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Billingsgate Island, also sometimes known as Bellingsgate Island, was an island off Cape Cod in Massachusetts in the United States. Originally settled as a fishing and whaling community as part of the town of Eastham, Massachusetts , Billingsgate Island was for a long time the site of a lighthouse used as a navigational aid in Cape Cod Bay .
Tide tables, sometimes called tide charts, are used for tidal prediction and show the daily times and levels of high and low tides, usually for a particular location. [1] Tide heights at intermediate times (between high and low water) can be approximated by using the rule of twelfths or more accurately calculated by using a published tidal ...
A U.S. Coast Guard boat steams past in 2021 as workers prepare to deploy a tidal turbine onto a lift arm on a platform just west of the railroad bridge on the Cape Cod Canal in Buzzards Bay.
The Cape Cod Canal is an artificial waterway in Massachusetts connecting Cape Cod Bay in the north to Buzzards Bay in the south, and is part of the Atlantic Intracoastal Waterway. The approximately 7.4-mile-long (11.9 km) canal traverses the neck of land joining Cape Cod to the state's mainland. It mostly follows tidal rivers widened to 480 ...
The islands of Massachusetts range from barren, almost completely submerged rocks in Massachusetts Bay (e.g. Abbott Rock, first on the list below) to the large, famous and heavily visited Martha's Vineyard and Nantucket. The recent history of Massachusetts' islands includes creation by flooding, connection to the mainland and subsumption into ...
Woods Hole is located at the southwestern tip of the town of Falmouth (and of Cape Cod) at (41.526730, -70.663184 The term "Woods Hole" refers to a strait named Woods Hole, which separates Cape Cod from the Elizabeth Islands (specifically, Uncatena Island and Nonamesset Island) and which boats, yachts, and small ferries can use to travel between Vineyard Sound and Buzzards Bay.
Buzzards Bay was created during the latter portion of the Pleistocene epoch through the interplay of glacial and oceanic processes. Beginning fifty thousand to seventy thousand years ago, the edges of the continental ice sheet covering much of North America began to fluctuate, leaving moraines to mark the former extent of the receded ice.
The Massachusetts Office of Coastal Zone Management limits its definition of the South Shore to the municipalities between Boston Harbor and Cape Cod, which includes Atlantic coastal and coastal watershed areas "from the three-mile (5 km) limit of the state territorial sea to 100 feet (30 m) beyond the first major land transportation route encountered (a road, highway, rail line, etc.)". [4]