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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 and Indian kindergarten and primary school students. The drawing is often produced by students who are asked by their teacher to draw natural ...
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.
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. Finally, many mountains can be characterized by the type of rock that make up their composition.
Of the 200 most prominent summits of the United States, 84 are located in Alaska, 17 in California, 17 in Nevada, 14 in Washington, 12 in Montana, 11 in Utah, nine in Arizona, seven in Hawaii, six in Colorado, six in Oregon, four in Wyoming, four in Idaho, four in New Mexico, two in North Carolina, and one each in New Hampshire, New York, Tennessee, Texas and Maine.
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:
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.
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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 ...