Geography Reference
In-Depth Information
the location of the same coastline (2 up to 3.5 km) in the same year 1592 remains between F
and P maps, therefore neither reliable coastal erosion rates (Figure 16) nor a correct point-
by-point response of the ancient beach line to the wind-induced long shore currents (Figure
17) can be believably proposed.
Figure 14.
Overlay of the “false case”, georeferenced by means of a second order polynomial
transformation, on present high resolution satellite images (
Bing Maps
TM
environment).
