期刊名称：Analele Universităţii din Oradea: Seria Geografie
印刷版ISSN：1221-1273
电子版ISSN：2065-3409
出版年度：2010
卷号：20
期号：1
页码：44-57
语种：English
出版社：University of Oradea Publishing House
摘要：Red Lake in Hasmas (Curmaturii) Mountains was formed by the natural barrage of the Bicaz brook in 1837. In a transversal profile, the western bank is steeper and hard (lithologically), and the eastern bank is mild and crumbly (landslide diluvium). In the same way the submerse slopes are maintained as well. The transport of the sedimentary material depends on the immerse slope, but also on the submerse slope. The central sectors, with great depths, have finer sediments, and the sectors situated immediately next to the river mouths have coarser particles. The total organic carbon and humus are distributed in such a way that they reflect a close connection between the development of vegetation and the zone with immediate impact with the river mouths of the brooks tributary to the lacustrine basin. In the spillway sectors of the main brooks, where important amounts of organic silt can be found, large wetlands develo.
