Abstract: | Somuzu Mare river is a Siret affluent and its origin is in Liteni depression. It crosses the whole north-west depression area, and through first class affluents (Lãmãºanca, Graniþa, Stupca, Drãgoiasca and others), it develops a lot of ridges, due exclusevely to the subsequent nature of the stream system.
Glacis microrelief, alluvial fans, special river flats represent a trully phreatic waters „store”, also related with lithologic constitution, on support clayey.
Hydrogeological aspects in Somuzu Mare superior basin have been considered part of natural resources from Suceava' s tableland western area, near the contact with carpethians miocene unit.
The attachment of phreatic waters map, with hydrocontourlines and hydroisobathes drawing, completes the information regarding hydrogeologic resources, their way of using and, related to this, the monitoring of other natural resources, like the soils and vegetation. |
