F River Wye

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  • Geological Structures and Processes
    • High flow rates may cause v-shaped valleys and waterfalls due to erosion.
    • Impermeable shales and gristones.
    • Leves, Steep valley's, waterfalls and meanders. Weathering and mass movement is frequent.
    • Flat valley (due to sweeping meanders) in Hereford and a gorge-Wye valley between Chepstow and Goodrich
    • Leeves and floodplains are common in the river's low and middle course. Waterfall in Cleddon Fells.


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