ИСТИНА

Blocked landslides are widespread in Moscow. The displacement of such landslides connects with Upper Jurassic clays. As a rule, these landslides have huge web depth. This depends on the possibility of huge damage. The last one obstructs stabilizing measures. Landslides have regressive (inside slope) development and durable (tens and hundreds of years) periods of slow deformations (1-30 centimeter per year). Such deformations give place to short periods of activation with displacements of some meters and more. In Moscow activation of such landslides threatens to cultural heritage, site which also a part of UNESCO. Landslide slope on Vorobievy Mountains where are Troicy Zhivonachalnoj temple, Andreevskij monastery, Muchenicy Tatiany temple under MSU is considered in depth.