Changes

Formed in large areas with the accumulation of sand deposition. The sediment resulting  from wind-blown sand. The clastic texture of the environment is granules ( 2 mm – 4 mm) and coarse (over 2 mm) (table 1).

Formed in large areas with the accumulation of sand deposition. The sediment resulting  from wind-blown sand. The clastic texture of the environment is granules ( 2 mm – 4 mm) and coarse (over 2 mm) (table 1).

[[File:Modern_dunes-McKee.jpg|500px|thumbnail|center|Table 1- Modern dunes classification (Adapted from McKee, 1979).]]

[[File:Modern_dunes-McKee.jpg|500px|thumbnail|center|{{table number|1|}}Modern dunes classification (Adapted from McKee, 1979).]]

====Fluvial Reservoir====

====Fluvial Reservoir====