Popham Beach vs. the Morse River
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The meandering Morse River ends its assault on Popham Beach
By Kirsten Weir
The 乐播传媒 Outing Club clambakes at Popham Beach State Park are one reason this sandy stretch of Maine coastline is a touchstone of the 乐播传媒 experience.
Longtime BOC adviser Judy Marden 鈥66 recalls the clambake ritual from her 乐播传媒 days: 鈥淭he night before, we鈥檇 go out and gather driftwood, then camp overnight. Early the next morning we鈥檇 dig pits and start the fires. Then we cooked the lobsters in trash cans with clams and corn.鈥
But this spring, the state asked the BOCers to relocate their clambake, which they did, to Reid State Park a few miles to the east. The reason: There鈥檚 not much public beach left at Popham.
Indeed, while an idealized and immutable Popham looms large in the alumni consciousness, the beach itself has rapidly eroded during the 2000s. These days, only a few feet remain at high tide.
If Popham Beach is this story鈥檚 protagonist, then the antagonist is the Morse River, which exits the coast just west of Popham Beach. In recent years, the river has migrated eastward, cutting away at Popham鈥檚 beach, particularly the western part of the beach, though the center beach, which connects to Fox Island, has also been eroded significantly.
鈥淲e鈥檝e been watching this river shift its course gradually for a long time,鈥 says 乐播传媒 geology professor Mike Retelle. By 2005, he says, 鈥渨e started noticing massive changes鈥 to the Morse River and Popham Beach.
Two factors pushed the river toward the beach. 鈥淎 double whammy,鈥 Retelle says.
One was the relentless growth of a sand spit just offshore from the Morse River outlet. The spit was created by a wave and sand mechanism called longshore sand transport, in which sand-carrying waves hit the shore at an angle and gradually deposit their sediments. Retelle and Dana Oster 鈥09 dubbed the Morse River spit 鈥淚-95鈥 for its great length and width, and it became an 鈥渋nsurmountable barrier鈥 that blocked the Morse from flowing directly into the ocean.
The sand spit deflected the river toward the beach, and the erosion just got worse and worse. 鈥淚t was like a firehose,鈥 Retelle says. As kayakers and canoeists know, when a river curves, the fastest and most powerful flow is the outside of the curve. As the Morse curved into Popham Beach, the strongest part of the current was eating away at the beach.
鈥淵ou want to see natural processes play out,鈥 Retelle says.
River outlets are always 鈥渢he most dynamic places鈥 along the coast, says Retelle. Even so, the stunning changes at Popham had observers 鈥渋n a panic鈥 by this past winter, Retelle says. Erosion had carved deeply into the dunes and toppled hundreds of shoreline pine trees. The ocean was within feet of the parking lot, and it threatened the park鈥檚 new bathhouses. State geologists say it鈥檚 the beach鈥檚 greatest retreat in a century.
In its inexorable eastward march, the river had even cut through the sand bar, known as a tombolo, making it nearly impossible for visitors to walk from Popham to Fox Island.
This past February, some local residents urged that a channel be cut through the sand spit to allow the river to return to a north-south orientation. But others said that the river, and nature, should take its course.
鈥淔rom an environmental perspective, you want to see natural processes play out,鈥 Retelle says. 鈥淥therwise you won鈥檛 know what would have happened.鈥
The 乐播传媒鈥揗orse Mountain Conservation Area is just across the Morse River from Popham Beach, and director Laura Sewall also opposed taking action.
鈥淭he mission of the conservation area emphasizes protecting ecological integrity and educational opportunities. That鈥檚 primary,鈥 says Sewall.
She subscribes to a philosophy promoted by naturalist Aldo Leopold, she explains: 鈥淚f you want to understand a natural system, you can鈥檛 study one that has already been in any way altered.鈥
While public attention peaked over the winter, scientists like Retelle and state geologist that the river was about to change course.
In April 2009, as Retelle and his students were doing measurements on that aforementioned I-95 sand spit, they saw a dry channel right across the spit, about 2 meters wide 鈥 evidence that the river had momentarily breached the spit during a recent storm and its associated high tide.
According to Dickson, the channel was the first sign of 鈥渁 new, and more direct, course to the sea across the…spit.鈥 In fact, winter storms had begun shaving the sand spit little by little over the last two years, Retelle says. He and Dickson agreed that a few more fierce winter storms would do the trick.
On Feb. 25 and 26, 2010, a major northeaster proved them right, as gale winds and high tides helped the Morse River barrel through the mound of sand to create a new north-south flow away from Popham Beach.
鈥淚 never know what I鈥檓 going to see when I go down to Popham.鈥
With summer鈥檚 arrival, calmer wave action should allow sand to be re-deposited along Popham, explains Retelle, so the beach should begin to grow again. In fact, Retelle and his geology thesis student, Molly Newton 鈥11 of Easthampton, Mass., are now working with the state to monitor the recovery of Popham Beach.
It鈥檚 an intriguing project, he says. 鈥淚 never know what I鈥檓 going to see when I go down to Popham.鈥
Kirsten Weir is a science writer based in southern Maine.




