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As recently as 2006, a magnitude 6.0 earthquake centered about 260 miles (420 km) southwest of Tampa and west of Fort Myers 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. Minor shaking was felt in Southwest Florida.
Some use the term "transform fault" to describe the seismically and tectonically active portion of a fracture zone after John Tuzo Wilson's concepts first developed with respect to the Mid-Atlantic Ridge. [2] The term fracture zone has a distinct geological meaning, but it is also used more loosely in the naming of some oceanic features.
At 345 feet (105 m) above mean sea level, Britton Hill in northern Walton County is the highest point in Florida and the lowest known highpoint of any U.S. state. [3] Much of the state south of Orlando is low-lying and fairly level; however, some places, such as Clearwater, feature vistas that rise 50 to 100 feet (15 to 30 m) above the water.
A few times each decade Miami might see a winter nightfall below 45°F. El Niño winters tend to be cooler due to increased cloud cover, but tend to have fewer freezes. [12] Five hardiness zones exist. USDA Zone 12A, the warmest zone found within the state, with average extreme annual lows between 50°F to 55°F, is found in the Dry Tortugas area.
The presumed seismically and tectonically active portion of this fracture zone is known as the Heirtzler transform fault and divides a portion of the Pacific-Antarctic Ridge where spreading rates increase towards its axial north from 56 to 66 mm (2.2 to 2.6 in)/year over a distance of 650 km (400 mi). [3]
At first, the hot, faulted edge of the continent was high and buoyant relative to the new ocean basin. As the edge of North America moved away from the hot rift zone, it began to cool and subside beneath the new Atlantic Ocean. This once-active divergent plate boundary became the passive, trailing edge of westward moving North America.
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