The geomorphologic forms in Florida result mainly from erosion and sedimentation. These are complementary processes in which materials such as rock, coral, soil, sand, and bottom sediment are worn away, removed from one area of the Earth's surface, and deposited in another area. Materials are often carried long distances by ocean or other aquatic currents before being deposited.
Also around 100,000 years ago, several parallel lines of patch reef formed along the shoreline of southern Florida. At that time, the sea level was about 8 m (about 25 ft) higher than it is today. As glaciers formed during the Ice Age, much of the ocean's water was withdrawn from the ocean basins. As the sea level fell, water drained off the patch reefs and barrier reef, exposing the coral to erosion. Erosion removed the top 17 meters (about 50 ft) of the barrier reef. The patch reef closest to the Everglades shoreline remained and became what is now known as the upper Florida Keys.
When the Earth's temperature rose and the glaciers began to melt, sea levels rose. When the water reached the level of the old reefs, a new barrier reef began to grow at the seaward edge, and patch reefs grew back between the barrier reef and the shoreline. Limestone sediment that had eroded from the reefs began to move to the south, covering the coral growing there and forming mounds of hard Miami limestone, now known as the Lower Keys.
The formation and melting of glaciers also shaped Florida Bay. Before the Pleistocene era, Florida Bay was a lagoon between the living coral reef and the mainland. Limestone that had eroded from the reef and was suspended in the water eventually covered the floor of the lagoon. When glaciation occurred, the sea level fell 33 meters (about 100 ft). The bay became eroded and the limestone hardened, forming Miami limestone. When the glaciers melted, the lagoon filled up with freshwater and looked similar to the Everglades. As the climate continued to warm up, sea levels rose. The sea reached its maximum level 4,000 years ago, flooding the lagoon and producing Florida Bay.
To prevent these disruptions, the United States government proposed that at least 17 miles of bridges be included in the railway to allow for tidal flow between the ocean and Florida Bay. Although these bridges were part of the final design, the railway still harmed the natural environment of the Florida Keys. The causeways buried thousands of acres of grass beds found in the shallow waters between the Keys. Hundreds of acres of mangrove forests were filled to make a firm roadbed. Sedimentation was widespread, because the bottom was churned and disturbed by filling, dredging, and bridge construction. Because the tidal flow was blocked in some areas, the flow doubled in open areas. The rapid currents that resulted changed the life on the bottom. Channels that were once deep became shallow through sedimentation. Seagrass beds and calcareous (calcium-containing) algae grew and changed the habitats of organisms living in the channels.
In 1935, a hurricane destroyed most of the railway. Between 1936 and 1944, an overseas highway was built to replace the railway. The highway used more bridges and fewer causeways than the railway did, and the highway builders used railway bridges that remained standing rather than constructing new ones. For these reasons, the impact of highway construction on the Keys was limited, some tidal flow was restored, and the Keys ecosystem recovered to some extent.
Direct observation is also critical. Scientists can directly observe geomorphologic forms using a wide range of technologies:
During JASON VII, Dr. Ballard and his team of engineer-researchers
will use these tools to look at marine geomorphologic features, such as
Pourtales Terrace and a shelf in the Straits of Florida maintained by the
constant movement of sediment in the Gulf Stream. He will also
explore ancient coral reefs 73 to 183 meters (240 to 600 ft) below the
surface, located 29 kilometers (18 mi) south of the Florida Keys. One of
these reefs, known as "the hump"-a pre-Pleistocene reef located on
Pourtales Terrace-has never been explored before!
The Florida Bay research team headed by Dr. John Hunt also will investigate marine communities. This team will examine the geomorphologic forms of the hard-bottom shoals and lakes in Florida Bay and the soft-bottom mud banks that join at irregular intervals to create a lace-like pattern around the lakes.
JASON VII Home Page
JASON Project Homepage
Gene Carl Feldman
Todd Carlo Viola, JASON Foundation for Education (firstname.lastname@example.org)
Revised: 26 April 1996