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  2. Mountain formation - Wikipedia

    en.wikipedia.org/wiki/Mountain_formation

    Fault-block mountain of the tilted type. [16] Sierra Nevada Mountains (formed by delamination) as seen from the International Space Station. When a fault block is raised or tilted, a block mountain can result. [17] Higher blocks are called horsts, and troughs are called grabens. A spreading apart of the surface causes tensional forces.

  3. Topographic prominence - Wikipedia

    en.wikipedia.org/wiki/Topographic_prominence

    For example, the world's second-highest mountain is K2 (height 8,611 m, prominence 4,017 m). While Mount Everest's South Summit (height 8,749 m, prominence 11 m [2]) is taller than K2, it is not considered an independent mountain because it is a sub-summit of the main summit (which has a height and prominence of 8,848 m).

  4. Raised-relief map - Wikipedia

    en.wikipedia.org/wiki/Raised-relief_map

    A raised-relief map, terrain model or embossed map is a three-dimensional representation, usually of terrain, materialized as a physical artifact. When representing terrain, the vertical dimension is usually exaggerated by a factor between five and ten; this facilitates the visual recognition of terrain features.

  5. List of mountain types - Wikipedia

    en.wikipedia.org/wiki/List_of_mountain_types

    Mountains and hills can be characterized in several ways. Some mountains are volcanoes and can be characterized by the type of lava and eruptive history. Other mountains are shaped by glacial processes and can be characterized by their shape.

  6. Yoshizawa–Randlett system - Wikipedia

    en.wikipedia.org/wiki/Yoshizawa–Randlett_system

    The preliminary fold consists of two perpendicular diagonal mountain folds that bisect the corners of the square and two perpendicular valley folds that bisect the edges of the square. The paper is then collapsed to form a square shape with four isosceles-right triangular flaps. It is sometimes called the Square Base

  7. Nappe - Wikipedia

    en.wikipedia.org/wiki/Nappe

    Klippe of Hronic nappe, Mt. Vápeč, Strážovské vrchy Mts., Slovakia. Nappe can be qualified in a number of ways to indicate various features of a formation. The frontal part in the direction of movement, is called the leading edge of a nappe; numerous folds and secondary thrusts and duplexes are common features here and are sometimes called digitations.

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  9. List of rock formations that resemble human beings - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_formations...

    The Sleeping Warrior — the profile of Arran, [2] here seen from Bute. The Old Man of Hoy in Orkney is a rock pillar that from certain angles is said to resemble a standing man.