Cape Cod , often referred to as simply the Cape , and called Cape of Keel by early Norse explorers, is a peninsula in the easternmost portion of the state of Massachusetts, in the Northeastern United States. It is coextensive with Barnstable County. Several smaller islands off Cape Cod, including Monomoy Island, Monomoscoy Island, Popponesset Island, and Seconsett Island, are also in Barnstable County, being part of municipalities with land on the Cape. The Cape's small-town character and large beachfront attract heavy tourism during the summer months.
Cape Cod was formed as the terminal moraine of a glacier, resulting in a peninsula in the Atlantic Ocean. In 1914, the Cape Cod Canal was cut through the base or isthmus of the peninsula. It is still identified as a peninsula by geographers, who do not change landform designations based on man-made canal construction.
Unofficially, it is one of the biggest barrier islands in the world, shielding much of the Massachusetts coastline from North Atlantic storm waves. This protection helps to erode the Cape shoreline at the expense of cliffs, while protecting towns from Fairhaven to Marshfield.
Road vehicles from the mainland cross over the Cape Cod Canal via the Sagamore Bridge and the Bourne Bridge. The two bridges are parallel, with the Bourne Bridge located slightly farther southwest. In addition, the Cape Cod Canal Railroad Bridge carries railway freight as well as tourist passenger services.
Geographic and political divisions
Cape Cod incorporates all of Barnstable County, which comprises 15 towns: Bourne, Sandwich, Falmouth, and Mashpee, Barnstable, Yarmouth, Dennis, Harwich, Brewster, Chatham, Orleans, Eastham, Wellfleet, Truro, and Provincetown. Two of the county's fifteen towns (Bourne and Sandwich) include land on the mainland side of the Cape Cod Canal. The towns of Plymouth and Wareham, in adjacent Plymouth County, are sometimes considered to be part of Cape Cod but are not located on the peninsula. Some "Cape Codders" (residents of Cape Cod) refer to all land on the mainland side of the canal as "off-Cape." In the 17th century the designation Cape Cod applied only to the tip of the peninsula, essentially present-day Provincetown. Over the ensuing decades, the name came to mean all the land east of the Manomet and Scussett rivers - essentially the line of the 20th century Cape Cod Canal. Now, the complete towns of Bourne and Sandwich are widely considered to incorporate the full perimeter of Cape Cod, even though small parts of these towns are located on the west side of the canal.
For most of the 18th, 19th, and 20th centuries, Cape Cod was considered to consist of three sections:
- The Upper Cape is the part of Cape Cod closest to the mainland, comprising the towns of Bourne, Sandwich, Falmouth, and Mashpee. Falmouth is the home of the famous Woods Hole Oceanographic Institution and several other research organizations, and is also the most-used ferry connection to Martha's Vineyard. Falmouth is composed of several separate villages, including East Falmouth, Falmouth Village, Hatchville, North Falmouth, Teaticket, Waquoit, West Falmouth, and Woods Hole, as well as several smaller hamlets that are incorporated into their larger neighbors (e.g., Davisville, Falmouth Heights, Quissett, Sippewissett, and others).
- The Mid-Cape includes the towns of Barnstable, Yarmouth and Dennis. The Mid-Cape area features many beautiful beaches, including warm-water beaches along Nantucket Sound, e.g. Kalmus Beach in Hyannis, which gets its name from one of the inventors of Technicolor, Herbert Kalmus. This popular windsurfing destination was bequeathed to the town of Barnstable by Dr. Kalmus on condition that it not be developed, possibly one of the first instances of open-space preservation in the US. The Mid-Cape is also the commercial and industrial center of the region. There are seven villages in Barnstable, including Barnstable Village, Centerville, Cotuit, Hyannis, Marstons Mills, Osterville, and West Barnstable, as well as several smaller hamlets that are incorporated into their larger neighbors (e.g., Craigville, Cummaquid, Hyannisport, Santuit, Wianno, and others). There are three villages in Yarmouth: South Yarmouth, West Yarmouth and Yarmouthport. There are five villages in Dennis including, Dennis Village(North Dennis), East Dennis, West Dennis, South Dennis and Dennisport.
