By K. J. Gregory (auth.), Professor Ken J. Gregory (eds.)
Fluvial Geomorphology of significant Britain stories the improvement of river-made land varieties, including the linked fluvial procedures. there are numerous websites of clinical curiosity and price in the course of the united kingdom. The GCR websites defined during this quantity symbolize the wide variety of fluvial land kinds within the united kingdom, and the money owed supply medical descriptions of the entire fluvial geomorphology websites in Britain chosen for statutory nature conservation as SSSIs.
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Additional resources for Fluvial Geomorphology of Great Britain
The net result may be akin to the passage of largescale sediment waves documented by Church (1983) on the Bella Coola River in British Columbia. Subsequent adjustment to these changes in regime is often evident through phases of aggradation and incision, resulting in staircases of terraces, some of the best examples being those along the Rivers Findhorn and Feshie. The specific impact of the glacial legacy varies according to differences in the regional and local glacial history; thus that for the Caimgorms differs from that for the Southern Uplands (Sissons, 1976).
Cial and Holocene fluvial adju Iment .. ig Dorback Burn Glen Coc composite sile Luibeg Burn AliI Mor/River ai m Alit Coire Gabhail Alit Mor/ River Druie Quoich Water alluvial fa n Alit a' Choire between slope and fluvial systems is frequently characterized by gullies, debris cones, alluvial fans and mountain torrents, where sediment is fed directly into a river system. Actual sediment inputs may be either progressive, through continuous weathering processes, or episodic with major inputs from point sources during high flows.
1 GCR site selection criteria for fluvial geomorphology in Scotland: channel and planform typology. ) Al luvial channels with high slopes Alluvial rivers . c: u " ~ -'" u ... r> r! "' " " ·a "C c 0 E ... , l:l ~ can be subdivided into 'discordant', 'progressive' and 'integrated' systems. Channels associated with abrupt discontinuities in these controls where streams emerge from upland to lowland environments are termed 'discordant' channel systems. At present only one such site, the AlIt Mor on the upper River Nairn, has been studied.