Geological Characteristics and Density of the Una Water System as a Factor of Spatial Planning, B&H

Geological structure has a significant effect on maintenance of rainwater on surface and its absorption into the underground. The depth of erosion processes and cutting of river valleys depend of it. Geological factors play an important role in the movement of groundwater. They determine the conditions of formation of groundwater, its position and speed of movement, depth of hydrological insulators and character of hydrological collector. Among other things, hydrogeological relations affect the density of the water system. Geological structure may be a limiting factor when it comes to planning and determining the purpose of the space, and as such, it largely affects the functionality of spatial planning. The highest population density in the area of Una basin is on those parts which are mainly consisted of watertight rocks with higher density of water system.

Keywords:

geological structure density of water system, spatial planning, river Una,

PDF

___

Geologic maps, sheets: Banja Luka, Bihac, Bos. Krupa, Bos. Novi, Drvar, Glamoc, Kljuc, Kostajnica, Prijedor, R 1:100 000, various authors, Savezni geološki zavod Beograd, Beograd 1975.
Geologic map of Yugoslavia, sheets Sarajevo, Zagreb, Dubrovnik, R 1:500 000, various authors, Savezni geološki zavod Beograd, Beograd 1971.
Hydro-geologic map of Yugoslavia, sheets Sarajevo, Zagreb, Dubrovnik, R 1:500 000, Komatina, M. i sar. Beograd 1980.
Interpreter BGM L 33-106 Kostajnica, Savezni geološki zavod, Beograd 1978. Interpreter BGM L 33-118 Prijedor, Savezni geološki zavod, Beograd 1977.
Interpreter BGM L 33-116 Bihać, Savezni geološki zavod, Beograd 1978. Interpreter BGM L 33-129 Drvar, Savezni geološki zavod,
Beograd 1979. Interpreter BGM L 33-119 Banja Luka, Savezni geološki zavod, Beograd 1977. Interpreter BGM L 33-117 Bosanska Krupa, Savezni geološki zavod, Beograd 1979. Interpreter BGM L 33-142 Glamoč, Savezni geološki zavod, Beograd 1978.
Interpreter of Geological map SFRY 1:500 000, Savezni geološki zavod, Beograd 1971.