Landform Interpretation

Objectives of Lecture

  1. Map Reading: making sense of contours
  2. Map Analysis: measuring slope gradient
  3. Map Interpretation: shapes and textures of geomorphic processes


Making Sense of Contours

Contour Interval

vertical spacing between contour lines

Index contour

provides (more frequent) reference to numerical value, every 5 or 10 contour levels...

Default rule

nested contours are "up" (at next contour interval)

EXCEPTION: "depression contours" (hash marks on down side)

Notches

contours bend inwards where a stream or valley cuts into a hill


Slope (see readings on page 352-355)

Terminology:

Muehrcke uses "slope" for the rate of rise or fall along a line; gradient for the steepest slope at a given point. Uses slope orientation for direction of slope.

More common usage (in GIS):

Slope is a composite of gradient and aspect (orientation of steepest slope), measured by the orientation of a plane tangent with the surface.

Aspect: often a key factor in vegetation in mountain environments (deserts too)

Estimating slope on a contour map

Other topographic analysis

Trace ridges, delineate watersheds (nested as streams merge)


Interpreting Landforms from Contours

The Easy Stuff (often infrequent)

Depressions are rare:

The Regular Clues

Some favorites


Version of 24 January 2000