Definition:
Inland valleys are the upper reaches of river systems, in which alluvial sedimentation processes are completely or almost absent. Inland valleys comprise the whole valley cross-section, i.e. valley bottoms, which may be submerged for part of the year, their hydromorphic fringes, and the contiguous upland slopes and crests extending over the area that contributes runoff and seepage to the valley bottom.
Source:
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Food and Agriculture Organization of the United Nations, AQUASTAT Web Site