This article presents the change while following the right bank of the Prut River from territorial administrative unit of the Prisacani commune - Iasi County in the period 1985 - 2015, caused by erosion / deposition of sediments, highlighted by comparing the ground surface modification of Prisacani Territorial Administrative Unit (TAU) in the observed period of time. The reference terrain of Prisacani TAU was considered the one defined by the territorial-administrative boundary during the last cadastral demarcation and the cadastral right bank of the Prut river digitized on topographic maps at 1:25000 scale edited in 1985. The reference terrain of Prisacani TAU used to conduct the comparative study was determined on the basis of admin...
The fluvial process is characterized by an intense meandering riverbed. The aim of this study was to...
<p>Situated in the north-eastern part of the Romanian Plain,<br />Lower Siret Plain is known in lite...
This article is focused on the analysis and evaluation of the changes of the bottom of the Bakomi re...
The planimetric position of the river banks is a main parameter in detecting the areas affected by e...
The article discusses the historical geography of the river Prut (967 km). In the ancient period it ...
The paper presents elements of analysis of the temporal stability of earth dams by using topographic...
The study captures the spatial-temporal evolution of the Someș river bed and the anthropic interfere...
In the last century in the south part of Moldavian Plain took place major land use changes, with irr...
The paper presents an analysis of the degradation phenomena of the riparian environment ...
The current geomorphologic processes are a form of land degradation. This is accomplished by mechani...
Studinet catchment is situated in the eastern part of Romania (Tutova Rolling Hills), having a surfa...
A diachronic analysis of the geomorphic units using a geographical information system (GIS) that int...
Climate changes and anthropogenic activities in the last centuries have modified the hydro-morpholo...
The river channel dynamics are result of the complex interaction between natural and human impact...
The article shows the influence of land reclamation and regulation of rivers on the transformation o...
The fluvial process is characterized by an intense meandering riverbed. The aim of this study was to...
<p>Situated in the north-eastern part of the Romanian Plain,<br />Lower Siret Plain is known in lite...
This article is focused on the analysis and evaluation of the changes of the bottom of the Bakomi re...
The planimetric position of the river banks is a main parameter in detecting the areas affected by e...
The article discusses the historical geography of the river Prut (967 km). In the ancient period it ...
The paper presents elements of analysis of the temporal stability of earth dams by using topographic...
The study captures the spatial-temporal evolution of the Someș river bed and the anthropic interfere...
In the last century in the south part of Moldavian Plain took place major land use changes, with irr...
The paper presents an analysis of the degradation phenomena of the riparian environment ...
The current geomorphologic processes are a form of land degradation. This is accomplished by mechani...
Studinet catchment is situated in the eastern part of Romania (Tutova Rolling Hills), having a surfa...
A diachronic analysis of the geomorphic units using a geographical information system (GIS) that int...
Climate changes and anthropogenic activities in the last centuries have modified the hydro-morpholo...
The river channel dynamics are result of the complex interaction between natural and human impact...
The article shows the influence of land reclamation and regulation of rivers on the transformation o...
The fluvial process is characterized by an intense meandering riverbed. The aim of this study was to...
<p>Situated in the north-eastern part of the Romanian Plain,<br />Lower Siret Plain is known in lite...
This article is focused on the analysis and evaluation of the changes of the bottom of the Bakomi re...