Английская Википедия:Calf Robe Mountain

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Шаблон:Short description Шаблон:Infobox mountain

Calf Robe Mountain is a Шаблон:Convert mountain summit located in Glacier National Park in the U.S. state of Montana.[1] It is situated on the Continental Divide in the Lewis Range, and can be seen from Highway 2 midway between Marias Pass and East Glacier Park. The summit is set on the border shared by Flathead County and Glacier County. Topographic relief is significant as the east aspect rises Шаблон:Convert in one mile. The immediate area between the mountain and highway is known for its aspen and beaver dams.[2]

Etymology

The mountain's name, which commemorates Calf Robe, member of the Blackfeet, was submitted by the National Park Service in 1939, and officially adopted in 1940 by the United States Board on Geographic Names.[1] Legend has it that Calf Robe supposedly had a weird experience with a grizzly bear about 1870. Calf Robe was deserted by his fellow warriors in enemy country and left to die; but he was soon rescued by a grizzly bear, which brought him food and carried him to help.[3] The grizzly only asked a favor in return: that Calf Robe would never kill a bear in winter, which is why the Piikani will never kill a hibernating bear.[4] The Blackfeet name for Calf Robe is "Onistai'yi".[5]

Файл:Calf Robe Mountain, north aspect.jpg
North aspect, from Firebrand Pass Trail, with the pass to right.

Geology

Like other mountains in Glacier National Park, Calf Robe Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks Шаблон:Convert thick, Шаблон:Convert wide and Шаблон:Convert long over younger rock of the cretaceous period.[6]

Файл:Mountain Glacier National Park 2 (8047654291).jpg
Calf Robe Glacier, east aspect

Climate

According to the Köppen climate classification system, Calf Robe Mountain is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers.[7] Winter temperatures can drop below −10 °F with wind chill factors below −30 °F. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer. Precipitation runoff from the east side of the mountain drains into tributaries of the Two Medicine River, and the west side drains to Ole Creek, which is a tributary of Middle Fork Flathead River.

See also

Файл:Summit Mountain, Calf Robe Mountain.jpg
Calf Robe Mountain seen with parent Summit Mountain (left)

References

Шаблон:Reflist

Файл:Calf Robe Mountain, aerial.jpg
Aerial view of Calf Robe Mountain, looking northwest

External links

  1. 1,0 1,1 Ошибка цитирования Неверный тег <ref>; для сносок gnis не указан текст
  2. Jane Gildart, 2012, Glacier Icons, Globe Pequot, Шаблон:ISBN, page 6.
  3. Donald H. Robinson, Through the Years in Glacier National Park, An Administrative History, 1960, Appendix A
  4. Brian O. K. Reeves, Sandra Leslie Peacock, Our Mountains are Our Pillows: An Ethnographic Overview of Glacier National Park, 2001, page 174.
  5. James Willard Schultz, 1926, Signposts of Adventure:Glacier National Park as the Indians Know it, page175.
  6. Шаблон:Cite journal
  7. Шаблон:Cite journal