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  2. Twin mountain drawing - Wikipedia

    en.wikipedia.org/wiki/Twin_mountain_drawing

    A drawing of twin mountains (Indonesian: pemandangan gunung kembar, "twin mountain view", or pemandangan gunung legendaris, "legendary mountain view") is a drawing pattern commonly made by Indonesian kindergarten and primary school students. The drawing is often produced by students who are asked by their teacher to draw natural features.

  3. Category:Doodling motifs - Wikipedia

    en.wikipedia.org/wiki/Category:Doodling_motifs

    Print/export Download as PDF; ... Twin mountain drawing ... This page was last edited on 18 October 2022, at 16:26 (UTC). ...

  4. 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).

  5. Shan shui - Wikipedia

    en.wikipedia.org/wiki/Shan_shui

    Most dictionaries and definitions of shan shui assume that the term includes all ancient Chinese paintings with mountain and water images. [3] Contemporary Chinese painters, however, feel that only paintings with mountain and water images that follow specific conventions of form, style and function should be called "shan shui painting".

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  7. Draw (terrain) - Wikipedia

    en.wikipedia.org/wiki/Draw_(terrain)

    A draw, sometimes known as a re-entrant in orienteering, is a terrain feature formed by two parallel ridges or spurs with low ground in between them. The area of low ground itself is the draw, and it is defined by the spurs surrounding it.

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  9. 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.

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