EtymologyThe word is an Algonquian languages, Algonquian word referring to a village 'at a big river'. It is the seventh-oldest surviving English place-name in the United States, first applied as ''Chesepiook'' by explorers heading north from the Roanoke Colony into a Chesapeake tributary in 1585 or 1586. The name may also refer to the Chesapeake people or the Chesepian, a Native American tribe who inhabited the area now known as South Hampton Roads in the U.S. state of Virginia. They occupied an area that is now the Norfolk, Portsmouth, Chesapeake, and Virginia Beach areas. In 2005, Algonquian linguist Blair Rudes "helped to dispel one of the area's most widely held beliefs: that 'Chesapeake' means something like 'great shellfish bay'. It does not, Rudes said. The name might have actually meant something like 'great water', or it might have just referred to a village location at the Bay's mouth."
Geology and formationThe Chesapeake Bay is an estuary to the North Atlantic, lying between the Delmarva Peninsula to the east and the North American mainland to the west. It is the ''ria'', or drowned valley, of the , meaning that it was the alluvial plain where the river flowed when the sea level was lower. It is not a ''fjord'', because the Laurentide Ice Sheet never reached as far south as the northernmost point on the Bay. North of Baltimore, the western shore borders the hilly Piedmont (United States), Piedmont region of Maryland; south of the city the Bay lies within the state's low-lying Atlantic coastal plain, coastal plain, with sedimentary cliffs to the west, and flat islands, winding creeks and marshes to the east. The large rivers entering the Bay from the west have broad mouths and are extensions of the main ria for miles up the course of each river. The Bay's geology, its present form, and its very location were created by a bolide impact event at the end of the Eocene (about 35.5 million years ago), forming the Chesapeake Bay impact crater and much later the Susquehanna River valley. The Bay was formed starting about 10,000 years ago when rising sea levels at the end of the last ice age flooded the Susquehanna River valley. Parts of the Bay, especially the Calvert County, Maryland, coastline, are lined by cliffs composed of deposits from receding waters millions of years ago. These cliffs, generally known as Calvert Cliffs State Park, Calvert Cliffs, are famous for their fossils, especially fossilized shark teeth, which are commonly found washed up on the beaches next to the cliffs. Scientists' Cliffs is a beach community in Calvert County named for the desire to create a retreat for scientists when the community was founded in 1935.
HydrologyMuch of the Bay is shallow. At the point where the Susquehanna River flows into the Bay, the average depth is , although this soon diminishes to an average of southeast of the city of Havre de Grace, Maryland, to about just north of Annapolis. On average, the depth of the Bay is , including tributaries; over 24 percent of the Bay is less than deep. Because the Bay is an estuary, it has fresh water, salt water and brackish water. Brackish water has three salinity zones: oligohaline, mesohaline, and polyhaline. The freshwater zone runs from the mouth of the Susquehanna River to north Baltimore, Maryland, Baltimore. The oligohaline zone has very little salt. Salinity varies from 0.5 Concentration#"Parts-per" notation, ppt (parts per thousand) to 10 ppt, and freshwater species can survive there. The north end of the oligohaline zone is north Baltimore and the south end is the Chesapeake Bay Bridge. The mesohaline zone has a medium amount of salt and runs from the Bay Bridge to the mouth of the Rappahannock River. Salinity there ranges from 1.07% to 1.8%. The polyhaline zone is the saltiest zone, and some of the water can be as salty as sea water. It runs from the mouth of the Rappahannock River to the mouth of the Bay. The salinity ranges from 1.87% to 3.6%. (3.6% is as salty as the ocean.) The climate of the area surrounding the Bay is primarily humid subtropical, with hot, very humid summers and cold to mild winters. Only the area around the mouth of the Susquehanna River is continental in nature, and the mouth of the Susquehanna River and the Susquehanna mudflat, flats often freeze in winter. It is rare for the surface of the Bay to freeze in winter, something that happened most recently in the winter of 1976–77. The largest rivers flowing directly into the Bay, from north to south, are: * * Patapsco River * Chester River * Miles River * Choptank River * Patuxent River * Nanticoke River * * Pocomoke River * Rappahannock River * York River (Virginia), York River * James River (Virginia), James River
