1 research outputs found
COMPLEX LANDSLIDE IN THE RJEÄINA RIVER VALLEY
U radu su prikazani rezultati istraživanja prve faze složenog kliziÅ”ta na sjeveroistoÄnoj padini doline RjeÄine izmeÄu brane ValiÄi i naselja PaÅ”ac. Bokovi doline oblikovani su u paleogenskom fliÅ”u i kvartarnim padinskim tvorevinama. Na vrhovima su zastupljene vapnenaÄke stijene tvoreÄi litice. Nastanak istražene kompleksne pojave kliziÅ”ta predodreÄen je geoloÅ”kom gradom i morfogenezom doline RjeÄine. To je složeno retrogresivno kliziÅ”te, koje se poÄelo razvijati od stope prema vrhu kosine. Na padini je otkriveno 13 pojedinaÄnih kliznih tijela. Klizanjem je zahvaÄen materijal padinskih tvorevina i dio kore fiziÄko-kemijskog raspadanja. VeÄi dio kliznog tijela saturiran je podzemnom vodom koja se procjeÄuje kroz pokrivaÄ po kontaktu s nepropusnom fliÅ”nom podlogom. Klizanje je relativno plitko buduÄi da u hidroteh-niÄkom tunelu, koji se nalazi ispod nožice kliziÅ”ta, nisu uoÄena oÅ”teÄenja prouzroÄena klizanjem. Pokrenuti su i megablokovi vapnenaÄke stijene koji, najvjerojatnije, klize po fliÅ”noj podlozi. To je posebna pojava, netipiÄna za kliziÅ”ta na fliÅ”nim padinama u Å”iroj okolici Rijeke. VapnenaÄka stijena na litici je jako dezintegrirana, a u njoj su vidljive svježe pukotine. Istraživanja su se sastojala od geodetskih mjerenja, geofiziÄkih, inženjerskogeoloÅ”kih i geotehniÄkih istraživanja. Geodetsko snimanje obavljeno je metodom terestiÄke fotogrametrije. Rezultati su usporeÄeni s aero-snimcima uÄinjenim godine 1981. Tako su se mogle otkriti promjene morfologije padine u razdoblju od 1981. do 1997. godine. Fotoskice su koriÅ”tene i za dopunu inženjersko-geoloÅ”kog kartiranja. GeofiziÄko mjerenje je obavljeno metodom plitkog seizmiÄko-refrakcijskog profiliranja.This paper presents the first phase investigation results of the complex landslide situated on north-eastern slope of the RjeÄina valley, between ValiÄi damm and the village of PaÅ”ac. The valley slopes were formed in Paleogene flysch and Quaternary formations. The limestone rocks are present on the top sites, forming the scarps there. The complex landslide formation has been preconditioned by the geological structure and morphogenesis of the RjeÄina valley. This is the type of complex retrogressive landslide, starting with its development from toe to head. Thirteen individual landslide bodies were discovered on the slope. The material of slope formation and a part of weathering zone is caught by the landsliding. The larger part of landslide body is saturated by underground water penetrating through the covering zone in contact with flysch bedrock. The landsliding is relatively shallow, because there is no visible damage affected by sliding in the hydrotechnical tunnel, situated below the landslide toe. The mega-blocks of the limestone rock have also been moved and, most probably, are sliding down the flysch bedrock. This is a special phenomenon, atypical of the flysch slope landslide type in the area of Rijeka. The limestone rock on a scarp is extremely disintegrated, with new visible fractures in it. The site investigations comprised the surveying, seismic and engineering geological explorations. The surveying was performed by the method of terrestrial photogrammetry. The results are compared with aerial photos from 1981. In this respect, it was possible to discover the changes of slope morphology during the period 1981 ā 1997. The photos were also used for the engineering geological mapping supplementation. The seismic surveying was performed by the surface seismic refraction method