Knowledge (XXG)

Fusillade Mountain

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zone characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F.
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periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the
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rocks 3 mi (4.8 km) thick, 50 miles (80 km) wide and 160 miles (260 km) long over younger rock of the
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for firing a futile volley at a group of goats on the side of this mountain".
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at the western terminus of the St. Mary Valley and can be seen from the
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Like the mountains in Glacier National Park, Fusillade is composed of
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Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias".
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Mountains and mountain ranges of Glacier National Park (U.S.)
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Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007).
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Index


Elevation
Prominence
Coordinates
48°38′25″N 113°43′21″W / 48.64028°N 113.72250°W / 48.64028; -113.72250
Fusillade Mountain is located in Montana
Fusillade Mountain is located in the United States
Glacier County, Montana
U.S.
Parent range
Lewis Range
Topo map
USGS
Lewis Range
Glacier National Park
U.S. state
Montana
Gunsight Lake
Going-to-the-Sun Road
George Bird Grinnell
W. H. Seward
Henry L. Stimson
sedimentary rock
Precambrian
Jurassic
Lewis Overthrust
precambrian
cretaceous
Köppen climate classification
subarctic climate

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