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Original scientific paper

The Recent Geomorphological Processes in the Area of the Rijeka Bay

Čedomir Benac

Fulltext: croatian, pdf (5 MB) pages 1-17 downloads: 668* cite
APA 6th Edition
Benac, Č. (1992). Recentni geomorfološki procesi i oblici u području Riječkog zaljeva. Hrvatski geografski glasnik, 54. (1.), 1-17. Retrieved from https://hrcak.srce.hr/63746
MLA 8th Edition
Benac, Čedomir. "Recentni geomorfološki procesi i oblici u području Riječkog zaljeva." Hrvatski geografski glasnik, vol. 54., no. 1., 1992, pp. 1-17. https://hrcak.srce.hr/63746. Accessed 5 Dec. 2021.
Chicago 17th Edition
Benac, Čedomir. "Recentni geomorfološki procesi i oblici u području Riječkog zaljeva." Hrvatski geografski glasnik 54., no. 1. (1992): 1-17. https://hrcak.srce.hr/63746
Harvard
Benac, Č. (1992). 'Recentni geomorfološki procesi i oblici u području Riječkog zaljeva', Hrvatski geografski glasnik, 54.(1.), pp. 1-17. Available at: https://hrcak.srce.hr/63746 (Accessed 05 December 2021)
Vancouver
Benac Č. Recentni geomorfološki procesi i oblici u području Riječkog zaljeva. Hrvatski geografski glasnik [Internet]. 1992 [cited 2021 December 05];54.(1.):1-17. Available from: https://hrcak.srce.hr/63746
IEEE
Č. Benac, "Recentni geomorfološki procesi i oblici u području Riječkog zaljeva", Hrvatski geografski glasnik, vol.54., no. 1., pp. 1-17, 1992. [Online]. Available: https://hrcak.srce.hr/63746. [Accessed: 05 December 2021]

Abstracts
In the paper has been analysed arecent geomorphological processes in coastal area of Rijeka Bay (Northern Adriatic). The rapidly sea-level rise started from the end of last Würm glacial age. Therefore the erosion base, the relief energy and the intensity of the erosion and the sedimentation have chaged. The lower parts of the numerious valleys have been submerged. The rapid sedimentation began near the Rječina River mouth. In the last milleniums there is expressive work of abrasion and bioerosion. The initial forms of the abrasion platform has been formed. The process abrasion is very selective. It primarily depends of geological structure and hardness of rocks in the littoral zone as well as of the local maritime conditions. A relief of the greatest part of the coastal area of Rijeka Bay depends primarily of local srtuctural and tectonic rock fabric. In littoral zone of carbonate composition we have been seen processes of bioerosion. The processes of bioerosion are apparently in the carbonate rocks of littoral zone. The gullies are active on slopes of Učka Mountain and island Cres, but this are mainly fossil in northern coastland and island Krk.

Keywords
recent geomorphological process; marine abrasion; littoral sedimentation; littoral bioerosion; Rijeka Bay; Adriatic Sea

Hrčak ID: 63746

URI
https://hrcak.srce.hr/63746

[croatian]

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