This is an old revision of this page, as edited by James McStub (talk | contribs) at 01:37, 14 March 2007 (rm spam per WP:EL and WP:SPAM). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
Revision as of 01:37, 14 March 2007 by James McStub (talk | contribs) (rm spam per WP:EL and WP:SPAM)(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff) | This article is an orphan, as no other articles link to it. Please introduce links to this page from related articles; try the Find link tool for suggestions. |
The Bradshaw Model is a geographical model which describes how a river's characteristics vary between the lower course and upper course of a river. It shows that discharge, occupied channel width, channel depth and average load quanity increases downstream. Load particle size, channel bed roughness and gradient are characterisitcs decrease downstream.
External links
 | This article related to topography is a stub. You can help Misplaced Pages by expanding it. |