Geography of Florida

Source: Wikipedia, the free encyclopedia.
A map of Florida, as seen from outer space.

Much of the state of Florida is situated on a peninsula between the Gulf of Mexico, the Atlantic Ocean, and the Straits of Florida. Spanning two time zones, it extends to the northwest into a panhandle along the northern Gulf of Mexico. It is bordered on the north by the states of Georgia and Alabama, on the west, at the end of the panhandle, by Alabama. It is near The Bahamas, and several Caribbean countries, particularly Cuba. Florida has 131 public airports, and more than 700 private airports, airstrips, heliports, and seaplane bases.[1] Florida is one of the largest states east of the Mississippi River, and only Alaska and Michigan are larger in water area.

Physiogeography

Florida has three distinct physiographic provinces: Gulf Coastal Lowlands, Atlantic Coastal Lowlands, and Interior Highlands. The coastal lowlands rim the entirety of the peninsula and panhandle from the shoreline to 30 to 50 miles (48 to 80 km) inland, merging with the Interior Highland.[2]

Terrain

The beach at Bahia Honda in the Florida Keys, and Crandon Park in Key Biscayne.

At 345 feet (105 m)

Gulf Coast, and up through the Everglades, endangering the plant biomass within its marsh communities.[7]

A 2014 study found Florida to be the flattest state.[8]

Boundaries

The state line begins in the Atlantic Ocean, traveling west, south, and north up the

Flint River (from Georgia) and the Chattahoochee River (down the Alabama/Georgia line) used to form Florida's Apalachicola River. (Since Woodruff Dam was built, this point has been under Lake Seminole.) The border with Georgia continues north through the lake for a short distance up the former thalweg of the Chattahoochee, then with Alabama runs due west along 31°N to the Perdido River, then south along its thalweg to the Gulf via Perdido Bay. Much of the state is at or near sea level
. Florida is also 65,755 square miles.

Topography

Topographic map of Florida

Geology

The Florida peninsula is a porous plateau of karst limestone sitting atop bedrock known as the Florida Platform. The emergent portion of the platform was created during the Eocene to Oligocene as the Gulf Trough filled with silts, clays, and sands. Flora and fauna began appearing during the Miocene. No land animals were present in Florida prior to the Miocene.

The largest deposits of

phosphate rock in the country are found in Florida.[9]

Extended systems of underwater caves,

last glacial period, lower sea levels and a drier climate revealed a much wider peninsula, largely savanna.[10] The Everglades
, a wide, slow-flowing river, encompasses the southern tip of the peninsula.

While there are sinkholes in much of the state, modern sinkholes have tended to be in West-Central Florida.[11][12]

Florida is tied for last place (with North Dakota) as having the fewest earthquakes of any US state.

Key West, Florida. (See List of earthquakes in Cuba) Another earthquake centered outside Florida was the 1886 Charleston earthquake. The shock was felt throughout northern Florida, ringing church bells at St. Augustine and severely jolting other towns along that section of Florida's east coast. Jacksonville residents felt many of the strong aftershocks that occurred in September, October, and November 1886.[14] As recently as 2006, a magnitude 6.0 earthquake centered about 260 miles (420 km) southwest of Tampa in the Gulf of Mexico sent shock waves through southwest and central Florida. The earthquake was too small to trigger a tsunami and no damage was reported.[15]

Climate