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  2. Ehagay Nakoda - Wikipedia

    en.wikipedia.org/wiki/Ehagay_Nakoda

    Ehagay Nakoda (/ eɪ ˈ h ɑː ɡ eɪ n ə ˈ k oʊ d ə / ay-HAH-gay nə-KOH-də; Stoney Nakoda variants include Ehage Nakoda and Îhage Nakoda IPA: [e'hage, ĩ'hage na'koda] [a]) is a multipeaked massif located immediately south of the town of Canmore just east of the Spray Lakes road in Alberta's Canadian Rockies.

  3. Mountain formation - Wikipedia

    en.wikipedia.org/wiki/Mountain_formation

    Mountain formation occurs due to a variety of geological processes associated with large-scale movements of the Earth's crust (tectonic plates). [1] Folding , faulting , volcanic activity , igneous intrusion and metamorphism can all be parts of the orogenic process of mountain building. [ 2 ]

  4. Glossary of landforms - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_landforms

    Mamelon – Rock formation created by eruption of relatively thick or stiff lava through a narrow vent; Mid-ocean ridge – Basaltic underwater mountain system formed by plate tectonic spreading; Pit crater – Depression formed by a sinking or collapse of the surface lying above a void or empty chamber

  5. Vadito Group - Wikipedia

    en.wikipedia.org/wiki/Vadito_Group

    The Burnt Mountain Formation probably correlates with the Glenwoody Formation while the Big Rock Conglomerate corresponds to a disconformity in the Picuris Mountains. Detrital zircon dating indicates that the Marquenas Formation , formerly assigned to the Vadito Group, has a maximum age of 1435 Mya and is not part of the Vadito Group.

  6. Mount Kosciuszko - Wikipedia

    en.wikipedia.org/wiki/Mount_Kosciuszko

    The mountain was formed by geologic uplift. [19] It was not formed by any recent volcanic activity. [20] Eroded granite intrusions remain at the summit as large boulders above the more heavily eroded sedimentary rocks. [20] Plant species found in the mountain include: Kosciuszko buttercup (Ranunculus anemoneus) Vickery's grass (Rytidosperma ...

  7. Tunnel Mountain Formation - Wikipedia

    en.wikipedia.org/wiki/Tunnel_Mountain_Formation

    The Tunnel Mountain Formation is present in the front ranges of the Canadian Rockies of western Alberta, and reaches a maximum thickness of about 200 metres (600 ft). It unconformably overlies the Etherington Formation or the Todhunter Formation of the Mississippian Rundle Group, and is conformably overlain by the Late Pennsylvanian Kananaskis Formation.

  8. Magmatism - Wikipedia

    en.wikipedia.org/wiki/Magmatism

    Magmatism is one of the main processes responsible for mountain formation. The nature of magmatism depends on the tectonic setting . [ 1 ] For example, andesitic magmatism is associated with the formation of island arcs at convergent plate boundaries while basaltic magmatism is found at mid-ocean ridges during sea-floor spreading at divergent ...

  9. Wood Mountain Formation - Wikipedia

    en.wikipedia.org/wiki/Wood_Mountain_Formation

    Print/export Download as PDF; Printable version; In other projects Wikidata item; Appearance. ... The Wood Mountain Formation is a geologic formation in Saskatchewan.