Wójcik, A., Garecka, M., Olszewska, B., Wódka, M., 2015. Fos sil karst in the Ju ras sic of the Kooeciuszko Mound in Kraków (south ern Po land) Geo log i cal Quar terly, 59 (1): 61-70, doi: 10.7306/gq.1204Study of four bore holes (each 100 m deep) drilled in St. Bronis³awa Hill (part of the horst of the Wolski For est, Kraków) in dicates that the Oxfordian lime stone is interbedded by claystones with cal car e ous rub ble (de tri tus) fill ing fos sil karst forms. The claystones, lo cally show ing pla nar strat i fi ca tion, con tain as sem blages of Late Cre ta ceous (Campanian-Maastrichtian) foraminifers. Mid dle Mio cene pla nar lam i nated lime stones have also been found in cav i ties formed in the Mid dle Oxfordian lime stones. Mio cene de pos its of this type, fill ing the fos sil karst, were not pre vi ously known from the area of Kraków. Both the Up per Cre ta ceous and Mid dle Mio cene de pos its doc u ment prob a bly ma rine sed i men ta tion that re sulted in the fill ing of the karst sys tem. This type of karst was prob a bly formed be fore the trans gres sion of the Late Cre ta ceous sea, and be fore the trans gres sion of the Mid dle Miocene sea on the area of the present-day horst of the Wolski For est.

Con di tions of land slide de vel op ment dur ing the last de cade in the Ro¿nów Dam-Lake re gion (South ern Po land) based on Air borne La ser Scan ning (ALS) data anal y sis. Geo log i cal Quar terly, 66: 4,

The relationship between the selected landslide morphology and the geologic setting of the Carpathians and the Carpathian Foredeep based on the digital terrain model. A b s t r a c t. This article presents the results of digital terrain model analysis and field observations related to occurrence of characteristic forms in landslide surface that may indicate the geological setting. Based on these observations, three characteristic structures were selected occurring on many landslides in the Carpathian Mountains and the Carpathian Foredeep. The former are the wrinkle structures visible on the digital terrain model associated with movement along the bedded surface. The other are the streak structures linked to the occurrence of gravels and sands on the clays. The third mogul type structures are related to cylindrical sliding surfaces formed in clay.

Assessment of activities of selected landslides in the Ro¿nowskie Dam Lake region based on field studies and analyses of differential digital models.

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