To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Re-entrant (terrain)

From Wikipedia, the free encyclopedia

Example on a topographical map, and how it would look in the real world.
Typical re-entrant, Little Carpathians

A re-entrant (international) or draw (US) 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. Re-entrants are similar to valleys on a smaller scale; however, while valleys are by nature parallel to a ridgeline, a re-entrant is perpendicular to the ridge, and rises with the surrounding ground, disappearing up-slope. It is usually etched in a hillside by water flow, is usually dry, but many contain an ephemeral stream or loose rocks from eroded rockfall.

In a re-entrant or draw the ground always slopes downward in only one direction, and upward in the other three.[1][2] 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.

YouTube Encyclopedic

  • 1/1
    Views:
    188 481
  • Contour lines and Contour Interval, Relief Features in a Toposheet | ICSE Geography

Transcription

See also

References

  1. ^ "FM3-25.26 CHPTR 10 ELEVATION AND RELIEF".
  2. ^ "Draw (Minor Terrain Feature)".
This page was last edited on 8 October 2023, at 03:13
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.