Salmon Glacier

Coordinates: 56°07′N 130°04′W / 56.117°N 130.067°W / 56.117; -130.067
Source: Wikipedia, the free encyclopedia.
Salmon Glacier
View of the Salmon Glacier from the viewpoint. Mount Bayard to left, Mount White-Fraser partially visible to right.
TypeValley glacier
LocationBoundary Ranges
British Columbia
Coordinates56°07′N 130°04′W / 56.117°N 130.067°W / 56.117; -130.067[1]

The Salmon Glacier is a

natural hazard. Summit Lake is located at the northern end of the glacier and every year around mid-July the lake breaks an ice-dam and then flows under the Salmon Glacier into the Salmon River. This causes the river to rise approximately 4–5 ft (1.2–1.5 m) for several days.[citation needed
]

The glacier can be accessed by road from Hyder, Alaska, from early July to late September.

The glacier's name was officially adopted January 20, 1955, by the Geographical Names Board of Canada.[1]

Climate

Based on the

marine west coast climate zone of western North America.[2] Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift
), causing them to drop their moisture in the form of rain or snowfall. As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C (−4 °F) with wind chill factors below −30 °C (−22 °F).

Panoramic view of Salmon Glacier

See also

References

  1. ^ a b "Salmon Glacier". Geographical Names Data Base. Natural Resources Canada. Retrieved 2019-12-05.
  2. S2CID 9654551
    .

External links

Further reading