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a•q <br /> ,-, , <br /> � � � <br /> ro :� <br /> a � � <br /> C H <br /> Y H N <br /> y � � -� <br /> ,�•. <br /> �` H � interpreted as advance outwazh sediments deposited by meitwaters from the advancinp ice ront <br /> � y H dur�ng the]ast glaciation. This material was subsequently overrun by the glaci:r which <br /> x � aa:ounts fot ils dense condition. <br /> o � � 4 2 Hvdroloev <br /> � � � ,.. <br /> � „ Ground water seepage was�esema uoccurdat random deptlis and l�ocat onssintunsu�perv�sed or <br /> H field study. However, seepaB Y, <br /> non-uniform filis. Evidence of prev�ous surficial ponding of water in the southeastern poition <br /> � o y '' of the site was noted during Qur s�te visit. Fluctuauons in the level of ground water may occur <br /> � � � � due to the time ot the ycar and variations in rainfall. <br /> O N <br /> N <br /> I ��' <br /> � <br /> � __; � <br /> �01 _. <br /> i '-_ . <br /> I __I <br /> 1 _ <br /> ��e <br /> r '�t�l � <br /> � <br /> �' 1 ' <br /> 4 <br />