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Geologic thrust fault of the Rocky Mountains
The Lewis Overthrust is a geologic thrust fault structure of the Rocky Mountains found within the bordering national parks of Glacier in Montana, United
Lewis_Overthrust
Mountain range in Montana, United States and Alberta, Canada
extreme southern Alberta, Canada. It was formed as a result of the Lewis Overthrust, a geologic thrust fault involving the overlying of younger Cretaceous
Lewis_Range
National park in Montana, United States
forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest
Glacier_National_Park_(U.S.)
Mountain range in Canada
Canadian Rockies extends into the U.S. state of Montana including Lewis Overthrust and various sites such as the Wilson Range, Upper Waterton Lake, Boundary
Canadian_Rockies
Mountain in Montana, United States
the Rocky Mountain Front, a 200-mile-long (320 km) overthrust fault, known as the Lewis Overthrust, which extends from central Montana into southern Alberta
Chief_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Norris_Mountain
Mountain range in Canada and United States
Livingston Range was uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Livingston_Range
Mountain in Alberta, Canada
younger rock during the Laramide orogeny. Jerram was created during the Lewis Overthrust. The steeply tilted strata are virtually the same in each peak of the
Mount_Jerram
Mountain in Montana, United States
the Atlantic's Gulf of Mexico near New Orleans. The Lewis Range was formed in the Lewis Overthrust, some 59–75 million years ago, when an enormous slab
Triple_Divide_Peak_(Montana)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Little_Matterhorn_(Montana)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Going-to-the-Sun_Mountain
Mountain ridge in Montana, United States
and over the top of younger rock during the Laramide orogeny. The Lewis Overthrust extends over 280 miles (450 km) from Mount Kidd in Alberta, south to
Sawtooth_Ridge
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Angel Wing (Glacier National Park)
Angel_Wing_(Glacier_National_Park)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Heavy_Runner_Mountain
North American region east of the range
south to about Helena is heavily deformed by faulting, folding, and overthrusting. During the Sevier orogeny mountain-building event about 115 and 55
Rocky_Mountain_Front
Mountain in Glacier National Park, Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Clements_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Cleveland_(Montana)
National park in Alberta, Canada
the Waterton sediments are characterized by a single overlap. The Lewis Overthrust allowed sediment Proterozoic to move as a unit, more or less, horizontally
Waterton_Lakes_National_Park
Mountain in Montana, US
and over the top of younger rock during the Laramide orogeny. The Lewis Overthrust extends over 280 miles (450 km) from Mount Kidd in Alberta, south to
Choteau_Mountain
Mountain in Alberta, Canada
and over the top of younger rock during the Laramide orogeny. The Lewis Overthrust extends over 450 km (280 mi) from Mount Kidd south to Steamboat Mountain
Mount_Kidd
Stratigraphic Group in Alberta, Canada
is a stratigraphic unit of Cenomanian to early Campanian age in the Lewis overthrust in the Western Canadian Sedimentary Basin. It takes its name from the
Alberta_Group
Double summit mountain in Montana
and over the top of younger rock during the Laramide orogeny. The Lewis Overthrust extends over 280 miles (450 km) from Mount Kidd in Alberta, south to
Old_Baldy_(Montana)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Sinopah_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Fusillade_Mountain
Ridge in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Dragons_Tail_(Montana)
1969 Guadeloupe (M7.2), 1974 Antigua (7.5), 2007 Martinique (M7.4) Lewis Overthrust Montana, United States Thrust Late Cretaceous to Early Paleocene Liquiñe-Ofqui
List_of_fault_zones
Mountain summit in Glacier National Park
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Crypt_Peak
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Kinnerly_Peak
Mountain summit in the Livingston Range
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Stanton_Mountain
Mountain in Montana, USA
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Iceberg_Peak_(Montana)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Kootenai_Peak
Mountain ridge in Montana, US
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Porcupine_Ridge
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Bearhat_Mountain
Road Logan Pass Marias Pass Geologic formations Appekunny Formation Lewis Overthrust Belt Supergroup Bighorn sheep Canadian lynx Grizzly bear Elk Gray wolf
Outline of Glacier National Park (U.S.)
