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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.
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 ]
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 ...
Mount Elbrus [a] is the highest mountain in Russia and Europe.It is a dormant stratovolcano rising 5,642 m (18,510 ft) above sea level, and is the highest volcano in the supercontinent of Eurasia, as well as the tenth-most prominent peak in the world. [7]
View of Monument Valley in Utah, looking south on U.S. Route 163 from 13 miles (21 km) north of the Utah–Arizona state line Mitchell Mesa from the View Hotel.. Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, pronounced [tsʰépìːʔ ǹtsɪ̀skɑ̀ìː], meaning "valley of the rocks") is a region of the Colorado Plateau characterized by a cluster of sandstone buttes, with the largest reaching ...
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.
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 ...
The Mist Mountain Formation is part of the Kootenay Group, an eastward-thinning wedge of sediments derived from the erosion of newly uplifted mountains to the west.The sediments were transported eastward by river systems and deposited in a variety of fluvial channel, floodplain, swamp, coastal plain and deltaic environments along the western edge of the Western Interior Seaway.