DOI: 10.5593/SGEM2015/B11/S1.012


S. Bulliqi, F.Isufi , B.Kastrati
Tuesday 4 August 2015 by Libadmin2015

References: 15th International Multidisciplinary Scientific GeoConference SGEM 2015, www.sgem.org, SGEM2015 Conference Proceedings, ISBN 978-619-7105-31-5 / ISSN 1314-2704, June 18-24, 2015, Book1 Vol. 1, 91-96 pp

In the complex of the tectonic escarpment of northeast part of Kosovo, the complex escarpment takes also an important place, which is directly bound with the new and current tectonic renewal always in the increase of half horst structures localizing graben lowlands of this space. Thus, all limitative fragmentation escarpments of the Llap graben pond and the North West part of Fushë e Kosoves/Field of Kosovo, which were covered by the lake deposits and the deluvo-proluvial ones in their lower part, are exhumed from these deposits by the selective erosions creating an escarpment of the fragmentation line in this part. Whereas, during the lower part of the escarpment of the fragmentation line, the activating of its plan leads to the formation of the fragmentation escarpment in its lower part granting it a complex character along with upper part of this escarpment. Between the complex escarpment, modeled by exhumation from the selective erosion onto the different scrappy materials of the fragmentation escarpment, it is differentiated the South West slope of Gollak between the outfall of the Graçanica and Llapi river (the right branches of the river Sitnica).

Keywords: Escarpment, Fragmentation line, Llap Graben, Terrigen rocks, Graçanica, Field Kosovo

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