LES PRINCIPAUX TOPOCLIMATS DU DELTA DU DANUBE

 FLOWING GEOLOGICAL CONDITIONS OF THE UNDERGROUND WATERS IN ZANOAGA TECTONIC GRABEN, BUCEGI MOUNTAINS

 The geological studies made in the area of Bucegi Mountain have covered a large surface in order to be posible the elaboration of a flowing hydrodynamic model of the underground waters. Bucegi Mountain is situated...

 THE HYDRODYNAMIC SIGNIFICATION OF CORRELATIONS ANALYSES

 Take up the carstic hydrostructure as system permits the agreement of internal structure through correlation analysis of different factors which compose the components of impulse (entrance) and of exit. Through t...

 A CASE OF MORPHOHYDROLOGICAL RISK IN DÂMBOVIŢA COUNTY – THE HIGH FLOOD ON ARGEŞ RIVER (GĂEŞTI, APRIL 15-17, 2004) ). DYNAMICAL GEOMORPHOLOGY REMARKS

 On April 15-17, 2004, on Argeş River, at Găeşti, a high flood was formed, the river flow growing up to a maximum value of 142m3/s on April 15 at 18 o’clock (Căteasca). The of the force of erosion increased signific...

 THE SOUTH MOLDAVIAN FORESTS (COVURLUI PLATEAU) AT THE END OF THE 19th CENTURY