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TABl£ 10.—SOILS CIASSIFIED ACCORDING TO TOE CURREhfT SYSTEM OF CLASSIFICATION—Continued <br />Series <br />I Rasset— <br />Salida......... <br />Shields 11/ <br />Shorewood-- <br />f^Ziwncnnan-- <br />Fajnily U <br />Coarse-loamy, mixed, r.csic- <br />Sandy-skeletal, mixed, mesic- <br />Fine, montmorillonitic, mesic <br />Fine, montmorillonitic, mesic <br />Sandy, mixed, frigid- - - - - <br />Subgroup <br />Typic Argiudolls-- <br />Entic Hapludolls-- <br />Mollic Albaqualfs- <br />Aquic Argiudolls-- <br />Alfic Udipsamments <br />Order <br />Mollisols. <br />Mollisols. <br />>bllisols a <br />Mollisols • <br />Entisols. <br />Hennepin County has soil temperatures on the border between the mesic and frigid soil temperature <br />"classes; therefore, soils in both classes occur in the county. However, these temperature differences are <br />minor and are usually not significant to growing crops in the county. <br />2/ <br />These soils are taxadjuncts of the Anoka series because the surface layer is thicker and darker <br />5"and the sand fraction is dominantly fine sand. <br />3/ <br />These soils are taxadjuncts of the Chaska series because they contain less fine sand than the de- <br />ined range for the series. <br />4/ <br />These soils are taxadjuncts of the Dakota series because they have less translocated clay in the B <br />i^oriion than the defined range for the series. <br />5/ <br />These soils are taxadjuncts of the Dorchester series because they have darker colored upper hori­ <br />zons and contain more sand than the defined range for the series. <br />Some of these soils are taxadjuncts of the Isan series because the C horizon is loam or heavy <br />andy loam. <br />7/ <br />These soils are taxadjuncts of the Langola series because they have more silt and clay in the solum <br />d some have grayer colors than the defined range for the series. <br />1/These soils are taxadjuncts of the Lerdal series because the A horizon is thicker than the defined <br />pnge for the series. <br />i/These soils are taxadjuncts of the Litchfield series because they have a thinner, darker colored A <br />'.orizon and contain more medium and coarse sand than the defined range for the series. <br />10/ <br />Organic soils that have not been classified at the series level. <br />11/These soils are taxadjuncts of the Shields series because the upper part of the B horizon is darker <br />an the defined range for the series. <br />mi■m <br />|il <br />n