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  2. Marquesas Keys - Wikipedia

    en.wikipedia.org/wiki/Marquesas_Keys

    The Marquesas Keys form an uninhabited island group about 20 miles (32 km) west of Key West, four miles (6 km) in diameter, and largely covered by mangrove forest. They are an unincorporated area of Monroe County, Florida and belong to the Lower Keys Census County Division. [1] They are protected as part of the Key West National Wildlife Refuge ...

  3. Key West - Wikipedia

    en.wikipedia.org/wiki/Key_West

    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]

  4. Fishing Boats, Key West - Wikipedia

    en.wikipedia.org/wiki/Fishing_Boats,_Key_West

    Fishing Boats, Key West is a 1903 watercolor and graphite drawing by the American artist Winslow Homer. It is in the collection of the Metropolitan Museum of Art. [1]

  5. Hawk Channel - Wikipedia

    en.wikipedia.org/wiki/Hawk_Channel

    View of Hawk Channel from Marathon or Islamorada at sunset. Hawk Channel is a shallow, elongated basin and navigable passage along the Atlantic coast of the Florida Keys.The channel makes up a smaller portion of the Florida Platform from Key West to the southernmost point of Key Biscayne and lies between the Keys and the Florida Reef Tract to the southeast. [1]

  6. History of Key West - Wikipedia

    en.wikipedia.org/wiki/History_of_Key_West

    Fishermen surround captured sea turtles in Key West, c., 1900. The fishing industry was the center of Key West's economy throughout the island's history. [86] Throughout much of the 19th and 20th centuries, Key West supplied eighty percent of all turtle products in the United States. [87]

  7. Florida Keys - Wikipedia

    en.wikipedia.org/wiki/Florida_Keys

    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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