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  2. 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 ]

  3. Ama Dablam - Wikipedia

    en.wikipedia.org/wiki/Ama_Dablam

    1979 North Ridge (VI 5.7 70deg 1600m) by a large French expedition led by Raymond Renaud and Yvan Estienne placed 14 Frenchmen and 4 Nepalese Sherpa in three groups on the summit over three days, 21-23 Oct 1979. [11] 1981 Northeast Spur to North Ridge (VI 5.7 70deg 1500m) by Tim McCartney-Snape, Lincoln Hall, and Andrew Henderson (AUS). [11]

  4. Glossary of landforms - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_landforms

    Massif – The principal mass of a mountain; Meander – One of a series of curves in a channel of a matured stream; Mesa – Elevated area of land with a flat top and sides, usually much wider than buttes; Mid-ocean ridge – Basaltic underwater mountain system formed by plate tectonic spreading

  5. Landform - Wikipedia

    en.wikipedia.org/wiki/Landform

    Examples are mountains, hills, polar caps, and valleys, which are found on all of the terrestrial planets. The scientific study of landforms is known as geomorphology. In onomastic terminology, toponyms (geographical proper names) of individual landform objects (mountains, hills, valleys, etc.) are called oronyms. [4]

  6. Pyramidal peak - Wikipedia

    en.wikipedia.org/wiki/Pyramidal_peak

    When three or more of these cirques converge on a central point, they create a pyramid-shaped peak with steep walls. These horns are a common shape for mountain tops in highly glaciated areas. The number of faces of a horn depends on the number of cirques involved in the formation of the peak: three to four is most common.

  7. Conical hill - Wikipedia

    en.wikipedia.org/wiki/Conical_hill

    These are new openings formed on the sides of the volcano through which new material is ejected sometimes only on one side. As a result, these mountains lose their ideal conical shape. The formation of an almost perfect conical mountain or hill is only possible where there is a stable, central crater.

  8. Bornhardt - Wikipedia

    en.wikipedia.org/wiki/Bornhardt

    [2] [3] While bornhardt was originally used to sometimes denote a type of inselberg (literally island mountain—an isolated dome in an otherwise flat landscape), the term bornhardt is used in modern literature to refer to domed hills and mountains regardless of isolation; thus, not all bornhardts are inselbergs and not all inselbergs are ...

  9. Butte - Wikipedia

    en.wikipedia.org/wiki/Butte

    Three notable formations that are either named butte or may be considered buttes even though they do not conform to the formal geographer's rule are Scotts Bluff in Nebraska which is a collection of five bluffs, Crested Butte, which is a 12,168 ft (3,709 m) mountain in Colorado, and Elephant Butte, which is now an island in Elephant Butte ...