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The Chesapeake Bay impact crater is a buried impact crater, located beneath the mouth of Chesapeake Bay, United States. It was formed by a bolide that struck the eastern shore of North America about 35.5 ± 0.3 million years ago, in the late Eocene epoch. It is one of the best-preserved "wet-target" impact craters in the world. [3]
Map of Tangier and its surrounding islands. Tangier Island is located in the Chesapeake Bay in Accomack County, Virginia. The island is composed of three sandy ridges divided by marshes and tidal streams. These three ridges, called West Ridge, Main Ridge, and Canton Ridge from west to east, run parallel north-to-south. [21]
The Chesapeake Ranch Estates (CRE), also known locally as the Ranch Club, is located in Lusby, Maryland, United States, in southern Calvert County. CRE was founded in 1958 and is governed by a homeowners' association , which is officially called the "Property Owner's Association of the Chesapeake Ranch Estates" (POACRE).
The Chesapeake Bay Bridge, connecting the eastern and western shores of Maryland was completed in 1952. Length of the suspension span is 2,922 feet and the roadway is about 200 feet above water at ...
Gibson Island's gated causeway. The Chesapeake Bay Bridge is visible in the background. Gibson Island is an island and unincorporated community on the western shore of the Chesapeake Bay. It is part of Anne Arundel County, Maryland, United States and is the eastern terminus of Maryland Route 177. It is connected by a causeway to Pasadena, Maryland.
The Chesapeake Bay watershed. The entire Chesapeake Bay watershed includes portions of six states (New York, Pennsylvania, West Virginia, Maryland, Virginia, and Delaware) and the District of Columbia. The watershed of the entire Chesapeake Bay covers 165,760 km 2 (approximately 64,000 mi 2 or 41 million acres [3] [4]).
Poplar Island is a 3-mile-long (4.8-kilometer-long) island located on the Chesapeake Bay, part of Talbot County, Maryland. In the late 1800s it had a population of 100 living in the town of Valliant but it was abandoned by the 1920s due to erosion of the island. By the 1990s its land mass had dwindled down to a few acres.
If the team can determine the site is a crater formed by an ancient impact event, then the next step is researching just when it happened. Of the world’s roughly 200 impact craters, 31 are ...