26 GEOLOGICAL JIEMOIES. 



have towered up out of the white marl (Baden) in the form of islands, 

 which must have been covered immediately by the Leithakalk. The 

 bed of white " Mergel" and " Kalk-mergel" extends from Orljava to 

 near Podversko, and from thence to the PozeganKange. Finally, from 

 Podversko towards Rogolje, whence the author started, only the 

 youngest member of the N^eogene-tertiary formation is seen. Near 

 Ober Lipovac, and between Maticevic and Pavlovce, the Leithakalk 

 consists of a bed of white calcareous sand containing nodules of Nulli- 

 pores as large as one's fist, and larger, and of an overlying bed of 

 porous limestone three to four feet thick, consisting of shells of the 

 following species, cemented together : — Cerithium pictum, Bast., 

 C. rubiginosum, Eichw., Mactra Podolica, Eichw., Ervilia Podolica, 

 Eichw., and Cardium Vindohonense, Partsch. 



North-eastern slope of the Pozegan Range, between Pleternica and 

 Pozeg. — In this district only a few patches of the Older Neogene 

 strata remain. The most important locality is a recess of the high- 

 road near Pozeg, close to a small chapel, where the following Bryozoa, 

 determined by Dr. Stoliczka, were found : — 



Crisia Edwardsi, Beuss. Idmonea foraminosa, Reuss. 



Pustulopora anomala, Eeuss. pertusa, Beuss. 



pulchella, Beuss. tenuisulca, Beuss. 



Filisparsa biloba, Beuss. Pavotubigera dimidiata, Beicss. 



Hornera bippolyta, Befr. Defrancia deformis, Beuss. 



Domopora prolifera, Beuss. Lepraria monoceras, Beuss. 



stellata, Goldf. stenostoma, Beuss. 



Ceriopora anomalopora, Goldf. Cellepora globularis, Br own. 



Myriozoum geminiporum, Beuss. Biflustra bipunctata, Beuss. 



Scrupocellaria elliptica, Beuss. Eschara polystomella, Beuss. 



Salicornaria marginata, Goldf. (crassa, macrocheila, Beuss. 



Busk). Reussi, Stol. 



Retepora cellulosa, Lam. cervicornis, Lam. 



Rubeschi, Beuss. undulata, Beuss. 



Membranipora angulata, Beuss. monilifera, Milne-Edw. 



The following Foraminifera from this locality were determined by 

 Herr E. Karrer : — 



Rotulina cultrata, 0. r. B. N. Amphistegina Haueri, 0. c. N. 

 Polystomella crispa, 0. vc. N. B. Heterostegina cristata, 0. N. 

 Rotalina Boueana, 0. c. N. B. Textiilaria, sp. n, similar to T. Icevigata, 

 Dutemplei, 0. c. N. O., but much larger. 



Besides these, there are also found in this formation Argiope decol- 

 lata, Eichw., and A. pusilla, Eichw., Balanus, Terehratula, spines of 

 Echinidce, and claws of Crabs. The " Kalkmergel " is found lying 

 against the side of the mountain between Dervisaga and Yidovci ; and 

 south of Pozeg, near Sevce, isolated thick beds of Older Neogene 

 strata are found upon the tops of the hills, covering superficially the 

 older rocks. 



The Brooder Gebirge. — This mountain is formed entirely of Older 

 Neogene strata. The Leithakalk appears only on the southern slope 

 near Grabarje, the white " Kalkmergel " (Cerithium-horizon) con- 

 stituting the whole of its upper portion, as also the district of Paka 

 and Eussevo, and from thence westward to the Pleternica, and south- 

 w^ard to the^ line of the Odvorze-Zdence. 



