Английская Википедия:Edwards Mountain
Шаблон:Short description Шаблон:Infobox mountain
Edwards Mountain (Шаблон:Convert) is located in the Lewis Range, Glacier National Park in the U.S. state of Montana.[1] Edwards Mountain rises just to the west of Sperry Glacier. Based on the Köppen climate classification, Edwards Mountain has an alpine climate characterized by long, usually very cold winters, and short, cool to mild summers.[2] Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Geology
Like other mountains in Glacier National Park, Edwards 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.[3]
See also
References
Шаблон:FlatheadCountyMT-geo-stub
- Английская Википедия
- Страницы с неработающими файловыми ссылками
- Mountains of Flathead County, Montana
- Mountains of Glacier National Park (U.S.)
- Lewis Range
- Mountains of Montana
- Страницы, где используется шаблон "Навигационная таблица/Телепорт"
- Страницы с телепортом
- Википедия
- Статья из Википедии
- Статья из Английской Википедии
