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1 <br /> ' San Joaquin County, California 141 <br /> NN )Ili <br /> AV <br /> l <br /> 4 V <br /> , <br /> - <br /> r� <br /> A <br /> v <br /> i'. <br /> /J/ {;�t➢➢ 4`rr I <br /> ,4 & <br /> ' Figure 4.—Typical vegetation In an area of WisflabArburua-San Timoteo complex,30 to 50 percent slopes,in the middle ground.The <br /> riparian vegetation in the foreground is In an area of Xerofluvents-Xerorthents complex, 1 to 8 percent slopes,occasionally flooded. <br /> Castle Rock is in the background. <br /> rooting depth is limited by the bedrock at a depth of 20 severe decrease in productivity and in the potential of <br /> ' to 40 inches. Runoff is rapid, and the hazard of water the unit to produce plants suitable for grazing. The very <br /> erosion is very severe. steep topography and the resulting runoff reduce the <br /> This unit is used for livestock grazing or wildlife amount of rainfall that enters the soils. The slope limits <br /> habitat. General management considerations include access by livestock and results in overgrazing of the <br /> the very severe hazard of erosion, the slope, the very less sloping areas. The very low or low available water <br /> low or low available water capacity, and the limited capacity limits the production of desirable forage plants <br /> depth of the Wisflat soils. The characteristic plant in some areas. Fencing is difficult because of the depth <br /> ' community is mainly soft chess, red brome, and to bedrock. <br /> California sagebrush on the Wisflat soil; soft chess, This map unit is in capability subclass We <br /> (oxtail fescue, and red brome on the Arburua soil; and (MLRA-15), nonirrigated. It is in vegetative soil group G. <br /> ' soft chess, wild oat, and filaree on the San Timoteo <br /> soil. Grazing should be controlled so that desirable 277—Xerofluvents, 0 to 2 percent slopes, <br /> vegetation, such as soft chess, is maintained and frequently flooded. These very deep, excessively <br /> enough vegetation is left standing to protect the soils drained and well drained, nearly level soils are on flood <br /> from erosion. Loss of the surface layer results in a plains and interchannel bars in river channels. They <br /> 1 <br />