A Road Less Traveled
Cape Cod's two-lane Route 6A offers a direct conduit to a New England of yesteryear
- By Jonathan Kandell
- Smithsonian magazine, April 2005, Subscribe
(Page 2 of 4)
The cape was formed by a glacier that retreated some 15,000 years ago, leaving behind the bay and the sandy peninsula that is constantly battered and reshaped by the Atlantic Ocean. By 8,000 years ago, the rising ocean had separated Nantucket and Martha's Vineyard from the peninsula's southern coast. "The basic fact of life around here is erosion," says Admont Clark, 85, a retired Coast Guard captain and founder of the Cape Cod Museum of Natural History, in Brewster (pop. 8,376), a few miles east of Dennis. "Every year, about three feet of beach are washed away and deposited elsewhere on the cape." It is pretty much a zero-sum game in the short run. But over a century or so, some ten inches of coastline are lost altogether.
During the past decade, two lighthouses, wobbling on bluffs undercut by constant waves, had to be placed on flatbed trailers and moved to more stable locations. Islets and inlets are repeatedly exposed and submerged, forcing harbor masters to update their maps frequently. Residents pay close attention to approaching storms, boarding up windows and otherwise battening down.
To walk Cape Cod's beaches and tidal flats is to be made aware that the terrain and waters shift by the hour—or the minute. The tides can fatally fool even the most knowledgeable old-timers. In the reedy wetlands behind my beachside bed-and-breakfast, I encounter the carcass of a seal, marooned by a rapidly receding tide. Clark recalls an ill-fated, 90-year-old farmer who scoured the flats for clams all his life. "One day about ten years ago the clamming was so good that he wasn't watching the rising waters around him," says Clark. "He drowned trying to swim back."
On an outing with Irwin Schorr, volunteer guide for the Museum of Natural History, I experience the vitality of this landscape. At his suggestion, I jump on a patch of grass—and bounce as if it were a mattress. "It's because of the constant tidal flooding," says Schorr. "Water is absorbed in between the grass roots and filtered underground into our aquifer."
When marsh grasses die, their stalks are absorbed into a spongy network of roots, forming peat. Bacterial decomposition nourishes crabs, crayfish and snails that in turn attract larger marine life and birds. Along the edges of a wood-planked walkway, I peer at fish—sticklebacks and silversides—feeding on mosquito larvae. The tide has risen so high we have to take off our shoes, roll up our pants and wade barefoot. A snaking column of recently hatched herring, glimmering in the tide, streaks toward the bay. Their timing is exquisite: within an hour, the water has receded so far there is a hardly a puddle left in the marsh. "The tide here rises and falls seven to nine feet every day," says Schorr.
Ranger Katie Buck, 23, patrols Roland C. Nickerson State Park, at the eastern end of the main part of 6A. The 2,000-acre preserve is a forest of oak, pine and spruce, populated by deer, raccoons, fox, coyotes and enough frogs to belie any global amphibian crisis.
"Sometimes there are so many they stick to the door and windows of our station," says Buck.
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