Bearpaw Mountain

Coordinates: 48°56′46″N 121°51′14″W / 48.9460515°N 121.8540180°W / 48.9460515; -121.8540180
Source: Wikipedia, the free encyclopedia.
Bearpaw Mountain
East aspect, summit right of center
Highest point
Elevation6,091 ft (1,857 m)[1]
Prominence251 ft (77 m)[1]
Parent peakChurch Mountain[2]
Isolation1.80 mi (2.90 km)[2]
Coordinates48°56′46″N 121°51′14″W / 48.9460515°N 121.8540180°W / 48.9460515; -121.8540180[3]
Geography
Bearpaw Mountain is located in Washington (state)
Bearpaw Mountain
Bearpaw Mountain
Location in Washington
Bearpaw Mountain is located in the United States
Bearpaw Mountain
Bearpaw Mountain
Bearpaw Mountain (the United States)
Location
class 3 scramble from southwest[2][4]

Bearpaw Mountain is a 6,091-foot (1,857-metre) mountain

Topographic relief
is significant as the north aspect rises 3,100 feet (945 m) above Canyon Creek in approximately 1.5 mile. Bearpaw Mountain houses Bearpaw Mountain Lake, 650 ft elevated fishing lake.

Climate

Bearpaw Mountain is located in the

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.[4] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.[4] Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below 0 °F (−18 °C) or above 80 °F (27 °C).[4] 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

glacial valleys
. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to various climate differences.

The history of the formation of the Cascade Mountains dates back millions of years ago to the late

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 and shaped the landscape.[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 "Bearpaw Mountain, Washington". Peakbagger.com. Retrieved 2022-02-01.
  2. ^ a b c "Bearpaw Mountain - 6,091' WA". listsofjohn.com. Retrieved 2022-02-01.
  3. ^ a b "Bearpaw Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2022-02-01.
  4. ^ a b c d e f 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.

5. https://www.wta.org/go-hiking/hikes/bearpaw-mountain-lake-757

External links