Wiercenie na Domańskim Wierchu w Kotlinie Nowotarskiej koło Czarnego Dunajca

Authors

  • Jadwiga Urbaniak

Abstract

THE BORE-HOLE AT DOMAŃSKI WIERCH, NEAR CZARNY DUNAJEC, PODHALE AREAThe author presents the description of the profile of the bore-hole drilled at Domański Wierch (753 meters above sea level) near Czarny Dunajec in the Podhale area.The aim of the drilling was to obtain a detailed geological profile and samples for an exact determination of the sequence and age of clays and gravels occurring in the depression of Nowy Targ. Besides, it was expected to reach the substratum of the Neogene series.The sediments drilled through are composed of looms, clayey shales, sands, gravels and conglomerates (for the geological profile see Fig. 2 in the polish text). Several horizons with fossil flora and fauna are present in the clayey shales (for the table of fossiliferous horizons see p. 793 in the polish text).The petrographic character of the sediments indicates, that both the Podhale Flysch and the Tatra Mts. contributed the detrital material during the sedimentation of the Neogene series at Domański Wierch.

Downloads

Issue

Vol. 4 No. 3 (1960)

Section

Articles

License

Authors who publish with this journal agree to the following terms:
  1. Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
  2. Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
  3. Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as this can lead to productive exchanges and earlier and more frequent citation of the published work (See The Effect of Open Access).