102
70°0
65· 0
60· 0
M. Cintia Piccolo· Gerardo M.E. Perillo
TIDAL AMPLITUDE
Microtidal
h;::;:';) Mesotidal
~ Macrotidal
55°0
35°5
40· 5
45°5
50· 5
55°5
50· 0
Fig. 6.1. Map of the Argentine coast showing the estuaries that discharge in the Argentine sea
on dIy, the sandy soil induces high water infiltration. In both cases, there is a reduction of the stream discharge and; therefore, a reduction in the deepening and channel
building capacity by the river.
70°0
65· 0
60· 0
M. Cintia Piccolo· Gerardo M.E. Perillo
TIDAL AMPLITUDE
Microtidal
h;::;:';) Mesotidal
~ Macrotidal
55°0
35°5
40· 5
45°5
50· 5
55°5
50· 0
Fig. 6.1. Map of the Argentine coast showing the estuaries that discharge in the Argentine sea
on dIy, the sandy soil induces high water infiltration. In both cases, there is a reduction of the stream discharge and; therefore, a reduction in the deepening and channel
building capacity by the river.