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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.
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.
A spur in the Tatra Mountains. A spur is a lateral ridge or tongue of land descending from a hill, mountain or main crest of a ridge. [1] [2] It can also be defined as another hill or mountain range which projects in a lateral direction from a main hill or mountain range. [3] Examples of spurs include:
Relief map: Sierra Nevada Mountains, Spain 3D rendering of a DEM used for the topography of Mars The digital elevation model (DEM) is a raster -based digital dataset of the topography ( hypsometry and/or bathymetry ) of all or part of the Earth (or a telluric planet ).
A glaciated valley in the Altai Mountains showing the characteristic U shape. Malyovitsa U-shaped valley, Rila Mountain, Bulgaria U-shaped valley in Leh valley, Ladakh, NW Indian Himalaya. The glacier visible at the head of the valley is the last remnant of the formerly much more extensive glacier which carved it.
Couloir – Steep, narrow mountain gully – a narrow gully with a steep gradient in a mountainous terrain; Dale (landform) – Open valley; Draw (terrain) – Terrain feature formed by two parallel ridges or spurs with low ground in between; Gulch – Deep V-shaped valley formed by erosion; Lavaka – Type of gully, formed via groundwater sapping
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A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in ...
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