Flora and faunaThe Chesapeake Bay is home to numerous fauna that either migrate to the Bay at some point during the year or live there year-round. There are over 300 species of fish and numerous shellfish and crab species. Some of these include the Atlantic menhaden, striped bass, American eel, eastern oyster, Atlantic horseshoe crab, and the Callinectes sapidus, blue crab. Birds include ospreys, great blue herons, bald eagles, and peregrine falcons, the last two of which were threatened by DDT; their numbers plummeted but have risen in recent years. The piping plover is a near threatened species that inhabits the wetlands. Larger fish such as Atlantic sturgeon, varieties of sharks, and stingrays visit the Chesapeake Bay. The waters of the Chesapeake Bay have been regarded one of the most important nursery areas for sharks along the east coast.The National Aquarium
Pre ColumbianThe Chesapeake Bay has had a human presence for over 11,500 years. “Paleoindians,” or the first humans in the Chesapeake Bay region, lived off the land by hunting games and living off the earth in small nomadic groups. Archeologists have also noted the presence of “foreign” stones in projectile points that came via trade from other parts of North America. For thousands of years, Native American societies lived in villages of wooden longhouses close to water bodies where they fished and farmed the land. Agricultural products included beans, corn, tobacco, and squash. Villages often lasted between 10 to 20 years before being abandoned due to local resources such as firewood running out or soil depleting. To produce enough food, labor was divided with men hunting while the women supervised the village’s farming. All village members took part in the harvesting of fish and shellfish from the local bodies of water. As time went on, communities around Chesapeake Bay formed confederations such as the Powhatan, the Piscataway, and the Nanticoke. Each of these confederations consisted of a collections of smaller tribes falling under the leadership of a central chief.
European exploration and settlementFile:1630 Hondius Map of Virginia and the Chesapeake - Geographicus - NovaVirginiaeTabula-hondius-1630.jpg, Later (1630) version of the 1612 map by Captain John Smith during his exploration of the Chesapeake. The map is oriented with west at top. In 1524, Italian explorer Giovanni da Verrazzano, (1485–1528), in service of the Kingdom of France, French crown, (famous for sailing through and thereafter naming the entrance to New York Bay as the "The Narrows, Verrazzano Narrows", including now in the 20th century, a suspension bridge also named for Verrazano-Narrows Bridge, him) sailed past the Chesapeake, but did not enter the Bay. Spanish explorer Lucas Vásquez de Ayllón sent an expedition out from Hispaniola in 1525 that reached the mouths of the Chesapeake and Delaware Bays. It may have been the first European expedition to explore parts of the Chesapeake Bay, which the Spaniards called "Bahía de Santa María" ("Bay of St. Mary") or "Bahía de Madre de Dios."("Bay of the Mother of God") De Ayllón established a short-lived Kingdom of Spain, Spanish mission settlement, San Miguel de Gualdape, in 1526 along the Atlantic Ocean, Atlantic coast. Many scholars doubt the assertion that it was as far north as the Chesapeake; most place it in present-day Georgia (U.S. state), Georgia's Sapelo Island. In 1573, Pedro Menéndez de Márquez, the governor of Spanish Florida, conducted further exploration of the Chesapeake. In 1570, Spanish Jesuits established the short-lived Ajacan Mission on one of the Chesapeake tributaries in present-day Virginia. The arrival of English people, English colonists under Sir Walter Raleigh and Humphrey Gilbert in the late 16th century to found a colony, later settled at Roanoke Island (off the present-day coast of North Carolina) for the Virginia Company, marked the first time that the English approached the gates to the Chesapeake Bay between the capes of Cape Charles and Cape Henry. Three decades later, in 1607, Europeans again entered the Bay. Captain John Smith of Kingdom of England, England explored and mapped the Bay between 1607 and 1609, resulting in the publication in 1612 back in the British Isles of ''"A Map of Virginia"''. Smith wrote in his journal: "Heaven and earth have never agreed better to frame a place for man's habitation." The new laying out of the "Captain John Smith Chesapeake National Historic Trail", the United States' first designated "all-water" National Historic Trail, was created in July 2006, by the National Park Service of the United States Department of the Interior, U.S. Department of the Interior following the route of Smith's historic 17th-century voyage. Because of economic hardships and civil strife in the "Mother Land", there was a mass migration of southern English Cavaliers and their servants to the Chesapeake Bay region between 1640 and 1675, to both of the new colonies of the Province of Virginia and the Province of Maryland.