Outline_of_Glacier_National_Park_(U.S.)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Jackson_(Montana)
Assembly of magmatic and sedimentary rocks that date to the Mesoproterozoic
This apparent violation of the law of superposition was caused by the Lewis Overthrust. The Belt Supergroup rocks host a variety of economically significant
Belt_Supergroup
Mountain in Alberta, Canada
"Patterson's Peak" in his honor. Mount Head was created during the Lewis Overthrust. The peak is underlain by folded and thrust-faulted sedimentary rock
Mount_Head_(Alberta)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Bear Mountain (Glacier County, Montana)
Bear_Mountain_(Glacier_County,_Montana)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Cannon
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Saint_Nicholas
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Red Mountain (Glacier County, Montana)
Red_Mountain_(Glacier_County,_Montana)
Mountain in Montana, United States
east and over the top of younger rock during the Sevier orogeny. The Lewis Overthrust extends over 280 miles (450 km) from Mount Kidd in Alberta, south to
Mount_Frazier_(Montana)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Rising_Wolf_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Gardner_Point
Mountain pass in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Bishops_Cap
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Doody
Mountain in Montana, United States
and over the top of younger rock during the Laramide orogeny. The Lewis Overthrust extends over 280 miles (450 km) from Mount Kidd in Alberta, south to
Old_Man_of_the_Hills
Mountain in the state of Montana
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Calf_Robe_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Wahcheechee_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Wilbur_(Montana)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_James
Mountain in the country of Canada
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of rocks three miles (4.8 km) thick,
Seven_Sisters_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Sentinel_Mountain_(Montana)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Gable_Peaks
Mountain in the Canadian Rockies
during the Laramide orogeny. Mount Packenham was created during the Lewis Overthrust. The steeply tilted strata are virtually the same in each peak of the
Mount_Packenham
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
The_Guardhouse
Mountain in the American state of Montana
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Elk Mountain (Flathead County, Montana)
Elk_Mountain_(Flathead_County,_Montana)
Peak on the Continental Divide in Glacier National Park, Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Gould_(Montana)
Mountain in Glacier National Park, US
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Olson_Mountain
Mountain in Montana, U.S.
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Little_Chief_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Heavens_Peak
Mountain in Alberta, Canada
rock during the Laramide orogeny. Gap Mountain was created during the Lewis Overthrust. The steeply tilted strata are virtually the same in each peak of the
Gap_Mountain_(Alberta)
Mountain in Alberta, Canada
during the Laramide orogeny. Tombstone Mountain was created during the Lewis Overthrust. The steeply tilted strata are virtually the same in each peak of the
Tombstone_Mountain
Mountain in Glacier Park
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Gunsight_Mountain_(Montana)
Mountain in the state of Montana
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Citadel_Peaks
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Siyeh
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Caper_Peak
Mountain in the state of Montana
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Red_Crow_Mountain
Mountain in the country of Canada
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks three miles (4.8 km)
Mount_Tecumseh_(Alberta)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Pentagon_Mountain
Mountain in the state of Montana
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Reynolds_Mountain
Mountain in the state of Montana
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Goat Mountain (Glacier County, Montana)
Goat_Mountain_(Glacier_County,_Montana)
Mountain on border of Alberta and British Columbia in Canada
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Phillipps_Peak
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Cataract_Mountain
Mountain in Alberta, Canada
"Patterson's Peak" in his honor. Holy Cross Mountain was created during the Lewis Overthrust. The peak is underlain by folded and thrust-faulted sedimentary rock
Holy_Cross_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Argosy_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Capitol_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Lone_Walker_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Piegan_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Cloudcroft_Peaks
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Haystack_Butte
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Custer
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Boulder_Peak
Mountain in Glacier County, Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Dusty_Star_Mountain
through Three Forks, Whitehall the Highland Mountains, and Armstead. The Lewis Overthrust is a geologic thrust fault structure of the Rocky Mountains found within
Geology_of_Montana
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mahtotopa_Mountain
Mountain in Montana, United States
and over the top of younger rock during the Laramide orogeny. The Lewis Overthrust extends over 280 miles (450 km) from Mount Kidd in Alberta, south to
Castle_Reef
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Clyde_Peak
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Phillips_(Montana)
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Kipp
Mountain in Alberta, Canada
during the Laramide orogeny. Mount Evan-Thomas was created during the Lewis Overthrust. The steeply tilted strata are virtually the same in each peak of the
Mount_Evan-Thomas
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Swiftcurrent_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Ipasha_Peak
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Mount_Helen_(Montana)
Mountain summit in Montana, USA
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Spot_Mountain
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Battlement_Mountain
Mountain in the state of Montana
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Scenic_Point
Pillar in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
B-7_Pillar
Representatives Lewis, Meriwether Lewis and Clark Caverns Lewis and Clark Expedition Lewis and Clark National Forest Lewis Overthrust Lewisia rediviva
Index of Montana-related articles
Index_of_Montana-related_articles
Mountain in Montana, United States
rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick
Union_Mountain
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