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Quaternary incised valleys, in particular, have been reported worldwide. [4] Because of extensive seismic data coverage on the continental shelf, most recent rivers along the US Gulf Coast have been recognized with their own incised valley extending to the continental shelf break. [5] [6]
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.
Sequence boundaries are formed due to the sea level fall. For example, multi-story fluvial sandstone packages often infill incised valleys formed by the sea level drop associated with sequence boundaries. The incised valleys of sequence boundaries correlate laterally with interfluves, palaeosols formed on the margins of incised valleys. The ...
The Gulf Coastal Lowlands is a geomorphological province in Florida. The province extends along the coast of the Gulf of Mexico from the western end of the Florida Panhandle to near Ft. Myers in southern Florida. The average width of the province is 40 km.
This map shows the Big Bend Coast of Florida in blue, and the Big Bend region in red. The Big Bend of Florida, United States, is an informally named geographic region of North Florida where the Florida Panhandle transitions to the Florida Peninsula south and east of Tallahassee (the area's principal city). [1]
The Gulf of Mexico and Coastal Plain. The Gulf Coastal Plain extends around the Gulf of Mexico in the Southern United States and eastern Mexico.. This coastal plain reaches from the Florida Panhandle, southwest Georgia, the southern two-thirds of Alabama, over most of Mississippi, western Tennessee and Kentucky, extreme southern Illinois, the Missouri Bootheel, eastern and southern Arkansas ...
The Big Bend Coastal Marsh is an extremely narrow but long region, following the Gulf coast beginning near the mouth of the Ochlockonee River (near 29° 45' N, 85° W), until just north of Tampa Bay (near 28° 14' N, 82° 45' W), a distance of approximately 280 miles (450 km), but typically penetrating only 0.5 to 1.5 miles (0.80 to 2.41 km ...
The Gulf Intracoastal Waterway (GIWW [1]) is the portion of the Intracoastal Waterway located along the Gulf Coast of the United States. It is a navigable inland waterway running approximately 1,300 mi (2,100 km) [ 1 ] from Saint Marks, Florida , to Brownsville , Texas .