American Revolution to the presentThe Chesapeake Bay was the site of the Battle of the Chesapeake (also known as the "Battle of the Capes", Cape Charles and Cape Henry) in 1781, during which the French fleet defeated the Royal Navy in the decisive naval battle of the American Revolutionary War. The British defeat enabled George Washington, General George Washington and his Kingdom of France, French allied armies under Jean-Baptiste Donatien de Vimeur, Comte de Rochambeau, Comte de Rochambeau to march down from History of New York City, New York and bottle up the rampaging southern British Army of Lord Cornwallis from the North Carolina in the American Revolution, North and South Carolina in the American Revolution, South Carolinas at the siege of Siege of Yorktown, Battle of Yorktown in Yorktown, Virginia. Their marching route from Newport, Rhode Island through Connecticut, New York State, Pennsylvania, New Jersey and Delaware to the Elkton, Maryland, "Head of Elk" by the along the shores and also partially sailing down the Bay to History of Virginia, Virginia. It is also the subject of a designated National Historic Trail under the National Park Service as the Washington–Rochambeau Revolutionary Route. The Bay would again see conflict during War of 1812. During the year of 1813, from their base on Tangier Island, British naval forces under the command of Admiral George Cockburn raided several towns on the shores of the Chesapeake, treating the Bay as if it were a "British Lake". The Chesapeake Bay Flotilla, a fleet of shallow-draft armed barges under the command of United States Navy, U.S. Navy Commodore Joshua Barney, was assembled to stall British shore raids and attacks. After months of harassment by Barney, the British landed on the west side of the Patuxent at Benedict, Maryland, the Chesapeake Flotilla was scuttled, and the British trekked overland to Battle of Bladensburg, rout the U.S. Army at Bladensburg and Burning of Washington, burn the U.S. Capitol in August 1814. A few days later in a "pincer attack", they also sailed up the to attack Fort Washington (Maryland), Fort Washington below the National Capital and Raid on Alexandria, raided the nearby port town of Alexandria, Virginia. There were so-called "Oyster Wars" in the late 19th and early 20th centuries. Until the mid-20th century, oyster harvesting rivaled the crab industry among Chesapeake watermen, a dwindling breed whose skipjack (boat), skipjacks and other workboats were supplanted by recreational craft in the latter part of the century. In the 1960s, the Calvert Cliffs Nuclear Power Plant on the historic Calvert Cliffs State Park, Calvert Cliffs in Calvert County, Maryland, Calvert County on the Western Shore of Maryland began using water from the Bay to cool its reactor.
NavigationThe Chesapeake Bay forms a link in the Intracoastal Waterway, of the bays, sounds and inlets between the off-shore barrier islands and the coastal mainland along the Atlantic Ocean, Atlantic coast connecting the Chesapeake and Delaware Canal (linking the Bay to the north and the Delaware River) with the Albemarle and Chesapeake Canal (linking the Bay, to the south, via the Elizabeth River (Virginia), Elizabeth River, by the cities of Norfolk, Virginia, Norfolk and Portsmouth, Virginia, Portsmouth to the Albemarle Sound and Pamlico Sound in North Carolina and further to the Sea Islands of Georgia). A busy shipping channel (dredged by the United States Army Corps of Engineers, U.S. Army Corps of Engineers since the 1850s) runs the length of the Bay, is an important transit route for large vessels entering or leaving the Helen Delich Bentley Port of Baltimore, Port of Baltimore, and further north through the Chesapeake and Delaware Canal to the ports of Wilmington, Delaware, Wilmington and Philadelphia, Pennsylvania, Philadelphia on the Delaware River. During the later half of the 19th century and first half of the 20th century, the Bay was plied by passenger steamships and packet boat lines connecting the various cities on it, notably the Baltimore Steam Packet Company ("Old Bay Line"). In the later 20th century, a series of road crossings were built. One, the Chesapeake Bay Bridge (also known as the Governor William Preston Lane, Jr. Memorial Bridge) between the state capital of Annapolis, Maryland and Matapeake, Maryland, Matapeake on the Eastern Shore of Maryland, Eastern Shore, crossing Kent Island, Maryland, Kent Island, was constructed 1949–1952. A second, parallel, span was added in 1973. The Chesapeake Bay Bridge–Tunnel, connecting Eastern Shore of Virginia, Virginia's Eastern Shore with its mainland (at the metropolitan areas of Virginia Beach, Virginia, Virginia Beach, Norfolk, Virginia, Norfolk, Portsmouth, Virginia, Portsmouth, and Chesapeake, Virginia, Chesapeake), is approximately long; it has trestle bridges as well as two stretches of tunnels that allow unimpeded shipping; the bridge is supported by four man-made islands. The Chesapeake Bay BridgeChesapeake Bay Bridge–Tunnel, –Tunnel was opened for two lanes in 1964 and four lanes in 1999.
