Hidrológiai Közlöny 2005 (85. évfolyam)
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(1992): Fractals and Chaos in Geology and Geophysics. Cambridge Univ. Press, Cambridge. 398 o. Warne, A. G., Tóth, L. A., White, W. A. (2000): Drainage basin-scale geomorphic analysis to determine reference conditions for ecologic restoration - Kissimmee River, Florida. Geol. Soc. Am. Bull. 112: 884-899. Williams, G. P. (1978): Bankfull discharge of rivers. Water Resource Research 14: 1141-1154. Wolman, M. G. (1954): A method of sampling coarse river-bed material. Am. Geophys. Union Trans. 35: 951-956. A kézirat beérkezett: 2004. június 7-én TIMÁR GÁBOR Abstract: Key words: dr., oki. geofizikus (1991), Ph.D. (2003), az ELTE TTK tudományos munkatársa Planform types of alluvial rivers and the conditions of their occurance Literature overview and consequences in the practice Timár, G. The alluvial rivers, flowing on their own sediment, show different, characterizable planforms. Besides the braided and meandering (sinuous), the most important types, the wandering, anabranching, anastomosing and straight planforms also occur. This work starts with a literature overview of the characteristics of these types and also the environmental parameters controlling their occurance. These parameters and the resulted planforms are depicted along the alluvial section of the Tisza River. The work ends with some consequences and examples concerning the practice of the river control measures, river regulation, river planform, meandering, self-organizing systems
