Jump to content

Relief ratio

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by BattyBot (talk | contribs) at 04:39, 18 July 2016 (fixed citation template(s) to remove page from Category:CS1 maint: Extra text & general fixes using AWB). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

The relief ratio is a number calculated to describe the grade of a river or stream.

The calculation is just the difference in elevation between the river's source and the river's confluence or mouth divided by the total length of the river or stream. This gives the average drop in elevation per unit length of river.[1]

See also

References

  1. ^ Shaw, Lewis C. Pennsylvania Gazetteer of Streams Part II (Water Resources Bulletin No. 16). Prepared in Cooperation with the United States Department of the Interior Geological Survey (1st ed.). Harrisburg, PA: Commonwealth of Pennsylvania, Department of Environmental Resources (no ISBN).