TidesTides in the Chesapeake Bay exhibit an interesting and unique behavior due to the nature of the topography (both horizontal and vertical shape), wind driven circulation, and how the Bay interacts with oceanic tides. Research into the peculiar behavior of tides both at the northern and southern extents of the Bay began in the late 1970s. One study noted sea level fluctuations at periods of 5 days, driven by sea level changes at the Bay's mouth on the Atlantic coast and local lateral winds, and 2.5 days, caused by resonant oscillations driven by local longitudinal winds, while another study later found that the geometry of the Bay permits for a resonant period of 1.46 days. A good example of how the different Chesapeake Bay sites experience different tides can be seen in the tidal predictions published by the National Oceanographic and Atmospheric Administration (NOAA) (see figure at right). At the Chesapeake Bay Bridge–Tunnel (CBBT) site, which lies at the southernmost point of the Bay where it meets the near Norfolk, Virginia, and the capes of Cape Charles (headland), Charles and Cape Henry, Henry, there is a distinct semi-diurnal tide throughout the lunar month, with small amplitude modulations during spring (new/full moon) vs. neap (one/three quarter moon) tidal periods. The main forcing of the CBBT tides are typical, semi-diurnal ocean tides that the East Coast of the United States experiences. Baltimore, in the northern portion of the Bay, experiences a noticeable modulation to form its mixed tidal nature during spring vs. neap tides. Spring tides, when the sun-earth-moon system forms a line, cause the largest tidal amplitudes during lunar monthly tidal variations. In contrast, neap tides, when the sun-earth-moon system forms a right angle, are muted, and in a semi-diurnal tidal system (such as that seen at the CBBT site) this can be seen as a lowest intertidal range. Two interesting points that arise from comparing these two sites at opposite ends of the Bay are their tidal characteristics - semi-diurnal tide for CBBT and mixed tide for Baltimore (due to resonance in the Bay) - and the differences in amplitude (due to dissipation in the Bay).
Fishing industryThe Bay is mostly known for its seafood production, especially blue crabs, clams, and oysters. In the middle of the 20th century, the Bay supported 9,000 full-time watermen, according to one account. Today, the body of water is less productive than it used to be because of surface runoff, runoff from urban areas (mostly on the Western Shore) and farms (especially on the Maryland Eastern Shore, Eastern Shore and in the Susquehanna River watershed), over-harvesting, and invasive species, invasion of foreign species. The plentiful oyster harvests led to the development of the Skipjack (boat), skipjack, the state boat of Maryland, which is the only remaining working boat type in the United States still under sail power. Other characteristic bay-area workboats include sail-powered boats such as the log canoe, the pungy, the Bugeye (boat), bugeye, and the motorized Chesapeake Bay deadrise, the state boat of Virginia. In contrast to harvesting wild oysters, oyster farming is a growing industry for the Bay to help maintain the estuary's productivity as well as a natural effort for filtering impurities such as nutrient pollution, excess nutrients from the water in an effort to reduce the effects of man-made water pollution, pollution. The Chesapeake Bay Program is using oysters to reduce the amount of nitrogen compounds entering the Chesapeake Bay. Oysters are hermaphroditic and will change gender at least once during their lifetime, often starting as male and ending as female; there are numerous ways to cook and eat them, as well as recipes and sauces to accompany oyster dishes. One account: The Bay is famous for its rockfish, a regional name for striped bass. Once on the verge of extinction, rockfish have made a significant comeback because of legislative action that put a moratorium on rockfishing, which allowed the species to re-populate. Rockfish can now be fished in strictly controlled and limited quantities.
