Everything about Key Largo totally explained
Key Largo is an island in the upper
Florida Keys archipelago and, at long, the largest of the Keys. It is also the northernmost of the Florida Keys in
Monroe County, and the northernmost of the Keys connected by
U.S. Highway 1 (the
Overseas Highway). Its earlier Spanish name was
Cayo Largo, meaning
Long Key.
Key Largo is connected to the mainland in
Miami-Dade County by two routes. The Overseas Highway, which is
U.S. Highway 1, enters Key Largo at Jewfish Creek near the middle of the island and turns southwest. Card Sound Road connects to the northern part of Key Largo at
Card Sound Bridge and runs eastward to connect with County Road 905, which runs southwest and joins U.S. 1 at about mile marker 106. These routes originate at
Florida City on the mainland.
Key Largo is a popular tourist destination and calls itself the "Diving Capital of the World" because the living coral reef a few miles offshore attracts thousands of
scuba divers and
sport-fishing enthusiasts. Key Largo's proximity to the
Everglades also makes it a premier destination for
kayakers and
ecotourists. Automotive and highway pioneer and
Miami Beach developer
Carl G. Fisher built Key Largo's famous
Caribbean Club in 1938 as his last project.
The island gained fame as the setting for the 1948
Humphrey Bogart-
Lauren Bacall film
Key Largo, although it was filmed entirely on a
Warner Brothers sound stage in Hollywood. The island's main village, which had been known as Rock Harbor after a nearby cove, changed its name to Key Largo after the film's success.
There are three
census-designated places on the island of Key Largo: North Key Largo, near the Card sound Bridge, Key Largo, eight or nine miles from the southern end of the island, and
Tavernier, at the southern end of the island.
Ocean Reef Club is a private
gated community and club at the northern end of the island. None of Key Largo is an incorporated municipality, so it's governed at the local level by
Monroe County.
Key Largo is situated between
Everglades National Park to the north-west and
John Pennekamp Coral Reef State Park to the east, the first
underwater park in the United States and the site of the only living coral barrier reef in the continental United States.
Geology and geography
The island of Key Largo is an exposed, fossilized remnant of a
coral reef that was formed during a period of higher sea level and then uncovered and eroded during a subsequent
ice age. The highest elevation is a slight ridge forming the spine of the island, which rises to as high as about 15 feet. The land slopes from the spine down to sea level on the oceanside and bayside.
The island's
substrate is called Key Largo
Limestone; in many places,
fossilized corals and smooth, eroded limestone "caprock" are visible at the surface. Solution holes, which are pockets dissolved in the limestone by acidic rainwater, form shallow depressions in the land.
The natural shoreline of the island is generally rocky. A slippery, gray, limestone-based clay called "
marl" is the shoreline and near-shore soil. There are no natural sand beaches on the island.
Inland, decomposed vegetation forms a rich, acidic humus soil up to about six inches thick, topped by "leaf litter." The soil supports a diverse flora of herbaceous plants and woody shrubs and hardwood trees.
Key Largo's climate is considered tropical. Frost has never been recorded in the island.
Further Information
Get more info on 'Key Largo'.
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