The river regulations of the 19th century have affected each of our rivers to a different degree. In the
case of the River Bodrog it was stronger than the average. In our paper a section of the river between
Bodroghalász and Szegi was examined, the extent and intensity of river channel changes was
intended to be determined. The applied series of maps and aerial photos was georeferred and the river
channel was vectorized. The morphometric parameters of the channel were measured and the changes
were evaluated using the created database. From methodological aspect we concluded that the 9
variables can be grouped into 3 factors therefore most of the indexes can be substituted. We measured
the changes of length and lateral shift of the channel using GIS methods. Three development periods
were identified based on our results. In the first period the development of the river was characterized
by natural processes. Then, the development of the river altered owing to the antropogenic impacts. In
this transient phase the average shifting of the channel was 7.43 m/y. In the third term this value
reduces to 0.2 m/y as the river is getting to reach the equilibrium stage.
The terraces of the Tárkány Basin, located in the SW part of the Bükk Mountains are known since the beginning of the 20th century. Based on field surveys, six morphological levels were delineated and described in 1936. During the later geological mapping surveys, three gravel terraces had been mapped in the basin. Since then, no comprehensive morphological mapping has been made in the Tárkány Basin. Our study aimed to validate the results of these early studies using a digital elevation model. We delineated the remnant surfaces of the basin by morphometric and GIS techniques. Then, based on field surveys and former geological maps; we characterised these remnant surfaces, and their area was measured as well. The results of this study contribute to a better understanding of the surface evolution of the basin and its surroundings.
The Thutapuzha watershed (TW) is one among the major tributaries of Bharathapuzha – the largest west flowing river in Kerala, India. Morphometric analysis was carried out to determine the spatial variations in the drainage characteristics and to understand the prevailing geologic variation, topographic information and structural setup of TW using Survey of India topographic maps and ASTER-DEM. Geoprocessing techniques has been used for the delineation and calculation of the morphometric parameters of the watershed. The TW sprawled over 1107Km2 and the study revealed that the watershed includes a sixth order stream and lower order streams mostly dominate the basin with a drianage density of 1.36 m/Km2 exhibiting highly resistant subsoil, dense vegetation, and low relief of surface nature . The study indicate that rainfall has a significant role in the drainage development whereas the drainage pattern is controlled by structure and relief. The watershed of TW is moderate to well-drained and exhibited a geomorphic maturity in its physiographic development. The shape parameters revealed the elongated nature of TW having less prone to flood, lower erosion and sediment transport capacities and drainage network development in the watershed. This study strongly brings to light that the drainage morphometric parameters have the enormou spotentiality to unveil the hydro-morphologicalcharacteristics of the river basins. Integrating hydro-morphological characteristics with conventional watershed assessment methods would have a beneficial effect on judicious watershed management, which helped to formulate a comprehensive watershed management plan.