Tourism and recreationThe Chesapeake Bay is a main feature for tourists who visit Maryland and Virginia each year. Fishing, crabbing, swimming, boating, kayaking, and sailing are extremely popular activities enjoyed on the waters of the Chesapeake Bay. As a result, tourism has a notable impact on Maryland's economy. One report suggested that Annapolis was an appealing spot for families, water sports and boating. Commentator Terry Smith spoke about the Bay's beauty: One account suggested how the Chesapeake attracts people: The Chesapeake Bay plays an important role in Maryland, Virginia, and Pennsylvania's economies, in addition to the ecosystem. The nature-based recreation of wildlife, boating, and ecotourism are dependent on the Clean Water Act (CWA), that was enacted in order to maintain a polluted-free Bay. In 2006, "roughly eight million wildlife watchers spent $636 million, $960 million, and $1.4 billion in Maryland, Virginia, and Pennsylvania." -Carrie Grisham, Chesapeake Bay Foundation, 2009
CuisineIn Cuisine of the Thirteen Colonies, colonial times, simple cooking techniques were used to create one pot meals like ham and potato casserole, clam chowder, or stews with common ingredients like oysters, chicken or venison. When John Smith landed in Chesapeake in 1608 he wrote: "The fish were so thick, we attempted to catch them with frying pans". Common regional ingredients in the local cuisine of Chesapeake included terrapins, smoked hams, blue crab, shellfish, local fish, game meats and various species of waterfowl. Blue crab continues to be an especially popular regional specialty.
PollutionIn the 1970s, the Chesapeake Bay was found to contain one of the planet's first identified marine dead zones, where waters were so depleted of oxygen that they were unable to support life, resulting in massive fish kills. Today the Bay's dead zones are estimated to kill 75,000 tons of bottom-dwelling clams and worms each year, weakening the base of the estuary's food chain and robbing the blue crab in particular of a primary food source. Crabs are sometimes observed to amass on shore to escape pockets of oxygen-poor water, a behavior known as a "crab jubilee". Hypoxia (environmental), Hypoxia results in part from large algal blooms, which are nourished by the runoff of residential, farm and industrial wastewater, waste throughout the watershed. One report in 2010 criticized Amish farmers for having cows that "generate heaps of manure that easily washes into streams and flows onward into the Chesapeake Bay". The pollution entering the bay has multiple components that contribute to the algal bloom, principally the nutrients phosphorus and nitrogen. The algae prevents sunlight from reaching the bottom of the Bay while alive and deoxygenates the Bay's water when it dies and rots. Soil erosion and runoff of sediment into the Bay, exacerbated by devegetation, construction and the prevalence of pavement in urban and suburban areas, also blocks vital sunlight. The resulting loss of aquatic plant, aquatic vegetation has depleted the habitat for much of the Bay's animal life. Beds of Zostera, eelgrass, the dominant variety in the southern Chesapeake Bay, have shrunk by more than half there since the early 1970s. Overharvesting, pollution, sedimentation and disease have turned much of the Bay's bottom into a muddy wasteland. One particularly harmful source of toxicity is ''Pfiesteria piscicida'', which can affect both fish and humans. ''Pfiesteria'' caused a small regional panic in the late 1990s when a series of large blooms started killing large numbers of fish while giving swimmers mysterious rashes; nutrient runoff from chicken farms was blamed for the growth. The Bay has improved slightly in terms of the overall health of its ecosystem, earning a rating of 31 out of 100 in 2010, up from 28 in 2008. An estimate in 2006 from a "blue ribbon panel" said cleanup costs would be $15 billion. Compounding the problem is that 100,000 new residents move to the area each year. A report in 2008 in ''The Washington Post'' suggested that government administrators had overstated progress on cleanup efforts as a way to "preserve the flow of federal and state money to the project." In January 2011, there were reports that millions of fish had died, but officials suggested it was probably the result of extremely cold weather.
