17-Sep-2008 - W.W.Locke Return to Class Home Page

Maps and Map Interpretation

Any aspect of the environment must be considered in its spatial context:

and a host of other issues - all best resolved through maps.  You know where to find maps - in the University Library, through government and commercial outlets and on-line from the Montana MapFinder, Topozone (now a subscription service), TerraServer, Google Maps, or elsewhere - but how do you use maps?  In teams of two, attempt as many of the following as time permits.  You do not need to perform them in order, although some logically follow others (e.g., "relief" after "elevation")


Location Elevation Relief Distance Direction Contouring

NOTE:  All exercises refer to the Sedan, MT, 1:62,500 (1951) topographic quadrangle.  Please do NOT write on the maps provided!


Location:

Location is determined with reference to one or more of the many grids [nearly rectangular or square coordinate systems] within which maps are defined.


Elevation

Elevations are determined on maps in either English units (feet) or metric units (meters).  They are shown as labeled points (BM = bench mark) rounded to the nearest foot from accurate surveys; as spot elevations (x or nothing), accurate to ± 0.3 contour interval; or as interpolations from contour lines, accurate to ± 0.5 contour interval.  Interpolation is generally to the nearest 1/2 contour interval (here, equal to what? _____).


Relief

Relief is simply the arithmetic difference (highest - lowest) between two points of interest.  The uncertainty is the square root of the sum of the squared individual errors.  Note that slope (rise/run) can be calculated from relief (rise) and distance (run).


Distance

Distance is measured using either the bar scale or the fractional scale.  The bar scales are located at bottom center of the map, and are given in a number of units.  The fractional scale is found above the bar scales, in the form of the ration between a distance on the map and the distance between the same points on the ground.  What is the fractional scale of this map?   ___:_____________


Direction

Direction is measured with a protractor relative to True North or Magnetic North according to the declination diagram in the lower map margin.   "Relative to" means in degrees E or W of North (or South), or as an azimuth (out of 360°, where N is 0°, E is 90°, S is 180°, and W is 270°).Why do you need more than one North, anyway? ____________________________________________________________________________________________________________


Contouring

Contours are lines connecting equal values.  Many data types other than elevation are shown by contoured maps - ground-water levels, geochemical characteristics, and rainfall amounts, to name a few.  How do they do that?  By following a few simple rules (some of which have rare exceptions).

Rule Exception
Contour numbering starts at zero
Contours are equally spaced - the "contour interval" Supplemental (dashed) lines may be inserted for detail
Every fifth line is a master contour (heavy line)
Contours must close on themselves Lines "end" at the edge of a map
Contours never join, split, or cross Lines may merge and diverge at a vertical cliff
Contour numbers repeat across a high or low spot
Between known points the slope is assumed constant
Contours are usually smooth, but "V" up a stream Ridges may "V" downhill as well

NOTE:  For a more in-depth discussion of topographic map interpretation, see the instructions for Geomorphology - ESCI 307.


REFLECTION:  

As a group, discuss what you have learned. Have you heard of these concepts before - if so, in what context? In what contexts do you expect to hear about them
again?  Have you used topographic maps before - when and where?  What have you learned here that might help your future map use?


17-Sep-2008 - W.W.Locke Return to Class Home Page