The stability and safety of the rock slopes of a high-head hydraulic facility assume major significance during both construction and operation of the structures; this also fully applies to the Sayano-Shushenkoe hydroelectric plant, which is constructed in a mountain gorge-canyon of the Yenisei Pdver Valley with steep banks rising 600 m above the shoreline. The construction region is referred to as a zone of seven-point seismicity. The section where the powerhouse is located is composed of durable crystalline hornstone shales of the Dzhebashsk series of the Proterozoic Era: parashales on the right bank and in a large part of the channel, and orthoshales on the left bank and partially in the channel.The left-bank slope of the valley is steep, vertical in places, and crosscut by steeply dipping passes. There are no terraces in this section of the left-bank slope. The original slope within the limits of elevations 340-410 m is completely exposed and forms a steep (65-90 ~ erosion bench with a height of 100 m and more. Above this bench, the slope assumes a steepness of 50-60 ~ with a stepwise form, where individual benches range from 3-10 m high. At elevations 500-570 m, the slope reduces to 25-35 ~ Significant development of edge-resistance and unloading cracks, which also govern primarily the potentially unstable state of individual blocks and large block masses, was realized within the limits of the erosion bench and the median section of the slope [1, 2]. The right-bank slope is less steep (30-55~ and is terraced.Potentially unstable masses (PUM) and talus with a total volume of 14,000 m 3 on the left-and right-bank slopes, which was found to be on the low side, were isolated in the development stage of the detailed design for the Sayano-Shushenskoe hydroelectric plant (1969). Within several years thereafter, a detailed study was conducted on the left-bank slope alone, since the construction of a transformer workshop, assembly site for the powerhouse, employee and production housing with a central control desk, and production housing for auxiliary services was planned beneath this slope. These studies indicated that only the three most characteristic potentially unstable masses -IV, VII, and VIII, which have a stability-reserve factor close to unity -on the left bank slope significantly exceed the total volume assumed in the detailed design for all unstable masses. Their volume is 81,500 m 3 (Fig. 1).To ensure the safety of construction operations on the left bank, other avalanche-prone blocks (II, III, V, and VI) were collapsed artificially. During the period of construction and operation, several spontaneous collapses of rock blocks occurred, the last of which with a volume of 450 m 3 was recorded in 1992 and only by good fortune, did not injure anyone working in the trench of the protective rock wall. The 50-m-high slab-like block that collapsed exposed uniform smooth planes roughened in sections along the cracks that had bounded the block in question. In the opinion of specialists at the Lengidroproekt [3], th...