Depletion of oystersWhile the Bay's salinity is ideal for oysters and the oyster fishery was at one time the Bay's most commercially viable,Oysters: Gem of the Ocean
Restoration effortsEfforts of federal, state and local governments, working in partnership through the Chesapeake Bay Program, an intergovernmental coalition, along with the Chesapeake Bay Foundation and other nonprofit environmental groups, to restore or at least maintain the current water quality, have had mixed results. One particular obstacle to cleaning up the Bay is that much of the polluting substances are discharged far upstream in tributary, tributaries lying within states far removed from the Bay: New York and Pennsylvania. Despite the State of Maryland spending over $100 million to restore the Bay, conditions have continued to grow worse. In the mid-20th century, the Bay supported over 6,000 oystermen. As of 2008 there were fewer than 500. In June 2000, the Chesapeake Bay Program adopted ''Chesapeake 2000,'' an agreement adopted by the member jurisdictions, intended to guide restoration activities throughout the Chesapeake Bay watershed through 2010. One component of this agreement was a series of upgrades to sewage treatment plants throughout the watershed. In 2016 the U.S. Environmental Protection Agency (EPA) stated that the upgrades "have resulted in steep reductions in nitrogen and phosphorus pollution... despite increases in human population and wastewater volume." Restoration efforts that began in the 1990s have continued into the 21st century and show potential for growth of the native oyster population. Efforts to repopulate the Bay using oyster hatcheries have been carried out by a group called the Oyster Recovery Partnership, with some success. In 2011 the group placed 6 million oysters on of the Trent Hall sanctuary.Program turns pork into oysters
Climate changeThe Chesapeake Bay is already experiencing the effects of climate change. Key among these is sea level rise: water levels in the bay have already risen one foot, with a predicted increase of 1.3 to 5.2 feet in the next 100 years. This has related environmental effects, causing changes in marine ecosystems, destruction of coastal marshes and wetlands, and intrusion of saltwater into otherwise brackish parts of the bay. Sea level rise also compounds the effects of extreme weather on the bay, making coastal flooding as part of the events more extreme and increasing runoff from upstream in the watershed. With increases in flooding events and sea level rise, the 11,600 miles of coastline, which include significant historic buildings and modern infrastructure, will be at risk of erosion. Already islands like Holland Island have disappeared due to the rising sea levels. Also, changes in the marine ecosystem due to climate change, such as ocean acidification and temperature increases, will put increasing pressure on marine life—decreasing dissolved oxygen, making it harder for shellfish to maintain shells, and changing the seasonal cycles important for breeding and other lifecycle activities. Seasonal shifts and warmer temperatures also mean that there is a greater likelihood of pathogens to stay active in the ecosystem. Climate change adaptation and mitigation programs in Climate change in Maryland, Maryland and Climate change in Virginia, Virginia often include significant programs to address the communities in the Chesapeake Bay. Key infrastructure in Virginia, such as the port of Norfolk, Virginia, Norfolk, and major agriculture and fishing industries of the Eastern Shore of Maryland will be directly impacted by the changes in the Bay.
Underwater archaeologyUnderwater archaeology is a subfield of archaeology that focuses on the exploration of submerged archaeological sites in seas, rivers, and other bodies of water. In 1988, the Maryland Maritime Archeology Program (MMAP) was established with the goal to manage and explore the various underwater archaeological sites that line the Chesapeake Bay. This was in response to the Abandoned Shipwrecks Act, National Abandoned Shipwreck Act passed in 1987, which gave ownership of historically significant shipwrecks to those states with proper management programs. Water makes up 25% of the State of Maryland and there are over 550 submerged archaeological sites that have been located across the Chesapeake Bay and its surrounding watersheds. Ranging from 12,000 year old, precolonial native settlements to shipwrecks from as recent as World War II, the MMAP researches thousands of years worth of history in these archaeological sites. Susan Langley has been Maryland's State Underwater Archaeologist, one of only nine state appointed underwater archaeologists in the United States, since assuming the role in 1995. Before Langley was hired, only 1% of the underwater archaeological sites in the bay area had been examined. Over the next 10 years, Langley made significant improvements to the MMAP's marine technology, allowing her and her team to explore 34% of the underwater archaeological sites by 2004.
