountain
| Southeast = Tradition Peak
| South = Taps Mountain
| Southwest = Red Face Mountain
| WSW = Indian Mountain
| West = Copper Mountain
| Northwest =
}}