CONCLUSIONSi. The hydraulic resistances of a !argo unlined canal in noncohesive soils (for conditions of a clarified flow) are determined by the uniqueness of the hydraulic regime during establishment of relative stabilization of all main elements of the flow and channel.2. The use of the kinematic index x, characterizing the rate of change in velocities vertically and being a function of the hydraulic resistances, as a criterion of the mobility of bed forms makes it possible to estimate the state of stability of dune forms on various stretches of a large irrigation canal running in an earth channel.3. An arbitrary assignment of the roughness coefficients n is impermissible when determining hydraulic resistances and longitudinal gradients of a large unlined canal with channelforming elements. The hydraulic gradients providing longitudinal stability of a straight channel can be predicted both by the traditional method (in terms of n) but with consideration of the regular variability of n and on the basis of the established relationship between hydraulic resistances and the channel shape parameter. LITERATURE CITED i. V.S. Altunin, Reclamation Canals in Earth Channels [in Russian], Koios, Moscow (!979). 2. A.D. Al'=shul', Hydraulic Resistances [in Russian], Nedra, Moscow (1982).Hydro developments with earth dams are being constructed and planned in all climatic zones of the world --from the tropics to permafrost regions. The majority of hydro developments that have been constructed and are being planned are located on large rivers, the design discharges of which reach 20,000 and 38,000 m3/sec respectively for the construction and service periods. The design discharges are considerably greater for individual unique hydro developments. Thus, for example, for the Middle Enisei hydro development they are 54,000 and 80,000 m3/sec and for the Turukhan hydroelectric station, 71,000 and 116,000 mS/sec. The highest earth dams are the Nurek (300 m) and Rogun (335 m).The use of earth dams, constructed from local materials, in remote, sparsely populated regions of the country, where the necessary transportation lines are absent and the creation of which extremely prolongs and increases thecost of construction of hydrostations, is prospective.