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Home > Explore! > Marine Geology > Field Localities > Seawall and Popham Beach Dynamics > Figure 22
Figure 22. Loss of relict dunes at Popham Beach state park is severe along the bank of the Morse River. The pitch pine forest has been growing for at least 50 years based on historical aerial photographs. Near the eastern end of the Seawall Beach spit the Morse River channel is directed close to the state park beach in the background. MGS file photo by S. M. Dickson taken November 4, 2008. Last updated on November 6, 2008 |
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