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Statistical modeling of the long-range-dependent structure of barrier island framework geology and surface geomorphology

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Figure

Figure 1. Location map and DEM of the study area at Padre Is-land National Seashore (PAIS), Texas, United States
Figure 2. The 100 km (a) and 10 km (b) alongshore EMI surveys showing DEMs of the study area and previously identified paleo-channelregion by Fisk (1959)
Figure 3. Comparison of EMI σa responses from the 100 km survey with 100 MHz GPR data within one of the Fisk (1959) paleo-channels.The 800 m segment (A–A′) crosses a smaller stream within the network of paleo-channels in the central zone of PAIS
Figure 4. DEM metrics extracted from aerial lidar data. The sampling interval (step size) for each data series is 10 m and the coordinates arematched with each EMI acquisition point
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