Maryland's Geologic Features

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Sunset on the Tred Avon River, Talbot County

contact: Dale Shelton (dshelton@mgs.md.gov)
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Sunset on the Tred Avon River
Photo by Bob Conkwright (July, 1964)

 

Evening falls on the Tred Avon River, a tributary in the Choptank River basin, on the eastern shore of the Chesapeake Bay. The Bay and the lower reaches of its tributaries are drowned river valleys. As the ice sheets of the last ice age continue to melt, sea level rises, flooding coastal rivers to create estuaries. Estuaries are essential habitats for both aquatic and land plants and animals. They are also important commercial and recreational resources. Careful resource management of the Bay and the land surrounding tidewater Maryland is critical to preserve these habitats.

here are many web sites featuring the Chesapeake Bay. Maryland Geological Survey's Coastal and Estuarine Geology Program maintains a site describing MGS's research on the Bay and coast. Other sites include the Chesapeake Bay Home Page, the Chesapeake Bay Foundation, the Chesapeake Bay Program, and EPA's Chesapeake Bay web pages.

Highly colored sunrises and sunsets are caused by atmospheric dust. A significant source of dust is volcanic eruptions.


 
Compiled by the Maryland Geological Survey, 2300 St. Paul Street, Baltimore, MD 21218
This web page was prepared by Bob Conkwright, Division of Coastal and Estuarine Geology, Maryland Geological Survey.
Please send comments on this page to Dale Shelton (dshelton@mgs.md.gov)
Maryland Geological Survey is a part of the Resource Assessment Service
Maryland Department of Natural Resources, State of Maryland
Updated February 13, 2007
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