Long Beach (Rockport)
From Wikipedia, the free encyclopedia
Long Beach | |
|---|---|
Neighborhood | |
| Country | United States |
| State | Massachusetts |
| County | Essex |
| Town | Rockport |
| Time zone | UTC-5 (EST) |
| • Summer (DST) | UTC-4 (EDT) |
Long Beach is a coastal neighborhood on the eastern shore of Rockport, Massachusetts, characterized by 152 seasonal cottages built on a sandy spit barrier beach.[1] The neighborhood faces significant vulnerabilities from climate change, including sea level rise and increasingly severe storm events, making it a focal point for debates over coastal adaptation strategies.[2]
Long Beach is located on a barrier beach on Rockport's eastern coast, forming a natural protection for the Saratoga salt marsh behind it. The sandy spit extends approximately three-quarters of a mile along the coast, ending at a narrow creek that allows ocean water to feed the tidal marsh.[1] For thousands of years prior to development, the dune system shifted naturally with the tides and seasons.[2]
History
In the 1800s, Finnish granite workers emigrated to Rockport and armored the coast with breakwaters, creating a series of safe harbors to protect the fishing and shipbuilding industries. The availability of quarried granite and the construction of hard infrastructure became part of the Cape's cultural imaginary.[2]
In the early 1900s, 149 seasonal cottages and accessory buildings were constructed on top of the barrier beach.[2] The cottages were initially defended from storm surge by a wooden bulkhead. Fill was dumped on the dune system, and the area was developed with manicured lawns featuring ornamental plant species including roses, hydrangeas, and catmint.[2]
When the wooden bulkhead burned in 1931, the Town of Rockport and the Commonwealth of Massachusetts split the cost to construct a 3,350-foot concrete seawall.[2] In 1958, a fierce late-season nor'easter washed over the first wall and toppled it seaward onto the beach.[1] Subsequent storms in 1976, 1985, 1991, and 2018 caused further damage to the seawall and eroded the fill behind it. Parts of the current seawall date to 1931 and 1959.[2]