Soils Associated ivith the JSforfoll: Series. 63 



Acres. 



Calvert County, Md 7, 950 



Mason County, Ky 320 



Norfolk, Va «'55, 488 



Prince George County, Mel... 

 St. Mary County, Md 



Acres. 



n 49, 480 



95. 500 



Monroe silt loam. — A fine sandy or silty loam 10 inches in depth, 

 underlain by a yellow or red silty clay, usually mottled with white 

 or brown beloAV 2 feet. Occurs as low terraces or in hills of little 

 elevation. The forest growth is oak and i)ine. Very little has 

 been cultivated and tliat with very poor success. Cotton can 

 hardly be made to yield one-half bale per acre, and corn propor- 

 tionally less. 



1 i 



Soil (2) 1 28 



Subsoil (2) 2 33 



Acres. 

 Ouachita, La 39,232 



Alloway clay. — Red or gray clay loam 6 inches deep, containing 

 some gravel, underlain liy a mottled yellow and gray sticky clay 

 to a depth of 3 feet or more. Kolling upland or bottoms. Derived 

 from Miocene or glacial material — recent sediments. Good grass 

 and wheat lands. Produces fine apples. Difficult to till. Gen- 

 erally in need of underdrainage. 



1 



Soil (8) 8 



Subsoil (8) ft 



Acres. 



Lyons, N. Y 16,448 



Salem,' X.J 10, 580 



Acres. 



Syracuse, N. Y 24, 832 



Trenton, N..1 11,904 



Mobile clay. — This type consists of a yellow loam, with an aver- 

 age depth of 8 inches, renting on a stiff, i)lastic yellow clay or 

 sandy clay subsoil extending to a depth of 3 or more feet. The 

 surface is characterized by the presence of many iron concretions. 

 Usually found overlying the materials forming the Orangeburg 

 sandy loam. The surface is flat and marked by many swampy, 

 pondlike depressions covered by a scrubby growth of gum. The 

 drainage is generally poor. The type is best adapted to grain and 

 grass. 



r' Part of this was mapped as Leonardtown gravelly loam. It should have 

 been mapped as Leonardtown silt loam with gravel symbol and the gravelly 

 phase described as such in the report. 



