In the Julian Alps (Mt. Prisojnik, NW Slovenia) and in the Kamnik–Savinja Alps (Mt. Križevnik, N Slovenia), both of which form part of the eastern Southern Alps, several meters of Upper Anisian ...pelagic red nodular, radiolarian-rich limestone (Loibl Formation) were deposited on the drowned platform carbonates of the Contrin Formation. The time of the platform drowning is dated with radiolarians and conodonts to the Illyrian, more precisely to the upper part of the
Paraceratites trinodosus
Ammonoid Zone. The red limestone is overlain by pyroclastics and volcanics (rhyolites) or carbonate (mega)breccia (Uggowitz Formation). The following unit consists of thin-bedded limestone, grainstone and subordinate marl (Buchenstein Formation) deposited during the final filling of the basin from the adjacent prograding carbonate platform (Schlern Formation) in the Ladinian. Map-scale geometry, neptunian dykes, the onset of volcanism, the presence of (mega)breccia and related paleo-escarpments, the lateral variations in thickness and the wedge-shaped geometry of the lithological units provide evidence of syn-sedimentary block faulting and the formation of small-scale, relatively shallow half-grabens within the previously uniform Slovenian Carbonate Platform. This analysis indicates a clear tectonic control over the development of the Middle Triassic stratigraphy. The described extensional event is well correlated and genetically connected with the syn-rift formation of the neighboring Slovenian Basin and other Southern Alpine basins that formed in connection with the opening of the Meliata-Maliac branch of the Neotethys Ocean.
A less known damaging earthquake in southern part of Kamnik-Savinja Alps, Slovenia, in 1840 is described. The main shock was on 27 August 1840 with the epicentre in Tuhinj Valley. The maximum ...intensity was VII EMS-98 in Ljubljana, Slovenia, and in Eisenkappel, Austria. It was felt as far as Venice, Italy, 200 km away. The macroseismic magnitude of the main shock, estimated from the area of intensity VI EMS-98, was 5.0. The effects of the main shock and its aftershocks are described, and an earthquake catalogue for Slovenia in 1840 is provided. Available primary sources (newspaper articles) are presented.
The area of the eastern Kamnik-Savinja Alps was glaciated in the time of the Last Pleistocene Glacial Maximum (LGM). The glacial landforms mentioned by the previous researchers and other landforms in ...the area were examined, gemorphologically mapped, morphographically and morphometrically analysed and a new map of the extent of the LGM was produced. The research revealed several glaciers in the area and that their sizes differed, primarily depending on the slope inclination direction.
Kamniški Mali grad je v pisnih virih prvič omenjen leta 1202,leta 1444 pa se omenja kot že opustel. Sodeč po najstarejšihohranjenih arhitekturnih členih je bil zgrajen v 11. ...stoletju, nipa izključena tudi zgodnjesrednjeveška naselbinska faza predtem. Arheološka izkopavanja so potekala v letih od 1976 do 1995.Obravnavana lončenina izvira iz izkopavanj leta 1992 in preds-tavlja približno desetino vsega gradiva. Z analizo stratigrafskihodnosov in lončenine so potrjene dosedanje domneve, da so bileizkopavalcem tam ohranjene le plasti iz druge gradbene fazegradu, umeščene v 13., 14. in začetek 15. stoletja
The in depth archaeological research of High Medieval castle presented in this book is unique in Slovenia and among just few in this part of Central Europe. The book is based on analysis of the ...archaeological data gathered in more than a decade of archaeological excavations in 1980s and 1990s.In the introductory chapter written sources and interpretative models are presented. The analysis of pictorial representations follows. The focus of the research is on the archaeological sources, though. Above all the analysis of the small finds, stratigraphy and spatial analysis of the castle itself and the castle in the landscape should be mentioned.
This case study of the Kamniška Bistrica forest management unit presents a 3D process-based model for determining forests protecting against rockfall. Modelling was performed using the ArcGIS 9.3.1 ...tool; the kinetic energy of rockfalls was calculated using the Conefall friction model. The finished map of protective forests was compared with the map of protective functions of forests, made by the Slovenia Forest Service. The protective function map covers 90% of forests classified in the 1st category forests by the modelled map. Taking into consideration the entire forest area in the forest management unit, the maps match in 48% of cases. The differences appear predominantly in higher altitudes where the protective function map includes dwarf pine sites, and in lower altitudes where the map does not consider the possibility that trees can perform their protective functions where the terrain becomes level. The aim of this article is to draw attention to the possibilities of using the models as tools for determining forests protecting against rockfalls.
Prispevek obravnava lončenino kot vir za kronološko oprede-ljevanje in rekonstrukcijo nekaterih elementov kuhinjske opreme. Gradivo je ovrednoteno kronološko in glede na namembnost. Pri slednjem gre ...za umeščanje posamičnih tipov lončenine v kontekst visokosrednjeveške in poznosrednjeveške kuhinje
Extended description:
"Televizija je prav lepa stvar, lepo pa bi bilo, če bi tudi šola imela televizijo in da bi lahko spremljali oddaje za šolo. To bi bila velika želja učencev in tudi učiteljev."
...Information:
Talk with television viewers: the transmitter on the mountain of Krvavec. Viewers’ statements, regarding television sets and television programmes.
Original language summary:
Pogovor s televizijskimi gledalci; oddajnik Krvavec, izjave gledalcev v Kamniku, Grosuplju, Gorišnici pri Ptuju in Kranju o televizijskih sprejemnikih in programu