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[2] [5] Measurements between 1941 and 1972 reported flows which varied between 26,000 and 36,000 US gallons per day (98 and 136 m 3 /d), according to Florida Geological Survey Bulletin 66. [6] The most recent test in 2010 showed daily flow at just 6,000 U.S. gallons per day (23 m 3 /d).
The first comprehensive study of Florida's springs was published in 1947. The next update was released 30 years later in the Florida Geological Survey Bulletin No. 31, Revised, "Springs of Florida". [6] In the 1977 Rosenau survey, there were sixteen offshore (under water) springs identified. All but two were situated on the Gulf coast.
Finch, J., Geological essay on the Tertiary formation in America: American Journal of Science, v. 7, p. 31–43, 1823. Berkenkotter, Richard D, Application of statistical analysis in evaluating bedded deposits of variable thickness—Florida phosphate data (United States. Bureau of Mines.
The lithostratigraphy of the Hawthorn Group (Miocene) of Florida: Florida Geological Survey Bulletin 59 (PDF) (Report). Florida Geological Survey. Scott, Thomas M. (1997). "Miocene to Holocene History of Florida". In Randazzo, Anthony F.; Jones, Douglas S. (eds.). The Geology of Florida. Gainesville, Florida: University Press of Florida. pp. 57 ...
The lithostratigraphy of the Hawthorn Group (Miocene) of Florida: Florida Geological Survey Bulletin 59 (PDF) (Report). Florida Geological Survey. Weems, Robert E.; Edwards, Lucy E. (2001). Geology of Oligocene, Miocene, and Younger Deposits in the Coastal Area of Georgia, Bulletin 131 (PDF) (Report). Atlanta, Georgia: Georgia Geologic Survey ...
The Florida Geological Survey fossil vertebrate collection (FGS) was started during the 1910s and was originally housed in Tallahassee. Under the direction of E. H. Sellards, Herman Gunter, and S. J. Olsen, the FGS collection was the primary source of fossil vertebrate descriptions from Florida until the early 1960s.
The Coharie terrace and shoreline was applied by C. W. Cook in 1931 and was named for the Great Coharie Creek, a tributary of the Black River in North Carolina.It is associated with a Pre-Illinoian interglacial [2] and was the third rise in sea level during the Early Pleistocene glacial retreat and left behind dry land in the form of six distinct islands.
Florida Geological Survey, Richard C. Green, David T. Paul, and Thomas M. Scott, P.G. This page was last edited on 20 January 2024, at 15:16 (UTC). Text is available ...