Seismodislocations - Geomorphological Anomalies on the Background of Developing Exogenic Relief in the Ulakhan-Chistay Ridge (Chersky Seismic Belt)
The article presents data on glacial and gravitational morphosculptures, dominant in the study area. On the background of dominant landforms, seismogravitational landforms are observed. The main relief elements are rockfall slopes, at the foot of which the colluvial and colluvial-proluvial cones are formed. Glacial morphosculpture, represented by troughes, kars, the basal moraine relief, terminal moraine arches and amphitheaters, is widespread. Some exogenous and seismogenic landforms are shown to have certain convergent characteristics that complicate their discernment. It was found that numerous paleoseismodislocations, distinguished by some authors, are a typical manifestation of glacial morphogenesis (kars and kars moraines) and have no relation to gravitational paleoseismodislocations.