Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Contour line
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
{{Short description|Curve along which a 3-D surface is at equal elevation}} {{About|lines of equal value in maps and diagrams|more meanings of the word "contour"|Contour (disambiguation)}} [[File:Courbe niveau.svg|thumb|The bottom part of the diagram shows some contour lines with a straight line running through the location of the maximum value. The curve at the top represents the values along that straight line.]] [[Image:Contour3D.jpg|thumb|upright=1.3|A three-dimensional surface, whose contour graph is below.]] [[Image:Contour2D.svg|thumb|upright=1.3|A two-dimensional contour graph of the three-dimensional surface in the above picture.]] A '''contour line''' (also '''isoline''', '''isopleth''', [[isoquant]] or '''isarithm''') of a [[Function of several real variables|function of two variables]] is a [[curve]] along which the function has a constant value, so that the curve joins points of equal value.<ref>Courant, Richard, Herbert Robbins, and Ian Stewart. ''What Is Mathematics?: An Elementary Approach to Ideas and Methods''. New York: Oxford University Press, 1996. [https://books.google.com/books?id=_kYBqLc5QoQC&pg=PA344 p. 344.]</ref><ref name="Hughes">{{cite book|last1=Hughes-Hallett|first1=Deborah|last2=McCallum|first2=William G.|last3=Gleason|first3=Andrew M.|title=Calculus : Single and Multivariable|date=2013|publisher=John wiley|isbn=978-0470-88861-2|edition=6}}</ref> It is a [[cross-section (geometry)#Definition|plane section]] of the [[graph of a function of two variables|three-dimensional graph]] of the function <math>f(x,y)</math> parallel to the <math>(x,y)</math>-plane. More generally, a contour line for a function of two variables is a curve connecting points where the function has the same particular value.<ref name="Hughes"/> In [[cartography]], a contour line (often just called a "contour") joins points of equal [[elevation]] (height) above a given level, such as [[mean sea level]].<ref>{{Cite web |title=Definition of contour line |url=https://www.dictionary.com/browse/contour-line |access-date=2022-04-04 |website=Dictionary.com |language=en}}</ref> A '''contour map''' is a [[map]] illustrated with contour lines, for example a [[topographic map]], which thus shows valleys and hills, and the steepness or gentleness of slopes.<ref>{{Cite web |title=Definition of CONTOUR MAP |url=https://www.merriam-webster.com/dictionary/contour+map |access-date=2022-04-04 |website=Merriam-Webster |language=en}}</ref> The '''contour interval''' of a contour map is the difference in elevation between successive contour lines.<ref>Tracy, John C. ''Plane Surveying; A Text-Book and Pocket Manual''. New York: J. Wiley & Sons, 1907. [https://books.google.com/books?id=lp0NAAAAYAAJ&pg=PA337 p. 337.]</ref> The [[gradient]] of the function is always perpendicular to the contour lines. When the lines are close together the magnitude of the gradient is large: the variation is steep. A [[level set]] is a generalization of a contour line for functions of any number of variables. Contour lines are curved, straight or a mixture of both lines on a [[map]] describing the intersection of a real or hypothetical surface with one or more horizontal planes. The configuration of these contours allows map readers to infer the relative gradient of a parameter and estimate that parameter at specific places. Contour lines may be either traced on a visible three-dimensional model of the [[surface (mathematics)|surface]], as when a photogrammetrist viewing a stereo-model plots elevation contours, or interpolated from the estimated surface [[elevations]], as when a computer program threads contours through a network of observation points of area centroids. In the latter case, the method of [[interpolation]] affects the reliability of individual isolines and their portrayal of [[slope]], pits and peaks.<ref>Davis, John C., 1986, ''Statistics and data analysis in geology'', Wiley {{ISBN|0-471-08079-9}}</ref>
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)