The Chesapeake Bay, one of the largest estuaries in the world, is a rich protein resource of oysters, clams, crabs, and fish. "Chesapeake" may have meant "Great Water," or may have referred to an individual Native American town. The long-standing tradition that "Chesapeake" meant "great shellfish bay" is not supported by the research of Blair Rudes, a linguist who re-studied the Algonquian language for a Hollywood movie, The New World - but the bay was still an extraordinary source of food.
In 1608, John Smith discovered a bay so rich in fish that his men tried catching them with frying pans:2
For Native American societies that hunted and gathered food after the harvest in the Fall, access to the bay was important. It is not surprising that on his 1608 voyage up the bay and some major tributaries, John Smith saw Native American towns surrounded by pallisades of tree trunks. The competition between tribes was not always peaceful; the protein resources of the bay were worth a fight. Despite having a river filled with seafood at the edge of their fort, the freshly-arrived English managed to starve to death in Jamestown. Later colonial Virginians made far better use of the protein in the bay. George Washington, for example, made a good profit from having his slaves seine herring in the Potomac River off the shores of Mount Vernon. He would preserve the fish in barrels with salt and sell them as food that could be carried back to Europe - or sold for the slaves in the Caribbean Islands, where most of the land was dedicated to growing sugar cane and food was imported (including much pork from Norfolk).3 The Chesapeake Bay is an "estuary" where fresh and salt water mingle together, creating a special environment that is highly productive biologically. Marine fish, species who can live in brackish water (with salinity between , and freshwater species both take advantage of the estuary. In addition, numerous plant and animal species have specialized over the centuries to thrive in the brackish water. Salinity is the key difference between a fresh water lake/river, an estuary, and the ocean. In the Chesapeake Bay, the range of salinity varies from 35 parts per thousand at the mouth of the Bay (the saltiness of the Atlantic Ocean) to 0-.5 parts per thousand for several miles below the Fall Line. Except in droughts when river flow is diminished, freshwater can extend on the surface of the Potomac River down to Mason Neck.4 Biological productivity as well as biodiversity is high in the Chesapeake Bay. Photosynthesis in an acre of Chesapeake Bay salt marsh can easily surpass the productivity of any Virginia farm in the Shenandoah Valley.5 Humans prefer to eat corn on the cob rather than marsh grasses, of course, so few of us normally think of salt water marshes as more valuable than corn fields. We may be picky eaters, but the decaying grasses are a great food source for the tiny zooplanton in the water that we can only see with a microscope. The decaying grasses provide the organic material at the base of the "detritus" food pyramid. Big fish eat little fish, little fish eat invetebrates, and invertebrates eat detritus - decomposing plant material with microorganisms connsuming the vegetation. The submerged grasses create especially valuable habitat - and are sensitive to pollution. The zooplankton, snails, small fish, birds, and larger fish that feed on each other in a hierarchy of life (and death) won't be there if the grasses disappear.6 The biological productivity of the bay was enhanced by the shape of the waterbody. The Chesapeake Bay is the largest of the 130 estuaries in the United States, and second only in North America to the Gulf of St. Lawrence in Canada. The Chesapeake Bay is about 200 miles long - and very shallow, averaging only 21 feet in depth (when including the tidal portion of its tributaries). There's an extraordinary amount - over 11,600 miles - of shoreline, more than the Pacific Ocean shoreline on the entire West Coast of the United States from Canada to Mexico.7 |
The vast amount of life in the bay was triggered in part by that large amount of ecological "edge" where the land meets the sea, plus the ability of sunlight to reach the bottom across much of the shallow bay. The depths at which submerged aquatic vegetation (SAV) will grow in the tidal waters of Virginia and Maryland is limited by wave action in the shallow end (the roots can't hold the plants in one place, if the water is sloshing around with too much energy) and by light penetration in the deep end (the deeper the water, the less light at the bottom). Submerged aquatic vegetation provided food and shelter for microscopic zooplankton, blue crabs, and other wildlife while oysters grew in such quantity that their old shells piled up into bars that obstructed navigation.
The Chesapeake Bay is a recent feature in the Virginia landscape. When the glaciers started to melt faster than they grew at the end of the last ice age 18,000 years ago, the volume of liquid water on earth increased significantly. Rising sea levels flooded first the continental shelf, and then the river valleys of the Susquehanna and James rivers. As the last ice sheet retreated, ocean currents brought sediments from the Delaware River south, extending the length of the Eastern Shore and blocking the direct path of the Susquehanna River.
The Chesapeake Bay did not exist until about 12,000 years ago, when the rising Atlantic Ocean finally covered the Continental Shelf and began to drown the separate channels of the Susquehanna and James river valleys.8 The bay grew from south to north for 9,000 years, as the sea level increased. About 3,000 years ago, the Chesapeake Bay finally looked like what we see today. The existing size and shape of the Chesapeake Bay has been altered only slightly by natural forces in the last 3,000 years.9
Native Americans have been in Virginia for 10,000-15,000 years, so humans saw the Virginia shoreline change dramatically. The first Virginia immigrants had to move up the hillsides, as the landscape evolved and the Chesapeake Bay developed. Current residents of Tangier Island face the same challenge, as sea levels continue to rise. News articles in Virginia media regularly highlight the challenge faced by the remaining 500 residents of that island, which is predicted to become an underwater sandbar rather than an inhabited island within the next 50-100 years.10
Modern scorecards to measure the bay's health have to use a baseline to define "healthy." Many references to "Save the Bay" initiatives are based on the assumption that the bay was healthy in 1600, so that is an appropriate base line for assessing restoration to the historic condition.
The biological conditions of the bay have changed far more than the geological setting in the last four centuries. The stocks of seafood could recover easily from the minor impacts of Native American/early colonial harvests, but the impacts of modern fishing, clamming, oystering, and crab harvests in the last century have reduced populations dramatically. New species have been introduced, and the balance between species has been altered. The physical conditions of the sediments and water in the bay have been changed forever, and 17 million people living in the watershed continue to contribute various forms of pollution every day.
Though restoration efforts for oysters and other species are underway, the bay will never return to its original condition. The states and District of Columbia failed to reduce pollution sufficiently to meet the minimum standards of the Clean Water Act, despite 25 years of synchronized promises dating back to the 1983 Chesapeake Bay Agreement (which was signed on the George Mason University Fairfax campus).
In May 2009, President Obama issued the Chesapeake Bay Protection and Restoration Executive Order defining a leadership role for the Federal government, and in 2010 a Federal ordered the Environmental Protection Agency to complete a Total Maximum Daily Load (TMDL) study and establish pollution limits. The estimated cost for Virginia to comply with the TMDL limits by 2025 is $25 billion.11
Chesapeake Geology and Sea Level RiseChesapeake Bay: Avenue for AttackWhere is "Tidewater" in Virginia?Will Norfolk (and the Rest of Hampton Roads) Drown?Save the Bay |