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Stratigraphic sequence of the Lower Subtatric Succession in the eastern part of the Polish Tatra Mountains includes 15 Triassic, Jurassic and Lower Cretaceous mappable lithostratigraphic units of formation ranks. Some formations include also non-mappable lithostratigraphic units of local significance, of member and bed ranks. This stratigraphic succession is typical of the Lower Subtatric Nappe (=...
Correlation of partial units of the Lower Subtatric Nappe (= Krizna Nappe) across the Biała Woda Valley (SK: Belovodska dolina; l - left slope; r - right slope), Eastern Tatra Mts, here presented, is a revision of that recently (1999) proposed by J. Lefeld. The Holica-Zadnia Kopa unit (r) seems to wedge out westward (l), but possibly reappears still further west as the Suchy Wierch unit. The Czerwona...
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