Environment
Natural Ecology


The Chesapeake Bay is comprised not only of the tidal waters in the Bay itself, but of all the waters flowing into the Bay from throughout the 64,000 square miles of the watershed. That watershed extends from and includes the salt water of the Atlantic Ocean entering from the south, to the fresh rainwater falling as far north as Cooperstown, New York where the Susquehanna begins; from Chester River headwaters in Delaware on the eastern shore, to the Alleghenies in Virginia and West Virginia.

Before European settlers began to arrive here some 400 years ago, the lands of the Chesapeake Bay watershed were largely in a natural state. Forest covered 95 percent of the land. Wetlands covered over 3.5 million acres and underwater grasses are estimated to have covered 600,000 acres.

These resources - forest, wetland, underwater grasses -serve to regulate the flow of rainfall running off the land and to filter the contaminants out of it as it moves into and through the streams and rivers to the Chesapeake Bay. Well-managed farmland can also function as a natural filter.

When development converts these resource lands to roads, buildings, even lawns, their ability to filter runoff is reduced while, at the same time, the rate and volume of runoff increases.

There are many technical methods for handling contaminated runoff; however, the most cost-effective and least disruptive is to preserve, maintain, and restore natural lands, particularly those closest to the water's edge.