Lithological features of sedimentary strata of seismic hazard territory in Ulan-Ude city

The features of microseismozoning territory of Ulan-Ude located within Ivolga-Nizhneudinsk intermountain basin. It was noted that the background seismicity area is 7 points, while, depending on geological conditions (lithology, thickness of loose sediments, water cut) seismic intensity varies from 7 to 9 points. We characterize the geological, geomorphological, paleopotamological, mineralogical and lithological characteristics of sediments.