Hydromorphology
Specific power of a river
Morphology
Spawning run
Meander
Section between two successive turning points. On the outside of the curve (or extrados) the concave river bank is eroded, steep, and conducive to lateral erosion. On the inside of the curve (or intrados) the convex river bank is sloping gently, suitable for sedimentation of alluvial benches. There are two main types of meanders, incised meanders and free meanders, and an intermediate type, forced cut meanders.
Minor bed
Part of the bed between well-marked river banks in which water entirely flows outside periods of very high-flow and overflowing. The minor bed includes the low-water channel. Its limit is the bankfull discharge channel. In the case of a braided bed, there may be several flow channels. The minor bed is home to varied flora and fauna (fish, invertebrates, crayfish, mussels, diatoms, macrophytes, etc) whose population status is closely linked to the heterogeneity of the bed and to connections with the floodplain and
Bankfull discharge bed
Limit beyond which the water spills into the floodplain. It corresponds to the high-flow (or morphogenetic flow). Calculating the width of the bankfull discharge bed is a convenient measurement unit to describe the relationship between the size of the watercourse and its
Low-flow channel
Part of the bed in which there is always water. It corresponds to the low-flow. Also referred to as "summer bed".