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<br />I <br /> <br />1-;" <br /> <br />1 <br /> <br />1 <br /> <br />1 <br /> <br />1 <br /> <br />1 <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />1 <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />. <br />.. <br /> <br />5. <br /> <br />The shoreline materials, being largely of glacial origin, have <br /> <br />been similarly stabilized by the processes described above. <br /> <br />However, the steeper areas of shoreline will be adversely affected <br /> <br />by fluctuating reservoir levels as described in Section II and <br /> <br />slope flattening is recommended in the vicinity of Borrow Area A. <br /> <br />, <br />