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  2. Geology of the Rocky Mountains - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Rocky_Mountains

    The geology of the Rocky Mountains is that of a discontinuous series of mountain ranges with distinct geological origins. Collectively these make up the Rocky Mountains , a mountain system that stretches from Northern British Columbia through central New Mexico and which is part of the great mountain system known as the North American Cordillera .

  3. Lewis Overthrust - Wikipedia

    en.wikipedia.org/wiki/Lewis_Overthrust

    The Canadian Rocky Mountain foreland thrust and fold belt is a northeastward tapering deformational belt consisting of Mesoproterozoic, Paleozoic, and Mesozoic strata. The Lewis thrust sheet is one of the major structures of the foreland thrust and fold belt extending over 280 mi (450 km) from Mount Kidd near Calgary, AB in the Southeast Canadian Cordillera to Steamboat Mountain, located west ...

  4. Rocky Mountains - Wikipedia

    en.wikipedia.org/wiki/Rocky_Mountains

    The Santa Fe Mountains at the southern end of the Rockies as seen from the Sandia Crest in New Mexico The summits of the Teton Range in Wyoming. The name of the mountains is a calque of an Algonquian name, specifically Plains Cree ᐊᓯᓃᐘᒋᐩ asinîwaciy (originally transcribed as-sin-wati), literally "rocky mountain / alp".

  5. Geology of North America - Wikipedia

    en.wikipedia.org/wiki/Geology_of_North_America

    The Rocky Mountains were formed by a series of events, the last of which is the Laramide Orogeny. [35] One of the outstanding features of the Rocky Mountains is the distance of the range from a subducting plate; this has led to the theory that the Laramide Orogeny took place when the Farallon plate subducted at a low angle, causing uplift far ...

  6. Geology of the United States - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_United_States

    Mountain building thrust up the Rocky Mountains to the north and east and tremendous, earth-stretching tension created the Basin and Range Province to the west and south. [ 11 ] Although the Basin and Range and Colorado Plateau may seem to have little in common, their geological stories are intimately intertwined.

  7. Yellowstone Caldera - Wikipedia

    en.wikipedia.org/wiki/Yellowstone_Caldera

    Studies and analysis may indicate that the greater hazard comes from hydrothermal activity which occurs independently of volcanic activity. [ citation needed ] Over 20 large craters have been produced in the past 14,000 years, resulting in such features as Mary Bay, Turbid Lake , and Indian Pond, which was created in an eruption about 1300 BC.

  8. Category:Geology of the Rocky Mountains - Wikipedia

    en.wikipedia.org/wiki/Category:Geology_of_the...

    Pages in category "Geology of the Rocky Mountains" The following 47 pages are in this category, out of 47 total. This list may not reflect recent changes. ...

  9. Geological hazard - Wikipedia

    en.wikipedia.org/wiki/Geological_hazard

    A geologic hazard or geohazard is an adverse geologic condition capable of causing widespread damage or loss of property and life. [1] These hazards are geological and environmental conditions and involve long-term or short-term geological processes.