The delimiting of wetland boundaries is generally performed by taking into account hydrological, geomorphological, pedological, and biological factors. The hydrogeomorphological factors that are considered include elevation, bathymetry, and the nature of the underlying soil. However, in the case of lacustrine wetlands, two factors affecting the distribution of living organisms have been ignored: the inclination and exposure of the slopes from the photic zone. The wetlands around the Red Lake in Romania were delimited using the maps from sonar bathymetric measurements. The processing of the data using GIS techniques revealed minute details about the features of the slopes and the size of the areas with suitable exposure for the living organisms from the lacustrine cuvette to thrive. The greatest depths (10.5 m) were observed in the central sector close to the outlet of the two arteries. The cross-section revealed that the western shore was steep and rocky, while the eastern cross-section had a gentler slope and was crumbly due to landslide. The wetlands associated with the Red Lake developed in the sectors with shallow depths, adequate insolation, and organic soils and limnosoils on gentle slopes, which are frequently or permanently inundated.