Geomorphological processes
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Geomorphologists typically recognise three primary river ‘stages’: the ‘young’ or ‘upper’, which river flows quickly in a constrained narrow valley the ‘middle aged’ or ‘middle’ river, which flows more slowly and is meandering with a flood plain linking between the extremities of the meanders and the ‘old age’ or ‘lower’ river, which flows slowly across...Explore the subscription options here to get full access to isurv, including downloads.
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