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52 <br />• Texture: The folowing notations are suggested:l~ <br /> gravel ..................g loam.................... 1 <br /> very coarse sand........vcos gravelly loam........... gl <br /> coarse sand .............cos stony loam.............. stl <br /> sand ....................s silt.................... si <br /> fine sand ...............fs silt loam............... sil <br /> very fine sand..........vfs clay loam ............... cl <br /> loamy warse sand.......lcos silty clay loam......... sicl <br /> loamy sa~ ..............ls sandy clay loam......... scl <br /> loamy fine sand.........lfs stony clay loam......... stcl <br /> sandy loam ..............sl silty clay.............. sic <br /> fine sandy loam.........fsl clay .................... c <br /> very fine sandy loam....vfsl <br /> gravelly sandy loam.....gsl 1~CaPitalized in Tables <br /> Structure: The terms used follow the outline given on page 228. <br /> Size or class: Fozm or type: <br /> very fine ...............vf platy................... pl <br />• fine ....................f prismatic............... pr <br /> mediisn ..................m columnar............. cpr <br /> coarse ..................c blocky.................. bk <br /> very coarse ............vc angular blocky....... sbk <br /> Grade or distinctness: granular ................ gr <br /> structureless...........0 crianb ................ cr <br /> weak ....................1 single grain............ sg <br /> moderate ................2 massive................. m <br /> strong ..................3 <br /> Thus, the structure of the B hor izon of a solodized-SOlonetz may <br /> be c3cpr; that of the A, o£ a Gray-Brown Podzolic, mlcr; and that <br /> of the B2 of a Reddish Chestnut, m2abk. Horizons having a mixed <br /> structure require two notations. The B1 of a Red-Yellow Podzolic <br /> may be flsbk or m2sbk. <br />• <br />