Location and research processesThe Chesapeake Bay watershed has been heavily impacted by natural forces such as erosion, tides, and a history of hurricanes and other storms. Along with environmental factors, the bay has been negatively impacted by humans since being settled in the 17th century, bringing with them problems like pollution, construction, and destruction of the environment. All of these circumstances have made it increasingly difficult for the MMAP to identify potential underwater archaeological sites. As sea levels rise and historically significant areas are sunk and covered in sediment, the MMAP relies on various pieces of equipment to locate these man-made anomalies but also ensure that the material being examined is kept intact. Using marine magnetometers(detects iron/absent space), side-scan sonar,(detects objects on sea floor), along with precise global positioning systems, Langley and the MMAP have been much more successful in locating submerged archaeological sites. After locating the site, Langley and her team have a strict process in order to preserve the site and its contents, allowing more accurate and thorough research to be conducted. The remains of nearly every site have been submerged in saltwater for sometimes centuries, the integrity of shipwrecks and other materials are fragile and careful precaution must be used when working with them. Taking photos and videos, creating maps, and constructing models are all a part of the process of preserving remains. Susan Langley notes herself, “If you have only ten percent of a ship’s hull, you can reconstruct the ship. Construction techniques can tell us about the people who built the vessels, artifacts can tell us about the people who profited from the ship’s trade, and eco-facts—evidence of insect infestation and organic remains, such as seeds, that are preserved in anaerobic, muddy environments—can tell us about the climate and season when a ship sank." Still, the MMAP makes it a point to publish their data and information once a site is officially identified, however the details of the location are left out to sway would be looters, who have plagued marine archaeologists for decades.
Significant sitesAltogether there are more than 1,800 ship and boat wrecks that scatter the bottom of the Chesapeake Bay and its surrounding waterways. Dozens of precolonial era canoes and artifacts have been extracted from the bay, helping to portray a better picture of the lives of Native Americans (e.g., Powhatan, Pamunkey, Nansemond) In 2014, underwater archaeologists identified the skull of a prehistoric mastodon, which through carbon dating was found to be 22,000 years old. Along with the skull, a carved blade was also discovered in the same area. Unable to accurately carbon date the stone tool, archaeologists looked at similar styles of blade carving in order to gauge when it was made. The technique was similar to the Solutrean tools that were crafted in Europe between 22,000 and 17,000 years ago and it was noted that the stone tool must be at least 14,000 years old. This challenges the previous theory regarding the first inhabitants of North America, where as its commonly accepted amongst anthropologists that the Clovis culture, Clovis people were the first to settle the region somewhere around 13,000 years ago. There is some controversy surrounding these findings, many anthropologists have disputed, this claiming that the environment and setting makes properly identifying the origins of these artifacts nearly impossible. The Chesapeake Bay Flotilla , which was constructed using shallow barges and ships to provide a blockade to the British during the War of 1812. After holding strong for some months, the British eventually dispersed the flotilla and dozens of these vessels were burnt and sunk. Starting in 1978, there were numerous expeditions launched in hopes of successfully discovering what was left of the Chesapeake Bay Flotilla. Since then, hundreds of artifacts and remains have been extracted from the submerged ships such as weapons, personal items, and many other objects. Underwater archaeologists have also been successful in constructing accurate models and maps of the wreckage amongst the sea floor. In October 1774, a British merchant ship arrived at the port of Annapolis, Maryland, Annapolis loaded with tea disguised as linens and garments. The tea was hidden by the British to avoid conflict with the colonists as the recently imposed tea tax had created hostility and uncertainty among the colonies. Named ''Peggy Stewart (ship), Peggy Stewart,'' the British vessel arrived and attempted to tax the colonists for the purchased tea. The colonists refused to pay the tax and after a few days of public meetings, the colonists decided to burn ''Peggy Stewart'' and the contents of it. The British ship was sunk in what became known as the 'Annapolis Tea Party' and has since become an important site for underwater archaeologists in the Chesapeake Bay. In 1949, after the Nazi's defeat in World War 2, the United States seized a German submarine U-1105, German U-1105 built with sonar-evading rubber sheathing for study purposes. It was sunk the same year in the Potomac River off of the Chesapeake Bay following a high explosives test hosted by the U.S. Navy and has since been a popular site for underwater archaeologists. Maryland has controlled the majority of underwater archaeology research around the Chesapeake Bay, however Virginia's Department of Historic Resources have had a State Underwater Archaeologist since the 1970s. In 1982, the Virginia Department of Historic Resources along with the first State Underwater Archaeologist, John Broadwater, led an expedition to explore and research a sunken fleet of Revolution-era battleships. In September 1781, during the Revolutionary War, the British intentionally sunk more than a dozen ships in the York River (Virginia), York River, near the mouth of the Chesapeake Bay. Led by Charles Cornwallis, 1st Marquess Cornwallis, Lord Charles Cornwallis, a fleet of British ships was pushed back towards the rivers of the Chesapeake, in a desperate attempt to avoid surrendering, Cornwallis began burning and sinking his own vessels with the hopes of stalling the incoming French and American ships. Cornwallis was eventually forced to surrender on October 19 and the ships along with its contents were at the bottom of the York River. One of the British ships, called Betsy, has been explored more than any other and over 5,000 relics were removed from Betsy on their original expedition in 1982, including weapons, personal objects, and some valuable metals. Broadwater and his team were awarded a 20-page article in the magazine ''National Geographic'' for their findings. Virginia has recently been granted funding for further research of these sunken vessels and expeditions are currently underway with the goal to fully explore this destroyed fleet of British ships. Unfortunately, following the publicity of these sunken ships, many divers have taken it upon themselves to explore the wreckage for 'treasure'.