- The Lower Cape traditionally included all of the rest of the Cape,or the towns of Harwich, Brewster, Chatham,Orleans, Eastham, Wellfleet, Truro, and Provincetown. This area includes the Cape Cod National Seashore, a national park comprising much of the outer Cape, including the entire east-facing coast, and is home to some of the most popular beaches in America, such as Coast Guard Beach and Nauset Light Beach in Eastham. Stephen Leatherman aka "Dr. Beach" named Coast Guard Beach the 5th best beach in America for 2007.
Late in the 1900s, new arrivals to much of the Lower Cape seemed uncomfortable residing in a place called "Lower" and began calling towns from Eastham to Provincetown the "Outer Cape", a fourth geographic label. Moreover, on a map, Provincetown is above Brewster, they noted. But the newcomers misunderstood the origin and meaning of the terms "Upper" and "Lower" as applied to the Cape. The terms derive from maritime practice of old. In the 18th and much of the 19th centuries the principal means of transportation involved watercraft. And when a boat left Sandwich to the west heading for Wellfleet to the east, for example, it travelled down the longitudinal scale - from up to down the scale. People have long since abandoned nautical charts as they traverse the Cape. The traditional nomenclature became unfamiliar and, therefore, discarded by many. However, the old way holds on elsewhere. On nearby Martha's Vineyard, "Up Island" still is the western section and "Down Island" is to the east, down the scale so to speak.
The large area of water spanning from Plymouth to Provincetown, bordered to the north by Massachusetts Bay and enclosed by Cape Cod, is Cape Cod Bay; west of Cape Cod is Buzzards Bay. To the south lie Nantucket Sound; Nantucket and Martha's Vineyard (both large islands); and the mostly privately owned Elizabeth Islands in the town of Gosnold, of which the most populated is Cuttyhunk.
The highest elevation on Cape Cod is 306 feet (93 m), at the top of Pine Hill, in the Bourne portion of the Massachusetts Military Reservation. The lowest point is sea level.
Geology
"East of America, there stands in the open Atlantic the last fragment of an ancient and vanished land. Worn by the breakers and the rains, and disintegrated by the wind, it still stands bold." - Henry Beston, from his book The Outermost House
Cape Cod forms a continuous archipelagic region with a thin line of islands stretching toward New York, historically known by naturalists as the Outer Lands. This continuity is due to the fact that the islands and Cape are all terminal glacial moraines laid down some 16,000 to 20,000 years ago.
Most of Cape Cod's geological history involves the advance and retreat of the Laurentide ice sheet in the late Pleistocene geological era and the subsequent changes in sea level. Using radiocarbon dating techniques, researchers have determined that around 23,000 years ago, the ice sheet reached its maximum southward advance over North America, and then started to retreat. Many "kettle ponds" — clear, cold lakes — were formed and remain on Cape Cod as a result of the receding glacier. By about 18,000 years ago, the ice sheet had retreated past Cape Cod. By roughly 15,000 years ago, it had retreated past southern New England. When so much of Earth's water was locked up in massive ice sheets, the sea level was lower. Truro's bayside beaches used to be a petrified forest, before it became a beach.
As the ice began to melt, the sea began to rise. Initially, sea level rose quickly, about 15 meters (50 ft) per 1,000 years, but then the rate declined. On Cape Cod, sea level rose roughly 3 meters (11 ft) per millennium between 6,000 and 2,000 years ago. After that, it continued to rise at about 1 meter (3 ft) per millennium. By 6,000 years ago, the sea level was high enough to start eroding the glacial deposits that the vanished continental ice sheet had left on Cape Cod. The water transported the eroded deposits north and south along the outer Cape's shoreline. Those reworked sediments that moved north went to the tip of Cape Cod.
Provincetown Spit, at the northern end of the Cape, consists largely of marine deposits, transported from farther up the shore. Sediments that moved south created the islands and shoals of Monomoy. So while other parts of the Cape have dwindled from the action of the waves, these parts of the Cape have grown.
This process continues today
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