| Show 1 MALADE FINE SANDY LOAM the soil of the malade fine sandy loam to a depth of from 2 to 2 21 11 feet consists of a gray fine sandy loam underlain to 6 feet with loam or clay loam usually clay loam in the fifth and sixth toot foot sections and intensely red in color the subsoil Is about the same as the subsoil of the jordan loam but is usually lighter in texture this thi s type occurs occurs in narrow strips of land along the east side of the valley usually occupying the lower portion of the mountain slopes also in small area at the foot of the mountain slope on the west side of the valley north of the southern pacific railroad a nother another south ot of corinne and a long strip on the west side of bear river just back of the higher forelands for elands adjacent to the river the type is generally well drained that on the east sibe side of the valley because of the mountain slope the lower part of which the type occupies and that along bear river because of its proximity to the banks of that stream the area south of corinne is located next to the bluff which also insures good natural drainage the heavy subsoil ot of this type has been deposited in quiet water from the salts sails and clays carried 7 don down by bear river w while bile the top covering of fine sandy loam joam has been formed ly from the surrounding higher lying forelands for fore elands linds along t the e river I 1 f 0 or r from the mountain slopes during later periods sr there Is b but t ve very litt attle le a ikall alkali in tl the ic malade ft aln ne e sandy andy loam the heavy subsoil being comparatively free f from rom it owing to the the good drainage conditions of the type the soil ip i cult cultivated hated principally to a alfalfa fal fa and anae kome orchard fruits faults are grown it Is well adapted to co sugar beets continued next week weak 1 |