PublicationsThere are several magazines and publications that cover topics directly related to the Chesapeake Bay and life and tourism within the Bay region. ''The Capital'', a newspaper based in Annapolis, reports about news pertaining to the Western Shore of Maryland and the Annapolis area. ''Chesapeake Bay Magazine'' and ''PropTalk'' focus on powerboating, while ''SpinSheet'' focuses on sailing. What's Up Magazine is a free monthly publication with special issues focused on Annapolis and the Eastern Shore. Bay Weekly is the Chesapeake Bay region's independent newspaper.https://bayweekly.com/
In literature* ''Beautiful Swimmers: Watermen, Crabs and the Chesapeake Bay'' (1976) is a Pulitzer Prize-winning non-fiction book by William W. Warner about the Chesapeake Bay, blue crabs, and watermen. * ''Chesapeake (novel), Chesapeake'', a 1978 novel by author James A. Michener. * John Barth wrote two novels featuring Chesapeake Bay; ''Sabbatical: A Romance'' (1982) centered on a yacht race through the Bay, and ''The Tidewater Tales'' (1987) detailed a married couple telling stories to each other as they cruise the Bay. * ''Jacob Have I Loved'' (1980) by Katherine Paterson, winner of the 1981 Newbery Medal. This is a novel about the relationship between two sisters in a waterman family who grow up on an island in the Bay. * In Tom Clancy's 1987 book ''Patriot Games'', the main protagonist Jack Ryan lives on the fictional Peregrine Cliffs, which overlook the Chesapeake Bay. * In Clancy's 1993 book, ''Without Remorse'', the protagonist John Kelly (later known as John Clark (Tom Clancy character), John Clark when he goes to work for the Central Intelligence Agency, CIA), lives on a boat and an island on the Bay. * Class conflict between waterman people and wealthy newcomers was portrayed in Priscilla Cummings's novel ''Red Kayak''. * Cynthia Voigt's Tillerman series, starting with Dicey's Song, are set in Crisfield on the Chesapeake Bay.
In film* ''The Bay (film), The Bay'', a 2012 found footage (pseudo-documentary), found footage-style eco-horror movie about a pandemic due to deadly pollution from chicken factory farm run-off and mutant isopods and aquatic parasites able to infect humans.
Other mediaSinger and songwriter Tom Wisner recorded several albums, often about the Chesapeake Bay. ''The Boston Globe'' wrote that Wisner "always tried to capture the voice of the water and the sky, of the rocks and the trees, of the fish and the birds, of the gods of nature he believed still watched over it all." He was known as the ''Bard of the Chesapeake Bay.'' The 1976 hit "Moonlight Feels Right" by Starbuck (band), Starbuck refers to the Chesapeake Bay: "I'll take you on a trip beside the ocean / And drop the top at Chesapeake Bay."
See also* Chesapeake Bay Interpretive Buoy System * Chesapeake Bay Retriever * Chesapeake Climate Action Network * Chesepian * Coastal and Estuarine Research Federation * Great Ireland * List of islands in Maryland (with the islands in the Bay) * National Estuarine Research Reserve * Old Bay Seasoning
Further reading* Cleaves, E.T. et al. (2006). ''Quaternary geologic map of the Chesapeake Bay 4º x 6º quadrangle, United States'' [Miscellaneous Investigations Series; Map I-1420 (NJ-18)]. Reston, VA: U.S. Department of the Interior, U.S. Geological Survey.