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<br />1 <br />1~ <br />~ ~. <br />' HG - Haverson-Glenberg fine sandy looms, 0 to 3 percent slopes. <br />These nearly level and moderately sloping soils are deep, <br />' calcareous and well-drained. They are on terraces and flood plains. <br />' The average annual precipitation is about 12 inches, the average annual <br />air temperature is about $2 degrees F., and the average frost-£ree <br />' season is about 12$ to 16$ days. The Haverson Soil makes up about 4$ <br />percent of the unit and the Glenberg soil about 35 percent. <br />1 <br />Included in map?ing is about 20 percent of Las :,nimas, eZeobank <br />' and a soil similar to Glenberg except it is darker colorad and non- <br />' calcareous to a depth of about 1~0 inches. <br />The Haverson soil formed in loam alluvium. <br />Typically the surface layer is grayish brcn~ fine sandy loav. <br />' about ~ inches thick. The substratum to a depth of 60 inches consists <br />of brown and grayish-brown layers of silt loam, loam and sandy loo.-.. <br />1 <br />Permeability is moderate and available water capacity is high. <br />' Runoff is slow and erosion hazard is slight. <br />The Glenberg soil forr:ed in sandy alluvium. <br />t 'I~jpically the surface layer is light bro•.+nish gray sandy loam <br />about 32 inches thick. The substratum tc a depth of b0 inches consists <br />;' of layers of pale brown gravelly sand and sandy loam. <br />b Permeability is moderately rapid. Available xater capacity is <br />~ moderate. Runoff is slow and erosion hazard is slight. <br />16 <br />I <br /> <br />