Poziom Goniatites crenistria z Glinna (Góry Sowie)
Abstract
HORIZON GONIATITES CRENISTRIA FROM GLINNO (SOWIE GÓRY, SUDETEN MTS.)The Lower carboniferous sediments of the southern part of GIinno·(Friedersdarf) village in Sowie Góry (Eulengebirge) are situated within the Middle Stedeten Mountains (Fig. 1).For the first· time these sediments have been described by E. Dathe and L. Finckh (1923) and, at that time, divided into 2 parts, the lower part consisting of gneiss conglomerates with intercalations of gneiss sandstones, the higher of argillaceous shales and greywacke sandstones with limestone lenticels. As to the latter part, the authors report from Ostrzew hill (Spitzberg) 11 forms of plants; they also mention the occurrence of compressed specimens of gastropods of genus Euomphalus.In 1956, W. Grocholski surveyed anew the region of Glinno (Fig. 2);the major part of the lower strata of the Lower Carboniferous mentioned by the German scientists he identified as periglacial gneiss rubble.Downloads
Issue
Section
Articles
License
Authors who publish with this journal agree to the following terms:- 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.
- 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.
- 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).
