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The article presents the first U-Pb data on the age of the rocks composing scenic erosional outliers located on the Manpupuner Ridge in the Northern Urals. Based on the analysis of the ages of detrital zircons micaceous quartzites exposed on the Manpupuner Ridge are thought to belong to Lower Ordovician Telpos Formation. Sources of clastic material are supposed.

Paleozoic sedimentary basins of the northeast European Platform is a component of large megabasin of the northeast passive continental margin of the European continent in the Paleozoic. The establishment of a connection between a paleodynamic history of a basin and its sedimentary formations types, which are the most reliable indicators of geodynamic conditions, is one of the primary problems of modern lithology. Reliable indicators at geodynamic reconstructions are genetically predetermined by laterial and vertical lines of the sedimentary formations. Formations and lithological complexes being the brightest indicators of the paleodynamic regimes change of the basin have been considered formations lines of the passive continental margin of the westuralian type during the Paleozoic.

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The composition and structure of the Lower Carboniferous part of the Yajyu Suite, common in the eastern subzone of the Lemva structural-formational zones of the Urals is given. It is an indicator of collision processes beginning in the northern part of the Urals and it reflects the geological history of this period. The scaly-thrust structure of the region, small isoclinal folds, numerous discontinuous disturbances and redeposition of organic remains strongly obscured layers succession. The discovery of the lithological marker allowed to decipher the geological structure of one of the tectonic «scales» (plates).