Search results
Results From The WOW.Com Content Network
Coffins Patch is a shallow coral reef (patch reef) located within the Florida Keys National Marine Sanctuary. It lies to the southeast of Bamboo Key . This reef lies within a Sanctuary Preservation Area (SPA).
Looe Key is a coral reef located within the Florida Keys National Marine Sanctuary. It lies to the south of Big Pine Key. This reef is within a Sanctuary Preservation Area (SPA). Part of Looe Key is designated as "Research Only," an area which protects some of the patch reefs landward of the main reef.
Cheeca Rocks is a shallow coral reef (patch reef) located within the Florida Keys National Marine Sanctuary. It lies approximately one mile to the southeast of Upper Matecumbe Key . This reef lies within a Sanctuary Preservation Area (SPA).
The Florida Keys National Marine Sanctuary is a U.S. National Marine Sanctuary in the Florida Keys. It includes the Florida Reef, the only barrier coral reef in North America [1] and the third-largest coral barrier reef in the world. It also has extensive mangrove forest and seagrass fields. The Florida Keys National Marine Sanctuary ...
Second is the patch reef community. Patch reefs form in shallow water (three to six meters deep), some in Hawk Channel and some on the outer reef, but mainly on White Bank between Hawk Channel and the outer reefs. Patch reefs start from corals growing on a hard bottom, but grow upward as new corals establish themselves on the skeletons of dead ...
Florida’s once-vibrant coral reefs are losing their color because of record-high ocean temperatures, but scientists and volunteers were working around the clock to save them.
These reefs all lie within the Florida Keys National Marine Sanctuary. Pages in category "Coral reefs of the Florida Keys" The following 32 pages are in this category, out of 32 total.
The Dry Tortugas are the western extension of an arcuate chain of Pleistocene reef and oolitic limestone islands, with the eastern limit in the vicinity of Miami. These Florida Keys are the surface expression of the 3.7 mi (6.0 km) thick southern Florida carbonate platform, which has been accumulating sediments since the Early Cretaceous.