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https://doi.org/10.21861/HGG.2005.67.02.02

The Upper Part of the Una River Valley Between Martin Brod and Pritoka - Geomorphological Characteristics

Andrija Bognar

Puni tekst: engleski, pdf (128 KB) str. 21-38 preuzimanja: 2.179* citiraj
APA 6th Edition
Bognar, A. (2005). The Upper Part of the Una River Valley Between Martin Brod and Pritoka - Geomorphological Characteristics. Hrvatski geografski glasnik, 67. (2.), 21-38. https://doi.org/10.21861/HGG.2005.67.02.02
MLA 8th Edition
Bognar, Andrija. "The Upper Part of the Una River Valley Between Martin Brod and Pritoka - Geomorphological Characteristics." Hrvatski geografski glasnik, vol. 67., br. 2., 2005, str. 21-38. https://doi.org/10.21861/HGG.2005.67.02.02. Citirano 23.10.2021.
Chicago 17th Edition
Bognar, Andrija. "The Upper Part of the Una River Valley Between Martin Brod and Pritoka - Geomorphological Characteristics." Hrvatski geografski glasnik 67., br. 2. (2005): 21-38. https://doi.org/10.21861/HGG.2005.67.02.02
Harvard
Bognar, A. (2005). 'The Upper Part of the Una River Valley Between Martin Brod and Pritoka - Geomorphological Characteristics', Hrvatski geografski glasnik, 67.(2.), str. 21-38. https://doi.org/10.21861/HGG.2005.67.02.02
Vancouver
Bognar A. The Upper Part of the Una River Valley Between Martin Brod and Pritoka - Geomorphological Characteristics. Hrvatski geografski glasnik [Internet]. 2005 [pristupljeno 23.10.2021.];67.(2.):21-38. https://doi.org/10.21861/HGG.2005.67.02.02
IEEE
A. Bognar, "The Upper Part of the Una River Valley Between Martin Brod and Pritoka - Geomorphological Characteristics", Hrvatski geografski glasnik, vol.67., br. 2., str. 21-38, 2005. [Online]. https://doi.org/10.21861/HGG.2005.67.02.02

Sažetak
The Una River Valley has complex characteristics defined by the interchange of gorges, basins and valley extensions. The river has adapted itself to the primary geologic structure and to the activity of tectonic movements. The longitudinal profile of the river is the result of numerous rapids, cascades and waterfalls, the formation of which is connected with calcareous sinter accumulation. Morphogenetic analysis has shown that a series of very attractive and strange relief forms is being formed in the riverbed of the River Una such as calcareous sinter barriers, sinter riverbeds, calcareous sinter islands and caves.

Ključne riječi
Una River; calcareous sinter; riverbed; micro-landforms

Hrčak ID: 9741

URI
https://hrcak.srce.hr/9741

Posjeta: 2.742 *