Profiling of a sandy hill

Profiling of a sandy hill. Movement of a georadar was from the foot of the hill (left) to its top (right). Therefore, signals from the grown water table and various boundaries are drifting down. A major nonuniformity is recorded almost at the top of the hill, at the depth of 35 m. Sounding frequency: 38 MHz. Location area: vicinity of Lilaste lake, Latvia.

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