Risks Associated To Present Geomorphologic Processes In The Stemnic (Buda) River Basin

Open access


The paper analyses the main geomorphologic processes in the Stemnic (Buda) river basin, conditioned by the joint action of several factors, among which are the lithological peculiarities and the nature of superficial deposits, morphometric characteristics, climate, vegetation type and structure, properties of the soil cover etc. The Stemnic river basin with an area of 15662.52 ha is characterized by its elongated shape (the maximum length is of 30.5 km, maximum width of 8.5 km), its relative lithological homogeneity, but also by a variety of superficial deposits (eluvium, diluvium, colluvium and proluvium, alluvium) and by a relief energy of significant values between 136 m and 10 m (mean value of 73 m). Under these conditions, study area is characterized by a high degree of susceptibility to the occurrence of geomorphologic risk processes. For the morphometric and morphological analysis, we applied the method of the digital terrain model (DTM) with vectorisation of the contour lines on topographic maps with a scale of 1:5,000. In this paper we used indicators that highlight the particular frequency of landslides, especially in the upper and middle sectors, but the rather reduced frequency of deep erosion. Due to the satisfactory coverage of the ground with vegetation, the erosion reaction is differentiated, as it depends on the use of the land and the concentration of liquid flow on the slopes. Consequently, landslides of different ages, types and forms hold large surfaces in the basin (approx. 8%), while surface erosion affects most areas of the slopes, but with different intensities depending on their use and on agricultural technologies.

Băcăuanu V. et al (1980), Moldavian Plateau. Nature. Man. Economy, Editura Ştiinţifică şi Enciclopedică, Bucharest;

Ioniţă I. (2000), Cuesta relief in the Moldavian Plateau, Editura Corson, Iaşi;

Ioniţă I. (2000), Formation and evolution of Ravines Bârladului Plateau, Editura Corson, Iaşi;

Ioniţă I. (2007), Critical erosion season in the Bârladului Plateau, in vol. „ The impact of the hydro-climatic and pedo-geomorphological risks on the environment in the Bârladului Basin”, Editura Universităţii „Al. I. Cuza”, Iaşi;

Jeanrenaud P., Saraiman A. (1995), Geology of Central Moldavia between Siret and Prut Rivers, Editura Universităţii „Al. I. Cuza”, Iaşi;

Larion Daniela (2004), The climate of Vaslui Municipality, Editura Terra Nostra, Iaşi;

Mac I. (1986), Elements of dynamic geomorphology, Editura Acadimei R.S. România, Bucharest;

Moţoc M., Munteanu S., Băloiu V., Stănescu P., Mihai Gh, (1975), Soil erosion and control methods, Editura Ceres, Bucharest;

Pujină D. (1997), Research on some sliding processes of agricultural lands in Bârladului Plateau and contributions to their landscaping, Thesis summary, “Gh. Asachi” Technical University, Iaşi;

Rădoane Maria, Rădoane N., Ichim I., Surdeanu V. (1999), Ravines – forms, processes, evolution, Editura Presa Universitară Clujeană;

Stângă I. C. (2007), Natural hazards. Notions and concepts, Editura Universităţii „Al. I. Cuza”, Iaşi;

Tufescu V. (1966), Natural modelling of the relief and accelerated erosion, Editura Acadimei R.S. România, Bucharest;

Journal Information


All Time Past Year Past 30 Days
Abstract Views 0 0 0
Full Text Views 138 138 14
PDF Downloads 36 36 4