GEOGRAPHY OF CENTRAL FLORIDA 



183 



TABLE II. 



Mechanical Analyses of Soils and Subsoils in Middle Florida Hammock Belt, 

 Marion Co. (From Soil Surveys of "Ocala" and "Gainesville" areas.) 



17. High hammock ("Portsmouth sandy loam"*) 25^2 miles 

 s. e. of Johnson Pond, Marion Co. A black sandy loam. Depth 

 0-8 inches. (Gainesville area.) 



18. Subsoil of same. A stiff heavy marly clay. Depth 8-36 

 inches. 



19. High hammock (or perhaps red oak woods, the two not 

 being satisfactorily distinguished in the report) 2 miles s. e. of 

 Ocala ' ("Gainesville loamy sand"). Depth o-io inches. (Ocala 

 area.) 



20. Subsoil of same. Depth 10-36 inches. 



21. High hammock ("Gainesville sandy loam") 5 miles s. of 

 Ocala. Depth 0-12 inches. (Ocala area.) 



22. Subsoil of same. Depth 12-36 inches. 



23. High hammock ("Fellowship clay loam") 2 miles s. w. 

 of Ocala. Depth 0-4 inches. (Ocala area.) 



24. Subsoil of same.. Depth 4-36 inches. 



25. Flatwoods soil ("Portsmouth fine sand"t) in n. m. cor- 

 ner of Marion Co., 2^ miles e. of Wacahoota. Depth o-io inches. 

 (Gainesville area.) 



26. Subsoil of same. Depth 10-36 inches. 



*This would doubtless be classified differently by the Bureau of Soils 



See 6th Annual Report, p. 255, footnote, 

 tinadvertently placed in a table headed "Gainesville sand." See 6th Annual 

 Report, p. 256, footnote. 



now, 



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