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The Key West Historic District (also known as Old Town of the City of Key West) is a U.S. historic district (designated as such on March 11, 1971) located in Key West, Florida. It encompasses approximately 4,000 acres (16 km 2 ), bounded by White, Angela, Windsor, Passover, Thomas and Whitehead Streets, and the Gulf of Mexico .
Pages in category "Tourist attractions in Key West, Florida" The following 27 pages are in this category, out of 27 total. This list may not reflect recent changes .
Key West is closer to Havana (about 106 miles or 171 kilometers by air or sea) [8] than it is to Miami (130 miles or 210 kilometers by air or 165 miles or 266 kilometers by road). [7] Key West is the usual endpoint for marathon swims from Cuba, including Diana Nyad's 2013 swim [33] [34] and Susie Maroney's 1997 swim from within a shark cage. [35]
Pages in category "National Register of Historic Places in Key West, Florida" The following 18 pages are in this category, out of 18 total. This list may not reflect recent changes .
The Custom House currently serves as the Key West Museum of Art & History, which is one of four museums operated by the Key West Art & Historical Society. Exhibits include local history, famous personalities including Ernest Hemingway , maritime history, and works by local artists.
Sigsbee Park, also known as Dredgers Key, is an island about half a mile (800 m) north of Key West island in the lower Florida Keys; administratively it is within the City of Key West, Florida, United States. [1] It is connected to the island of Key West by Sigsbee Road. The island and causeway are part of the Key West Naval Air Station. It is ...
Following Spain's secession of Florida to the United States in 1819, the first permanent colonization of Key West began with American possession in 1821. [6] Legal claim of the island occurred with the purchase by businessman, John W. Simonton, in 1822, in which federal property was asserted only three months later with the arrival of U.S. Navy Lieutenant Mathew C. Perry.
The limestone that eroded from the reef formed oolites in the shallow sea behind the reef, and together with the skeletal remains of bryozoans, formed the Miami Limestone that is the current surface bedrock of the lower Florida peninsula and the lower keys from Big Pine Key to Key West. To the west of Key West the ancient reef is covered by ...
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