Draw (terrain)
Encyclopedia
A draw a terrain feature formed by two parallel ridge
Ridge
A ridge is a geological feature consisting of a chain of mountains or hills that form a continuous elevated crest for some distance. Ridges are usually termed hills or mountains as well, depending on size. There are several main types of ridges:...

s or spur
Spur (mountain)
A spur is a subsidiary summit of a hill or mountain. By definition, spurs have low topographic prominence, as they are lower than their parent summit and are closely connected to them on the same ridgeline...

s with low ground in between them. The area of low ground itself is the draw, and it is defined by the spurs surrounding it. Draws are similar to valleys on a smaller scale, however while valleys are by nature parallel to a ridgeline, a draw is perpendicular to the ridge, and rises with the surrounding ground, disappearing up-slope. A draw is usually etched in a hillside
Hill
A hill is a landform that extends above the surrounding terrain. Hills often have a distinct summit, although in areas with scarp/dip topography a hill may refer to a particular section of flat terrain without a massive summit A hill is a landform that extends above the surrounding terrain. Hills...

 by water flow, and often contains a stream or loose rocks from eroded rockfall.

A draw differs from a valley or an arroyo, in that the ground always slopes downward from a draw in only one direction, and upward in the other three; while in a valley or arroyo there is only noticeable upward slope in two directions. The slope on a draw is generally quite sharp, with a clearly established fall line and characterized by a generally steep vertical drop over a short horizontal distance.

In snowy climates, draws often form chutes for avalanches, particularly with loose snow hanging from an exposed cornice
Cornice (climbing)
A snow cornice or simply cornice is an overhanging edge of snow on a ridge or the crest of a mountain. They form by wind blowing snow over the crest of the mountain, so they often form on the leeward sides of mountains...

 near the top of the ridgeline.

See also

  • Arroyo (creek)
    Arroyo (creek)
    An arroyo , a Spanish word translated as brook, and also called a wash is usually a dry creek or stream bed—gulch that temporarily or seasonally fills and flows after sufficient rain. Wadi is a similar term in Africa. In Spain, a rambla has a similar meaning to arroyo.-Types and processes:Arroyos...

  • Canyon / Gorge
    Canyon
    A canyon or gorge is a deep ravine between cliffs often carved from the landscape by a river. Rivers have a natural tendency to reach a baseline elevation, which is the same elevation as the body of water it will eventually drain into. This forms a canyon. Most canyons were formed by a process of...

  • Chine
    Chine
    A chine is a steep-sided river valley where the river flows through coastal cliffs to the sea. Typically these are soft eroding cliffs such as sandstone or clays. The word chine originates from the Saxon "Cinan" meaning a gap or yawn....

  • Defile (geography)‎
  • Riparian zone
    Riparian zone
    A riparian zone or riparian area is the interface between land and a river or stream. Riparian is also the proper nomenclature for one of the fifteen terrestrial biomes of the earth. Plant habitats and communities along the river margins and banks are called riparian vegetation, characterized by...

  • Salients, re-entrants and pockets
    Salients, re-entrants and pockets
    A salient is a battlefield feature that projects into enemy territory. The salient is surrounded by the enemy on three sides, making the troops occupying the salient vulnerable. The enemy's line facing a salient is referred to as a re-entrant...

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